Abstract
Watershed area and a bunch of relief, land use, and wastewater characteristics for 32 upland and 33 lowland small river courses are generated. Based on these characteristics, logistic binary regression models are trained to predict if the river achieves the good physico-chemical status, and discriminant analysis models are trained to predict the physico-chemical status class on a five-class scale.
Univariate models revealed that elevation (for upland rivers), the share of artificial surfaces (for lowland rivers) along with forests, and wastewater quality variables such as biochemical oxygen demand, chemical oxygen demand, and phosphorus are the most significant predictors. Discriminant analysis models performed better on upland than on lowland rivers. Achievement of good status could be predicted with an accuracy of ~90% (with 2 to 4 variable logit models), whereas the status class with an accuracy of 63/48% (with 2 to 4 variable discriminant analysis models) for upland and lowland rivers, respectively. This contribution uses Hungary as a case study.
1 Introduction
Starting in the early 20th century, the pollution of waters, and, in particular, rivers has received growing attention worldwide. Protecting them to fulfill human needs turned out not to be sustainable in the long term. Starting in the late 20th century, water protection measures began to focus on the ecosystems of the water. Two examples are the Clean Water Act in the US [1] or the Water Framework Directive (WFD) in Europe [2]. The goal of the latter is to achieve good ecological status / potential of all surface and subsurface waters by (at the latest) 2027 from a biological point of view. Groundwater, rivers, lakes, transitional and coastal waters as well as estuaries are all in the scope of the WFD.
The primary tool of the WFD is the river basin management plans to be prepared by each member state in a 6-year cycle. Basic unit of the river basin management plans are the water bodies comprising one or more stretches/parts of the waters mentioned above. Categorizing water bodies into a few types facilitates their management. For surface freshwaters, the typology is based on altitude, slope (in case of rivers), geology, sediment, and catchment size of the water body (Table 1) [2, 3, 4].
Hungarian river water body types, and number of the particular water bodies. nWB = number of water bodies in the particular type category. High = number of water bodies classified with high reliability.
type # | altitude | slope | geology | sediment | catchment size | nWB | high |
---|---|---|---|---|---|---|---|
1 | upland | high | siliceous | coarse | small | 20 | 9 |
2 | upland | high | calcareous | coarse | small to medium | 31 | 7 |
3 | upland | medium | calcareous | any | small to medium | 359 | 32 |
4 | upland | medium | calcareous | coarse | large to very large | 19 | 12 |
5 | lowland | low | calcareous | coarse | small to medium | 23 | 8 |
6 | lowland | low | calcareous | medium to fine | small to medium | 376 | 33 |
7 | lowland | low | calcareous | medium to fine | large | 33 | 20 |
8 | lowland | low | calcareous | medium to fine | very large | 18 | 15 |
9 | lowland | m– low | calcareous | coarse | Danube-size | 9 | 9 |
10 | lowland | low | calcareous | medium to fine | Danube-size | 1 | 1 |
After delimiting the water bodies and their watershed, river basin management plans require to list all pressures (i.e., natural and human effects influencing the water quality) and to assess the status of each water body. The status evaluation results in each water body assigned to one of the classes high, good, moderate, poor or bad. Assessing the reliability of the classification (high, medium or low) is also part of the status evaluation. The primary base of the classification is water quality monitoring data. Monitoring here means hydro-morphological, biological and physico-chemical monitoring of each water body. For more details on the physico-chemical status assessment of Hungarian river water bodies, the reader is referred to [5, 6].
For most countries, implementation of the monitoring required by the WFD is a considerable challenge. Traditional monitoring of all water bodies with the necessary reliability would require unreasonably high efforts [7, 8]. This statement is particularly true for Hungary. With a few exemptions, smaller rivers and lakes have not been monitored before the year 2007. The status of only a tiny part (170 out of 1078) of all surface water bodies could be assessed with high reliability in the 2nd river basin management plan, while 145 out of 1078 surface water bodies stayed “grey” (meaning unknown status) [4, 9]. Emerging methods like citizen science, remote sensing, and big data, along with machine learning algorithms, are to be considered as a solution to the monitoring dilemma. However, these methods are not widely known and elaborated yet [10, 11]. On the other hand, monitoring of large rivers is in some cases excessive [12, 13, 14].
A plethora of studies reveal that there is an apparent link between a watershed’s characteristics and it’s water quality [15, 16, 17]. In the hypothetical case of having all the knowledge on the background factors and the processes, no monitoring would be needed. In reality, the relationships are complex, and it is due to this fact that deterministic models (based on the physical processes and referred to as water quality or watershed models) usually do not perform better than statistical ones [18, 19, 20, 21].
The statistical modeling task is usually data-driven: the watershed properties taken into account as predictor variables are those the data is available for. The most important predictor variables are geology, land use, and point sources pollutions [22, 23, 24]. The established relationships, however, are strongly site-specific, since agricultural and industrial as well as wastewater treatment technologies have a substantial variation around the globe. The statistical modeling method has widely been applied in the Americas [25, 26, 27] or Asia [28, 29, 30] but less frequently in Europe. A few European examples are [31, 32].
Logistic binary regression (in short: logit) is widely used in finances (e.g., credit assessment) or medicine (e.g., in predicting disease from the way of life or deoxyribonucleic acid) [33, 34]. It is somewhat less known in predicting the probability of a water pollution event [35, 36]. Linear discriminant analysis is widely used for dimensionality reduction of large datasets, among other things of water quality monitoring [37, 38, 39]. It can also be used to predict class assignation based on continuous or categorical covariates. Since water quality is more mapped on a continuous scale rather than as nominal categories, the use of linear discriminant analysis for predicting water quality is rare. The authors are not aware of any of these methods used to establish a direct link between the watershed’s characteristics, and it’s physico-chemical status class on a regional scale.
1.1 Objectives of the study
This study aims at defining relationships between the physico-chemical status of small watercourses and the physical characteristics of their watershed that can be calculated from databases covering large areas. Also, we aim at defining the accuracy and reliability of such relationships. In particular, we will
determine linear discriminant analysis and logit models with watershed properties as the predictor and the water body’s physico-chemical status class as the predicted variable;
describe the reliability / accuracy of these models.
2 Material & Methods
2.1 Study site
Hungary is a landlocked country situated in the Carpathian basin (Figure 1). About two-thirds of the country’s area is flat, and the rest is hilly. The highest point is 1014 and the lowest 76 meters above sea level. Mountainous regions are typically calcareous whereas lowland regions are loamy or sandy.

Cumulated watershed of study water bodies. Brown: type 3, green: type 6 watersheds. Darker colors show nested catchments.
The climate is continental; yearly mean precipitation is between 500 mm on central lowland regions and 850 mm on the southwestern and hilly areas. Mean monthly temperatures range from −2∘C in January to 20∘C in July. Larger rivers (except for the Danube) originate in direct neighboring countries (it is a typical “downstream country”).
