Abstract
Horizontal control networks established with monuments are functional if the conditions related to the number of control points, their density, condition and stability of coordinates are met. For functionality defined in those terms, deterministic accuracy characteristics are of little use. The subject matter discussed herein includes the two key features of geodetic control points, i.e., usability and stability. Due to the varying properties of those variables and the impact of the operating time of the system, there is no alternative to reliability-based approach in developing the functionality model. The measures of functionality and the procedures of data acquisition for developing the model of the control network destruction process have been defined. The solution presented herein is relevant for geodetic practice, providing a standard procedure for defining the time frame and the scope of the control network upgrading. The identified destruction process model optimizes this task assuming critical states expressed by the functionality probability. The applied approach is an example of the reliability theory-based approach typical for engineering. The issue of simulating the destruction process is illustrated with the results of the tests of class 3 control networks conducted in Kielce and Lodz regions in Poland. As a result of the tests, the characteristic properties of the control network destruction process have been identified. It was also shown how the patterns of usability and accuracy of the geodetic control points are relevant on the stage of implementing investment project tasks.
1 Introduction
The spatial correctness of any investment project depends on the quality of the control network. On the territory of Poland, in accordance with technical regulations in practice, class 3 control networks are usually used [1,2]. Geodetic control points are physically represented in the field by appropriate monuments that ensure the stability of their coordinates. The coordinates, recorded in the National Geodetic and Cartographic Database on the basis of the original measurement, are then used for years in the unchanged form. In terms of accuracy, class 3 