The average population density is 105 capita km−2. Seventy percent of the inhabitants live in towns covering 3.6% of the country’s surface; more than one-fourth of the population lives in or around the capital (Budapest). The most important economic activities include agriculture, industry, and tourism.
2.2 Material
The study presented in this paper is based on the physico-chemical classification of the 2nd river basin management plan of Hungary [40]. The classification was based on water quality measurements from years 2009 – 2012 for following water quality variables: pH, electric conductivity, chloride ion concentration, dissolved oxygen, oxygen saturation, biochemical oxygen demand, chemical oxygen demand, total organic carbon, ammoniumion concentration, total inorganic nitrogen, total nitrogen, orthophosphate ion concentration, total phosphorus [17, 41]. Only river water bodies classified with high reliability were included in the present study.
The cumulated watershed belonging to the outflow point of each water body was generated by summing up the immediate catchment of all upstream water bodies [42]. Basins extending to neighboring countries were created based on the topography (EU-DEM v1.1 [43]) with the Tau-DEM algorithm [44]. Only type 3 and type 6 water bodies classified with high reliability were included in the study (Table 1). In both types, all five classes were represented; in both of them, status good was the most frequent (Table 2).
Frequency of physico-chemical classes in the studied types of water bodies.
type 3 | type 6 | |
---|---|---|
high | 3 | 5 |
good | 13 | 11 |
moderate | 9 | 6 |
poor | 6 | 7 |
bad | 1 | 4 |
total | 32 | 33 |
The EU-DEM also served for calculating mean elevation and slope for each watershed. Based on the Corine Land Cover database [45], land use share for four categories was generated for each basin (Table 3). Point source pollution values were based on two databases. The European Environment Agency’s Urban Wastewater Directive
Characteristics of study watersheds. Mean (minimum – maximum) values; LMQ = long term mean flow of the water body; masl = meters above sea level; PE = population equivalent. WB = Water body, WWTP = wastewater treatment plant.
Type 3 | Type 6 | |
---|---|---|
Relief & hydrology | ||
Watershed area [km2] | 240 (25 - 1000) | 360 (4 - 1000) |
Percent inland [%] | 86 (6.7 – 100) | 100 (89 – 100) |
Mean elevation [masl] | 280 (150 - 540) | 150 (85 - 270) |
Mean slope [%] | 8.8 (1.7 - 16) | 3.1 (0.32 - 8.8) |
Long term specific runoff [mm] | 97 (31 - 170) | 67 (18 - 140) |
Long term mean flow of the WB (LMQ) [m3s−1] | 0.75 (0.053 – 4.0) | 0.75 (0.008 - 3.5) |
Land cover and land use | ||
Artificial surfaces [%] | 7.0 (2.4 - 33) | 6.6 (1.6 - 22) |
Agricultural areas [%] | 47 (5.6 - 88) | 62 (26 - 90) |
Forest and semi natural areas [%] | 46 (4.3 - 86) | 30 (1.1 - 71) |
Wetlands and water bodies [%] | 0.27 (0 - 2) | 1.4 (0 - 12) |
EU urban wastewater database [46] | ||
Number of WWTP-s [-] | 2.7 (0 - 12) | 2.6 (0 - 11) |
Load relative to LMQ [PE m−3s1] (eq. (1)) | 620 (0 - 5900) | 2900 (0 - 54000) |
HU-RWBM WWTP database [48] | ||
Number of WWTP-s [-] | 5.1 (0 - 23) | 6.1 (0 - 28) |
BOD relative to WB LMQ [mg l−1] | 0.61 (0 - 5) | 3.3 (0 - 53) |
COD relative to WB LMQ [mg l−1] | 3.3 (0 - 56) | 14 (0 - 230) |
TN relative to WB LMQ [mg l−1] | 0.85 (0 - 5) | 4.7 (0 - 63) |
TP relative to WB LMQ [mg l−1] | 0.074 (0 - 0.63) | 0.74 (0 - 11) |
Treatment Plants database [46] contains a list of all European Union wastewater plants along with their effluent load values (in population equivalent) and the treatment technology applied, classified into one of seven categories (no treatment / primary / secondary / secondary + nitrogen removal / secondary + phosphorus removal / secondary + nitrogen and phosphorus removal / secondary + other). From this database, the load entering each water body was calculated with the following formula.
where L0 means load from plants with no treatment, L1 means load from plants with primary treatment, L2 means load from plants with secondary treatment, and L3 means plants with secondary + optionally any other treatment. The numbers 0.65, 0.15 and 0.02 are intended to represent mean removal efficiencies [47].
The second source of point sources was a cadaster of the Hungarian wastewater treatment plants enclosed to the 2nd river basin management plan [48]. This database comprises the self-control reports of wastewater treatment plants from the years 2010-2012. It contains yearly mean discharge (in m3/s) and yearly mean effiuent biochemical oxygen demand, chemical oxygen demand, total nitrogen, and total phosphorus concentrations for each plant. Annual load values were calculated, summed up for each watershed, and divided by the long-term mean flow of the respective water body. The values can be interpreted as yearly mean concentrations originating from point sources, with the hypothesis of no in-stream retention and degradation. Tables 3-4 list the watershed properties along with their statistical values.
Matrix of Pearson's linear correlation coefficients of the predictor variables. Upper right part: Type 3, lower left part: Type 6 dataset. Elev = elevation; artif = artificial surfaces; agric = agricultural surfaces. BOD = Biochemical oxygen demand; COD = chemical oxygen demand; TN = total nitrogen; TP = total phosphorus; PCC = physico-chemical status class. Significance codes: 0 < *** < 0.001 < ** < 0.01 < *< 0.05 < x < 0.1< ' ' < 1.
area | elev | slope | artif. | agric | forest | lake | wwQ | load | BOD | COD | TN | TP | PCC | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
area | 0.15 | –0.02 | –0.15 | 0.21 | –0.17 | 0.05 | –0.07 | –0.06 | –0.12 | –0.13 | 0 | –0.05 | 0.03 | |
elev | 0.16 | 0.77*** | 0.01 | –0.63*** | 0.63*** | –0.42* | –0.19 | –0.27 | –0.18 | –0.16 | –0.15 | –0.15 | –0.50** | |
slope | 0.00 | 0.83*** | 0.07 | –0.72*** | 0.70*** | –0.28 | –0.01 | –0.09 | 0.06 | 0.07 | –0.03 | 0.05 | –0.25 | |
artif. | –0.19 | 0.12 | 0.08 | –0.14 | –0.16 | –0.18 | 0.21 | 0.15 | 0.12 | 0.06 | 0.11 | 0.14 | 0.31x | |
agric. | 0.09 | –0.67*** | –0.52** | 0.00 | –0.96*** | 0.35* | –0.04 | 0.14 | –0.02 | –0.08 | 0.03 | –0.03 | 0.33x | |
forest | –0.05 | 0.60*** | 0.45** | –0.27 | –0.95*** | –0.32x | –0.01 | –0.18 | –0.01 | 0.06 | –0.06 | –0.01 | –0.42* | |
lake | 0.08 | 0.26 | 0.31x | –0.12 | –0.27 | 0.17 | –0.18 | –0.11 | –0.14 | –0.14 | –0.19 | –0.18 | –0.04 | |
wwQ | –0.17 | 0.00 | –0.13 | 0.76*** | –0.07 | –0.14 | –0.08 | 0.86*** | 0.81*** | 0.96*** | 0.79*** | 0.88*** | 0.63*** | |
load | –0.11 | –0.09 | –0.14 | 0.64*** | –0.11 | –0.06 | –0.14 | 0.92*** | 0.81*** | 0.88*** | 0.77*** | 0.90*** | 0.59*** | |
BOD | –0.15 | –0.10 | –0.19 | 0.68*** | –0.04 | –0.14 | –0.13 | 0.98*** | 0.96*** | 0.82*** | 0.91*** | 0.88*** | 0.67*** | |
COD | –0.14 | –0.08 | –0.20 | 0.68*** | –0.03 | –0.15 | –0.14 | 0.98*** | 0.95*** | 1.00*** | 0.72*** | 0.85*** | 0.54** | |
TN | –0.17 | 0.00 | –0.15 | 0.71*** | –0.06 | –0.14 | –0.07 | 0.99*** | 0.89*** | 0.97*** | 0.98*** | 0.91*** | 0.64*** | |
TP | –0.19 | –0.08 | –0.21 | 0.69*** | 0.03 | –0.20 | –0.17 | 0.96*** | 0.86*** | 0.96*** | 0.98*** | 0.98*** | 0.64*** | |
PCC | 0.30x | 0.05 | 0.05 | 0.41* | 0.30x | –0.39* | –0.23 | 0.39* | 0.36* | 0.37* | 0.39* | 0.38* | 0.37* |
2.3 Methods
Logistic binary regression is a special case among the generalized linear models. Instead of predicting a continuous variable (as does a linear regression model), the probability of falling into one of two classes is predicted. In our case, the probability of achieving good status is predicted as the function of one or more watershed properties.
While being in their use very similar to regression models, discriminant analysis models have very different underlying mathematics. Instead of defining a predictor function, they aim at describing the discriminant functions that are the best in differentiating among the categories of the function variable. As a result, they still do predict a categorical variable (of two or more categories).
As a first step of the present study, univariate logit models are established and visualized. Based on these models, and predictor variable’s correlation table (Table 4), variables to be included in multivariable models are determined. Two times four multivariable models are investigated on both datasets and with both multivariable methods (Table 5).
List of studied models. All indicated combinations of covariates were applied with both of the logit and the linear discriminant analysis methods. WW = wastewater; COD = chemical oxygen demand; TP = total phosphorus.
Model # | Elevation | Artificial | Forest | WW COD | WW TP | Dataset |
---|---|---|---|---|---|---|
1.3 | x | type 3 | ||||
1.6 | x | type 6 | ||||
2.3 | x | x | type 3 | |||
2.6 | x | x | type 6 | |||
3.3 | x | x | x | type 3 | ||
3.6 | x | x | x | type 6 | ||
4.3 | x | x | x | x | type 3 | |
4.6 | x | x | x | x | type 6 |
The present study had the aim to predict physico-chemical water quality based on the simplest possible watershed properties. Due to the relatively low number of training cases (32/33 watersheds for type 3 / type 6, respectively), the number of predictors could not exceed ~5 (5-6 training cases per predictors, see e.g. [34]). Relatively simple parameters were chosen as predictor variables: relief properties (area, slope, elevation), main land use categories (Table 3), and a few wastewater indicators. The chosen variables are supposed to have the most substantial influence on physico-chemical water quality. Other possible variables would include catchment shape indicators, drainage network (river network) density in the catchment, the slope of the channel network, fragmentation indicators of individual land-use types, land slope within individual land-use classes. These are subjects of future studies.
Variables were added sequentially. Models 1.3 and 1.6 consisted of one and the most significant predictor variable: total phosphorus emitted from point sources. Predictor variables of Models 2.3 and 2.6 were the share of forests (indicating absence of diffuse pollution) on the watershed and the phosphorus from point sources. The results of this model can be visualized on the 2D plane and thus help the reader to understand it’s functioning.
The third predictor variable was elevation (for type 3) and artificial surfaces (type 6). These are still quite significant and at the same time, possibly uncorrelated predictors (Figures 2-3 and Table 4). As a fourth predictor, chemical oxygen demand emitted from point sources was added, representing another aspect of point sources pollution, but is highly correlated with total phosphorus.

Relative probability of status good or high as function of unique watershed properties and 95% confidence intervals. Type 3 water bodies. Black dots show observations. X-axis ranges are calculated as the union of type 3 and type 6 watersheds, but two type 6 watersheds with extremely high point source pollution were excluded. Significance indicated (for the whole dataset).

Relative probability of status good or high as function of unique watershed properties, and 95% confidence intervals. Type 6 water bodies. Black dots show observations. X-axis ranges are calculated as the union of type 3 and type 6 watersheds, but two type 6 watersheds with extremely high point source pollution were excluded. Significance indicated (for the whole dataset).
The same combination of covariates was applied when running the logit and the linear discriminant analysis models. In the case of the logit models, the significance level of the predictor variables, the accuracy of the model, and the “area under the curve” are used as model performance indicators. In the case of linear discriminant analysis models, accuracy and false negative predictions, as well as the difference in the predicted classes, are studied.
Calculations in this study were conducted using the R programming language [49]. For logit models, the stats package, for linear discriminant analysis models, the MASS package [50] was used. ggplot2 package was used to prepare the figures [51].
3 Results
3.1 Logit models
Figures 2 and 3 show fit for one-variable logit models and their 95% confidence interval. Elevation (for type 3 only), artificial surfaces (type 6 only), agricultural and forested areas as well as three wastewater concentrations (except for nitrogen) show high significance levels. The significance of wastewater nitrogen is somewhat weaker (0.06 and 0.09 for type 3 and type 6 waters, respectively). The significance of the aggregated wastewater load (in population equivalent) is around 0.1 (0.08 for type 3 and 0.12 for type 6). As an overall tendency, significance levels are comparable for type 3 and type 6 watersheds. In addition to the already mentioned ones, the most important differences are: area – higher significance for type 6 watersheds; slope – much more significant for type 3 watersheds; wetland and water surfaces – higher significance for type 6.
Concerning the multivariate models, the performance indicators generally increase with the number of variables, although already the one-variable models 1.3 and 1.6 perform quite well: accuracy of 75 – 79% (Table 6). While in the case of Type 3, the elevation, in case of Type 6, the area of artificial surfaces is a better predictor. Adding the second wastewater indicator (COD) hardly adds anything to Type 3 models and adds nothing to type 6 models. The best accuracy is 91% for both types, and the best AUC is 97/94% for type 3 and type 6, respectively.
Performance indicators of logit models [%]. AUC = “area under the curve”.
Model | accuracy | AUC | Model | accuracy | AUC |
---|---|---|---|---|---|
# | # | ||||
1.3 | 75 | 81 | 1.6 | 79 | 91 |
2.3 | 78 | 93 | 2.6 | 88 | 94 |
3.3 | 88 | 96 | 3.6 | 91 | 94 |
4.3 | 91 | 97 | 4.6 | 91 | 94 |
Tables 7 and 8 show confusion matrices for 2×2 selected models. These tables show the amount and type of errors. The terms “positive” and “negative” are used considering the water management point of view: a case (a specific water body) is regarded as positive when interventions/measures are needed to ensure it’s good status (so it’s status is in fact not good). Type II errors (false negatives) are the more severe errors: the waters where the need for a measure is not predicted although needed. In the presented models, Type II errors amount to 6 – 13% of the cases (red numbers in Tables 7 and 8).
Confusion matrices for models 2.3 and 4.3. Red numbers indicate type II errors. Accur. = accuracy.
measured | model 2.3 | model 4.3 | |||||
---|---|---|---|---|---|---|---|
total | good | not good | accur. | good | not good | accur. | |
good | 16 | 13 | 3 | 81% | 15 | 1 | 94% |
not good | 16 | 4 | 12 | 75% | 2 | 14 | 88% |
total | 32 | 17 | 15 | 78% | 17 | 15 | 91% |
Confusion matrices for models 2.6, and 4.6. Red numbers indicate type II errors. Accur. = accuracy.
measured | model 2.6 | model 4.6 | |||||
---|---|---|---|---|---|---|---|
total | good | not good | accur. | good | not good | accur. | |
good | 16 | 14 | 2 | 88% | 15 | 1 | 94% |
not good | 17 | 2 | 15 | 88% | 2 | 15 | 88% |
total | 33 | 16 | 17 | 88% | 17 | 16 | 91% |
3.2 Linear discriminant analysis models
Just as with the logit models, we start with a graphical investigation. This step can not be done if the number of predictor variables is higher than two, thus only models 2.3 and 2.6 are graphically investigated. As a first step, each water body is depicted on a 2D plane as a function of the model variables, with the color representing the status. Secondly, prediction areas of the models are filled up with color for the respective class. At the same time, an uncertainty analysis is conducted: reliability (confidence) of the models is tested with the bootstrapping method [34]: the model is fitted on a random 90% subsample of the training dataset (“submodels”). This step is repeated many times. Those points of the prediction area that belonged to the same class in 95% of the submodels are enclosed with a black line; those belonging to the same class in 80% of the models with a grey line on Figures 4 left and right.

Composite graphs of models 2.3 (left) and 2.6 (right).
The above figures – along with the multivariate models – also help us in concluding the role of the single variables. Considering the models,
only water bodies with a forest share above 80% have a chance to be in high status;
only water bodies with forest share above ~30% have an opportunity to achieve good status;
water bodies where wastewater total phosphorus relative to long term mean flow is higher than 0.5 (type3) or 4 mg/l (type 6) are unlikely to achieve good status.
These numbers will be slightly different with the inclusion of other variables or with a different training dataset; what is essential now is that they can be defined.
As already mentioned, rather than predicting if a water body achieves or not the good status, linear discriminant analysis models aim at predicting its status on a five-class scale. It is easy to understand: without any knowledge, the class (on a five-class scale) will be met with a 20% probability (blind model). Knowing the frequencies of the unique classes and presuming all cases in the most frequent class, a higher probability can be achieved. In our study, the accuracy of the so-called naïve model will be 13/32 = 41% and 11/33 = 33% for type 3 and type 6 models, respectively (Table 2). To quantify the performance difference between type 3 and type 6 models, the accuracy increments (compared to the naïve model) are also represented in Table 9.
Linear discriminant analysis models’ performance indicators. Increment = increment in accuracy compared to the naïve model.
Model # | accuracy | increment | Model # | accuracy | increment |
---|---|---|---|---|---|
1.3 | 47 | 06 | 1.6 | 36 | 03 |
2.3 | 66 | 25 | 2.6 | 48 | 15 |
3.3 | 63 | 22 | 3.6 | 48 | 15 |
4.3 | 63 | 22 | 4.6 | 48 | 15 |
Tables 10 and 11 contain confusion matrices for two-and four-variable linear discriminant analysis models.
Confusion matrix for type 3 models. Red: false negative predictions.
measured | model 2.3 | model 4.3 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
total | high | good | mod. | poor | bad | accur. | high | good | mod. | poor | bad | accur. | |
high | 3 | 1 | 2 | 0 | 0 | 0 | 33% | 1 | 2 | 0 | 0 | 0 | 33% |
good | 13 | 0 | 11 | 2 | 0 | 0 | 85% | 1 | 10 | 2 | 0 | 0 | 77% |
mod. | 9 | 0 | 3 | 6 | 0 | 0 | 67% | 0 | 4 | 5 | 0 | 0 | 56% |
poor | 6 | 0 | 1[x] | 2 | 2 | 1 | 33% | 0 | 1[x] | 2 | 3 | 0 | 50% |
bad | 1 | 0 | 0 | 0 | 0 | 1 | 100% | 0 | 0 | 0 | 0 | 1 | 100% |
total | 32 | 1 | 17 | 10 | 2 | 2 | 66% | 2 | 17 | 9 | 3 | 1 | 63% |
*prediction three classes aside. Mod. = moderate; accur. = accuracy. Zeros not indicated.
Confusion matrix for type 6 models. Red: false negative predictions.
measured | model 2.6 | model 4.6 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
total | high | good | mod. | poor | bad | accur. | high | good | mod. | poor | bad | accur. | |
high | 5 | 0 | 3 | 0 | 2[*] | 0 | 0% | 0 | 3 | 0 | 2[*] | 0 | 0% |
good | 11 | 0 | 10 | 0 | 1[x] | 0 | 91% | 0 | 9 | 0 | 2[x] | 0 | 82% |
mod. | 6 | 0 | 3 | 0 | 2 | 1[x] | 0% | 0 | 3 | 1 | 2 | 0 | 17% |
poor | 7 | 0 | 2[x] | 0 | 5 | 0 | 71% | 0 | 2[x] | 0 | 5 | 0 | 71% |
bad | 4 | 0 | 2[*] | 0 | 1 | 1 | 25% | 0 | 2[*] | 0 | 1 | 1 | 25% |
total | 33 | 0 | 20 | 0 | 11 | 2 | 48% | 0 | 19 | 1 | 12 | 1 | 48% |
Mod. = moderate; accur. = accuracy. Zeros not indicated.
Two kinds of errors are investigated: first, false negatives (type II errors) and second, misclassification by two or more classes (the formers are marked with red, the latter with x and * in Tables 10 – 11). The number of false negative cases is 4 and 5 for models 2.3 and 4.3, respectively, and 7 for both of the models 2.6 and 4.6.
"Very big" mistakes (misclassification by three classes) only happen with type 6 models, however, in both directions. Their number is 2×2 with both models (2× underestimation by three classes, 2x overestimation by three classes. The number of "big" mistakes (over- or underestimation by two classes) is just the same for type 6 models. One type 3 case is overestimated by both of the models 2.3 and 4.3.
4 Discussion
Two times four logit models plus two times four linear discriminant analysis models were studied. All of them yielded consistent results, which indicates the suitability of the training data – modeling methods combinations for the required purpose.
Concerning the basic watershed properties (area, elevation, slope), only elevation is significant and only with the type 3 dataset. The cause of this fact might be that elevation of the watershed is in a strong correlation with land use: both settlements and agricultural activities tend to concentrate on lower areas. The next two most significant covariates are slope with type 3 watersheds (significance = 0.08) and area with type 6 (significance = 0.14). The slope of type 6 basins is not so indicative because it covers only a narrower range (Table 3). Relatively higher importance of catchment area on lowlands can be understood, taking into account that agricultural surfaces have a higher (62 versus 47) whereas forests a lower (30 versus 46) percentage on type 6 versus type 3 watersheds.
From the four land use covariates, agricultural and forested surfaces along with artificial surfaces turned out to be significant, this latter only with type 6. Non-significance of wetlands and waters might be explained by the fact that the extent of their effect very much depends on their location (near to outflow point versus close to the origin) [52] which was not accounted for in the models.
The aggregated wastewater indicator (load in population equivalent) turned out not to be significant. From the unique components of wastewater, both biochemical and chemical oxygen demand are significant with both types; however, biochemical oxygen demand more with type 3 and chemical oxygen demand more with type 6. From the nutrient indicators, only total phosphorus is significant, which emphasizes the role of point sources in phosphorus contamination of rivers [53].
Univariate logit models quantify the role of each watershed characteristic in water bodies’ status. Concerning type 3 watersheds, those with a mean elevation above 400 meters above sea level or with an agricultural share < 30% or with a forest share > 60% will achieve good status (confidence > 95%). On the contrary, type 3 watersheds with elevation < 200m, agricultural share > 70% or forest share < 30% will not achieve good status. As for type 6 watersheds, forest share > 45% or phosphorus load below 0.1 mg/l are guarantees for achieving;whereas forest share < 15%, COD load above 15 mg/l or phosphorus above 0.5 mg/l for not achieving good status. Kändler et al. [31] also concluded that forest proportions bigger than 70% lead to low concentrations of contaminants; however, concerning arable land, their threshold was somewhat lower (40%).
Regarding the multivariate logit models, already the two-variable (forest + total phosphorus) models perform quite well: they show an accuracy of 78/88% and an “area under the curve” value of 93/94% for type 3 and type 6 models, respectively. Three- and four-variable models supersede these values.
Considering multivariate linear discriminant analysis models, two- or more variable models perform better than univariate ones. Concerning type 3 models, there is no significant difference between models 2.3, 3.3, 4.3; the two-variable model even performs slightly better. Concerning type 6 models, there is no difference at all, between models 2.6, 3.6, and 4.6.
The more marked difference (concerning discriminant analysis models) is between type 3 and type 6 models: the former perform much better. A possible cause for this is the presence of waters loaded with extremely high point source pollution in this data set (Figure 4 right).
A comparison of logit models with linear discriminant analysis models, in general, is not straightforward since they had a different objective. Counting the amount / proportion of water bodies misclassified to achieve good status, logit models perform better. The fact that linear discriminant analysis models treat classes as nominal variables serves as a reason for this. The finding is in line with Avila et al. [36], who concluded that multinomial regression models performed slightly better than linear discriminant analysis models in terms of cross-validation error rates.
The most frequent cause for status overprediction (by discriminant analysis models) is that water quality at the monitoring location is influenced by a near wastewater inlet (IDs 31, 67-70, Table 12) or industrial wastewater (ID 69) or a fishing pond (ID 66). Industrial wastewater was not accounted for in the models due to a lack of data. In many cases, a more recent study [54] assessed a status closer to the one predicted by the models (IDs 31, 63, 65-70).
Water bodies misclassified by two or more classes by any of models 2.3 to 4.3 or 2.6 to 4.6.
Type | ID | wbname | measured | model | model | model |
---|---|---|---|---|---|---|
1.3 / 2.6 | 3.3 / 3.6 | 4.3 / 4.6 | ||||
3 | 31 | Dobroda-creek and tributaries | poor | good[x] | good[x] | good[x] |
6 | 61 | Ferenc-channel | high | poor[*] | poor[*] | poor[*] |
6 | 62 | Hunyor-creek | high | poor[*] | poor[*] | poor[*] |
6 | 63 | Lanka-channel | good | poor[x] | poor[x] | poor[x] |
6 | 64 | Tapolca-creek | good | good | poor[x] | poor[x] |
6 | 65 | Répce-spillway | mod | bad[x] | bad[x] | mod |
6 | 66 | Kõrös-ér | poor | good[x] | good[x] | good[x] |
6 | 67 | Mirhó-Gyolcsi-channel | poor | poor | mod | good[x] |
6 | 68 | Pécsi-víz middle | poor | good[x] | poor | poor |
6 | 69 | Nádor-channel (Sárvíz) upper | bad | good[*] | good[*] | good[*] |
6 | 70 | Völgységi-creek to Rák-creek | bad | good[*] | good[*] | good[*] |
Mod. = moderate.
Two of the under-predicted waters are water diversion channels (IDs 61 and 65, Table 12); water quality here is determined not by the own watershed, instead by the source water (Duna and Répce). Hunyor-creek (ID 62) is a small creek, with mainly of agricultural land use on the watershed. However, the monitoring point far upstream. The proportion of forests on the basin of the monitoring point is much higher than on the watershed draining to the water body outflow point. Tapolca-creek (ID 64) has a high wastewater share; however, effiuent wastewater thresholds in this region are stricter than in the other areas of the country due to the vulnerability of the Lake Balaton (receptor of the Tapolca-creek).
Bearing the false predictions in mind, future developments should be the exclusion of water diversion channels (where their watershed does not determine water quality). Also, the next models should account for the distance between the monitoring location and the source of wastewaters (including industrial plants and fishing ponds).
5 Conclusions
Both logit and linear discriminant analysis models are useful in predicting if a water body achieves good status and / or it’s status class. The most significant covariates for both upland and lowland rivers, with both of the logit and linear discriminant analysis methods were the share of agricultural land and the share of forests, the organic wastewater indicators and wastewater TP load. Models perform better on upland than on lowland rivers.
Achievement of good status could be predicted with an accuracy of ~90% (with 5-variable logit models), whereas the status class with an accuracy of 72/55% (with 5-variable linear discriminant analysis models) for upland and lowland rivers, respectively.
Acknowledgement
The Higher Education Excellence Program of the Ministry of Human Capacities, Hungary supported the research presented in this paper in the frame of the Water sciences and Disaster Prevention research area of the Budapest University of Technology and Economics (BME FIKP-VÍZ).
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- The influence of river training on the location of erosion and accumulation zones (Kłodzko County, South West Poland)
- Multi-temporal survey of diaphragm wall with terrestrial laser scanning method
- Functionality and reliability of horizontal control net (Poland)
- Strata behavior and control strategy of backfilling collaborate with caving fully-mechanized mining
- The use of classical methods and neural networks in deformation studies of hydrotechnical objects
- Ice-crevasse sedimentation in the eastern part of the Głubczyce Plateau (S Poland) during the final stage of the Drenthian Glaciation
- Structure of end moraines and dynamics of the recession phase of the Warta Stadial ice sheet, Kłodawa Upland, Central Poland
- Mineralogy, mineral chemistry and thermobarometry of post-mineralization dykes of the Sungun Cu–Mo porphyry deposit (Northwest Iran)
- Main problems of the research on the Palaeolithic of Halych-Dnister region (Ukraine)
- Application of isometric transformation and robust estimation to compare the measurement results of steel pipe spools
- Hybrid machine learning hydrological model for flood forecast purpose
- Rainfall thresholds of shallow landslides in Wuyuan County of Jiangxi Province, China
- Dynamic simulation for the process of mining subsidence based on cellular automata model
- Developing large-scale international ecological networks based on least-cost path analysis – a case study of Altai mountains
- Seismic characteristics of polygonal fault systems in the Great South Basin, New Zealand
- New approach of clustering of late Pleni-Weichselian loess deposits (L1LL1) in Poland
- Implementation of virtual reference points in registering scanning images of tall structures
- Constraints of nonseismic geophysical data on the deep geological structure of the Benxi iron-ore district, Liaoning, China
- Mechanical analysis of basic roof fracture mechanism and feature in coal mining with partial gangue backfilling
- The violent ground motion before the Jiuzhaigou earthquake Ms7.0
- Landslide site delineation from geometric signatures derived with the Hilbert–Huang transform for cases in Southern Taiwan
- Hydrological process simulation in Manas River Basin using CMADS
- LA-ICP-MS U–Pb ages of detrital zircons from Middle Jurassic sedimentary rocks in southwestern Fujian: Sedimentary provenance and its geological significance
- Analysis of pore throat characteristics of tight sandstone reservoirs
- Effects of igneous intrusions on source rock in the early diagenetic stage: A case study on Beipiao Formation in Jinyang Basin, Northeast China
- Applying floodplain geomorphology to flood management (The Lower Vistula River upstream from Plock, Poland)
- Effect of photogrammetric RPAS flight parameters on plani-altimetric accuracy of DTM
- Morphodynamic conditions of heavy metal concentration in deposits of the Vistula River valley near Kępa Gostecka (central Poland)
- Accuracy and functional assessment of an original low-cost fibre-based inclinometer designed for structural monitoring
- The impacts of diagenetic facies on reservoir quality in tight sandstones
- Application of electrical resistivity imaging to detection of hidden geological structures in a single roadway
- Comparison between electrical resistivity tomography and tunnel seismic prediction 303 methods for detecting the water zone ahead of the tunnel face: A case study
- The genesis model of carbonate cementation in the tight oil reservoir: A case of Chang 6 oil layers of the Upper Triassic Yanchang Formation in the western Jiyuan area, Ordos Basin, China
- Disintegration characteristics in granite residual soil and their relationship with the collapsing gully in South China
- Analysis of surface deformation and driving forces in Lanzhou
- Geochemical characteristics of produced water from coalbed methane wells and its influence on productivity in Laochang Coalfield, China
- A combination of genetic inversion and seismic frequency attributes to delineate reservoir targets in offshore northern Orange Basin, South Africa
- Explore the application of high-resolution nighttime light remote sensing images in nighttime marine ship detection: A case study of LJ1-01 data
- DTM-based analysis of the spatial distribution of topolineaments
- Spatiotemporal variation and climatic response of water level of major lakes in China, Mongolia, and Russia
- The Cretaceous stratigraphy, Songliao Basin, Northeast China: Constrains from drillings and geophysics
- Canal of St. Bartholomew in Seča/Sezza: Social construction of the seascape
- A modelling resin material and its application in rock-failure study: Samples with two 3D internal fracture surfaces
- Utilization of marble piece wastes as base materials
- Slope stability evaluation using backpropagation neural networks and multivariate adaptive regression splines
- Rigidity of “Warsaw clay” from the Poznań Formation determined by in situ tests
- Numerical simulation for the effects of waves and grain size on deltaic processes and morphologies
- Impact of tourism activities on water pollution in the West Lake Basin (Hangzhou, China)
- Fracture characteristics from outcrops and its meaning to gas accumulation in the Jiyuan Basin, Henan Province, China
- Impact evaluation and driving type identification of human factors on rural human settlement environment: Taking Gansu Province, China as an example
- Identification of the spatial distributions, pollution levels, sources, and health risk of heavy metals in surface dusts from Korla, NW China
- Petrography and geochemistry of clastic sedimentary rocks as evidence for the provenance of the Jurassic stratum in the Daqingshan area
- Super-resolution reconstruction of a digital elevation model based on a deep residual network
- Seismic prediction of lithofacies heterogeneity in paleogene hetaoyuan shale play, Biyang depression, China
- Cultural landscape of the Gorica Hills in the nineteenth century: Franciscean land cadastre reports as the source for clarification of the classification of cultivable land types
- Analysis and prediction of LUCC change in Huang-Huai-Hai river basin
- Hydrochemical differences between river water and groundwater in Suzhou, Northern Anhui Province, China
- The relationship between heat flow and seismicity in global tectonically active zones
- Modeling of Landslide susceptibility in a part of Abay Basin, northwestern Ethiopia
- M-GAM method in function of tourism potential assessment: Case study of the Sokobanja basin in eastern Serbia
- Dehydration and stabilization of unconsolidated laminated lake sediments using gypsum for the preparation of thin sections
- Agriculture and land use in the North of Russia: Case study of Karelia and Yakutia
- Textural characteristics, mode of transportation and depositional environment of the Cretaceous sandstone in the Bredasdorp Basin, off the south coast of South Africa: Evidence from grain size analysis
- One-dimensional constrained inversion study of TEM and application in coal goafs’ detection
- The spatial distribution of retail outlets in Urumqi: The application of points of interest
- Aptian–Albian deposits of the Ait Ourir basin (High Atlas, Morocco): New additional data on their paleoenvironment, sedimentology, and palaeogeography
- Traditional agricultural landscapes in Uskopaljska valley (Bosnia and Herzegovina)
- A detection method for reservoir waterbodies vector data based on EGADS
- Modelling and mapping of the COVID-19 trajectory and pandemic paths at global scale: A geographer’s perspective
- Effect of organic maturity on shale gas genesis and pores development: A case study on marine shale in the upper Yangtze region, South China
- Gravel roundness quantitative analysis for sedimentary microfacies of fan delta deposition, Baikouquan Formation, Mahu Depression, Northwestern China
- Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
- Application of laser scanning technology for structure gauge measurement
- Calibration of the depth invariant algorithm to monitor the tidal action of Rabigh City at the Red Sea Coast, Saudi Arabia
- Evolution of the Bystrzyca River valley during Middle Pleistocene Interglacial (Sudetic Foreland, south-western Poland)
- A 3D numerical analysis of the compaction effects on the behavior of panel-type MSE walls
- Landscape dynamics at borderlands: analysing land use changes from Southern Slovenia
- Effects of oil viscosity on waterflooding: A case study of high water-cut sandstone oilfield in Kazakhstan
- Special Issue: Alkaline-Carbonatitic magmatism
- Carbonatites from the southern Brazilian Platform: A review. II: Isotopic evidences
- Review Article
- Technology and innovation: Changing concept of rural tourism – A systematic review
Articles in the same Issue
- Regular Articles
- The simulation approach to the interpretation of archival aerial photographs
- The application of137Cs and210Pbexmethods in soil erosion research of Titel loess plateau, Vojvodina, Northern Serbia
- Provenance and tectonic significance of the Zhongwunongshan Group from the Zhongwunongshan Structural Belt in China: insights from zircon geochronology
- Analysis, Assessment and Early Warning of Mudflow Disasters along the Shigatse Section of the China–Nepal Highway
- Sedimentary succession and recognition marks of lacustrine gravel beach-bars, a case study from the Qinghai Lake, China
- Predicting small water courses’ physico-chemical status from watershed characteristics with two multivariate statistical methods
- An Overview of the Carbonatites from the Indian Subcontinent
- A new statistical approach to the geochemical systematics of Italian alkaline igneous rocks
- The significance of karst areas in European national parks and geoparks
- Geochronology, trace elements and Hf isotopic geochemistry of zircons from Swat orthogneisses, Northern Pakistan
- Regional-scale drought monitor using synthesized index based on remote sensing in northeast China
- Application of combined electrical resistivity tomography and seismic reflection method to explore hidden active faults in Pingwu, Sichuan, China
- Impact of interpolation techniques on the accuracy of large-scale digital elevation model
- Natural and human-induced factors controlling the phreatic groundwater geochemistry of the Longgang River basin, South China
- Land use/land cover assessment as related to soil and irrigation water salinity over an oasis in arid environment
- Effect of tillage, slope, and rainfall on soil surface microtopography quantified by geostatistical and fractal indices during sheet erosion
- Validation of the number of tie vectors in post-processing using the method of frequency in a centric cube
- An integrated petrophysical-based wedge modeling and thin bed AVO analysis for improved reservoir characterization of Zhujiang Formation, Huizhou sub-basin, China: A case study
- A grain size auto-classification of Baikouquan Formation, Mahu Depression, Junggar Basin, China
- Dynamics of mid-channel bars in the Middle Vistula River in response to ferry crossing abutment construction
- Estimation of permeability and saturation based on imaginary component of complex resistivity spectra: A laboratory study
- Distribution characteristics of typical geological relics in the Western Sichuan Plateau
- Inconsistency distribution patterns of different remote sensing land-cover data from the perspective of ecological zoning
- A new methodological approach (QEMSCAN®) in the mineralogical study of Polish loess: Guidelines for further research
- Displacement and deformation study of engineering structures with the use of modern laser technologies
- Virtual resolution enhancement: A new enhancement tool for seismic data
- Aeromagnetic mapping of fault architecture along Lagos–Ore axis, southwestern Nigeria
- Deformation and failure mechanism of full seam chamber with extra-large section and its control technology
- Plastic failure zone characteristics and stability control technology of roadway in the fault area under non-uniformly high geostress: A case study from Yuandian Coal Mine in Northern Anhui Province, China
- Comparison of swarm intelligence algorithms for optimized band selection of hyperspectral remote sensing image
- Soil carbon stock and nutrient characteristics of Senna siamea grove in the semi-deciduous forest zone of Ghana
- Carbonatites from the Southern Brazilian platform: I
- Seismicity, focal mechanism, and stress tensor analysis of the Simav region, western Turkey
- Application of simulated annealing algorithm for 3D coordinate transformation problem solution
- Application of the terrestrial laser scanner in the monitoring of earth structures
- The Cretaceous igneous rocks in southeastern Guangxi and their implication for tectonic environment in southwestern South China Block
- Pore-scale gas–water flow in rock: Visualization experiment and simulation
- Assessment of surface parameters of VDW foundation piles using geodetic measurement techniques
- Spatial distribution and risk assessment of toxic metals in agricultural soils from endemic nasopharyngeal carcinoma region in South China
- An ABC-optimized fuzzy ELECTRE approach for assessing petroleum potential at the petroleum system level
- Microscopic mechanism of sandstone hydration in Yungang Grottoes, China
- Importance of traditional landscapes in Slovenia for conservation of endangered butterfly
- Landscape pattern and economic factors’ effect on prediction accuracy of cellular automata-Markov chain model on county scale
- The influence of river training on the location of erosion and accumulation zones (Kłodzko County, South West Poland)
- Multi-temporal survey of diaphragm wall with terrestrial laser scanning method
- Functionality and reliability of horizontal control net (Poland)
- Strata behavior and control strategy of backfilling collaborate with caving fully-mechanized mining
- The use of classical methods and neural networks in deformation studies of hydrotechnical objects
- Ice-crevasse sedimentation in the eastern part of the Głubczyce Plateau (S Poland) during the final stage of the Drenthian Glaciation
- Structure of end moraines and dynamics of the recession phase of the Warta Stadial ice sheet, Kłodawa Upland, Central Poland
- Mineralogy, mineral chemistry and thermobarometry of post-mineralization dykes of the Sungun Cu–Mo porphyry deposit (Northwest Iran)
- Main problems of the research on the Palaeolithic of Halych-Dnister region (Ukraine)
- Application of isometric transformation and robust estimation to compare the measurement results of steel pipe spools
- Hybrid machine learning hydrological model for flood forecast purpose
- Rainfall thresholds of shallow landslides in Wuyuan County of Jiangxi Province, China
- Dynamic simulation for the process of mining subsidence based on cellular automata model
- Developing large-scale international ecological networks based on least-cost path analysis – a case study of Altai mountains
- Seismic characteristics of polygonal fault systems in the Great South Basin, New Zealand
- New approach of clustering of late Pleni-Weichselian loess deposits (L1LL1) in Poland
- Implementation of virtual reference points in registering scanning images of tall structures
- Constraints of nonseismic geophysical data on the deep geological structure of the Benxi iron-ore district, Liaoning, China
- Mechanical analysis of basic roof fracture mechanism and feature in coal mining with partial gangue backfilling
- The violent ground motion before the Jiuzhaigou earthquake Ms7.0
- Landslide site delineation from geometric signatures derived with the Hilbert–Huang transform for cases in Southern Taiwan
- Hydrological process simulation in Manas River Basin using CMADS
- LA-ICP-MS U–Pb ages of detrital zircons from Middle Jurassic sedimentary rocks in southwestern Fujian: Sedimentary provenance and its geological significance
- Analysis of pore throat characteristics of tight sandstone reservoirs
- Effects of igneous intrusions on source rock in the early diagenetic stage: A case study on Beipiao Formation in Jinyang Basin, Northeast China
- Applying floodplain geomorphology to flood management (The Lower Vistula River upstream from Plock, Poland)
- Effect of photogrammetric RPAS flight parameters on plani-altimetric accuracy of DTM
- Morphodynamic conditions of heavy metal concentration in deposits of the Vistula River valley near Kępa Gostecka (central Poland)
- Accuracy and functional assessment of an original low-cost fibre-based inclinometer designed for structural monitoring
- The impacts of diagenetic facies on reservoir quality in tight sandstones
- Application of electrical resistivity imaging to detection of hidden geological structures in a single roadway
- Comparison between electrical resistivity tomography and tunnel seismic prediction 303 methods for detecting the water zone ahead of the tunnel face: A case study
- The genesis model of carbonate cementation in the tight oil reservoir: A case of Chang 6 oil layers of the Upper Triassic Yanchang Formation in the western Jiyuan area, Ordos Basin, China
- Disintegration characteristics in granite residual soil and their relationship with the collapsing gully in South China
- Analysis of surface deformation and driving forces in Lanzhou
- Geochemical characteristics of produced water from coalbed methane wells and its influence on productivity in Laochang Coalfield, China
- A combination of genetic inversion and seismic frequency attributes to delineate reservoir targets in offshore northern Orange Basin, South Africa
- Explore the application of high-resolution nighttime light remote sensing images in nighttime marine ship detection: A case study of LJ1-01 data
- DTM-based analysis of the spatial distribution of topolineaments
- Spatiotemporal variation and climatic response of water level of major lakes in China, Mongolia, and Russia
- The Cretaceous stratigraphy, Songliao Basin, Northeast China: Constrains from drillings and geophysics
- Canal of St. Bartholomew in Seča/Sezza: Social construction of the seascape
- A modelling resin material and its application in rock-failure study: Samples with two 3D internal fracture surfaces
- Utilization of marble piece wastes as base materials
- Slope stability evaluation using backpropagation neural networks and multivariate adaptive regression splines
- Rigidity of “Warsaw clay” from the Poznań Formation determined by in situ tests
- Numerical simulation for the effects of waves and grain size on deltaic processes and morphologies
- Impact of tourism activities on water pollution in the West Lake Basin (Hangzhou, China)
- Fracture characteristics from outcrops and its meaning to gas accumulation in the Jiyuan Basin, Henan Province, China
- Impact evaluation and driving type identification of human factors on rural human settlement environment: Taking Gansu Province, China as an example
- Identification of the spatial distributions, pollution levels, sources, and health risk of heavy metals in surface dusts from Korla, NW China
- Petrography and geochemistry of clastic sedimentary rocks as evidence for the provenance of the Jurassic stratum in the Daqingshan area
- Super-resolution reconstruction of a digital elevation model based on a deep residual network
- Seismic prediction of lithofacies heterogeneity in paleogene hetaoyuan shale play, Biyang depression, China
- Cultural landscape of the Gorica Hills in the nineteenth century: Franciscean land cadastre reports as the source for clarification of the classification of cultivable land types
- Analysis and prediction of LUCC change in Huang-Huai-Hai river basin
- Hydrochemical differences between river water and groundwater in Suzhou, Northern Anhui Province, China
- The relationship between heat flow and seismicity in global tectonically active zones
- Modeling of Landslide susceptibility in a part of Abay Basin, northwestern Ethiopia
- M-GAM method in function of tourism potential assessment: Case study of the Sokobanja basin in eastern Serbia
- Dehydration and stabilization of unconsolidated laminated lake sediments using gypsum for the preparation of thin sections
- Agriculture and land use in the North of Russia: Case study of Karelia and Yakutia
- Textural characteristics, mode of transportation and depositional environment of the Cretaceous sandstone in the Bredasdorp Basin, off the south coast of South Africa: Evidence from grain size analysis
- One-dimensional constrained inversion study of TEM and application in coal goafs’ detection
- The spatial distribution of retail outlets in Urumqi: The application of points of interest
- Aptian–Albian deposits of the Ait Ourir basin (High Atlas, Morocco): New additional data on their paleoenvironment, sedimentology, and palaeogeography
- Traditional agricultural landscapes in Uskopaljska valley (Bosnia and Herzegovina)
- A detection method for reservoir waterbodies vector data based on EGADS
- Modelling and mapping of the COVID-19 trajectory and pandemic paths at global scale: A geographer’s perspective
- Effect of organic maturity on shale gas genesis and pores development: A case study on marine shale in the upper Yangtze region, South China
- Gravel roundness quantitative analysis for sedimentary microfacies of fan delta deposition, Baikouquan Formation, Mahu Depression, Northwestern China
- Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
- Application of laser scanning technology for structure gauge measurement
- Calibration of the depth invariant algorithm to monitor the tidal action of Rabigh City at the Red Sea Coast, Saudi Arabia
- Evolution of the Bystrzyca River valley during Middle Pleistocene Interglacial (Sudetic Foreland, south-western Poland)
- A 3D numerical analysis of the compaction effects on the behavior of panel-type MSE walls
- Landscape dynamics at borderlands: analysing land use changes from Southern Slovenia
- Effects of oil viscosity on waterflooding: A case study of high water-cut sandstone oilfield in Kazakhstan
- Special Issue: Alkaline-Carbonatitic magmatism
- Carbonatites from the southern Brazilian Platform: A review. II: Isotopic evidences
- Review Article
- Technology and innovation: Changing concept of rural tourism – A systematic review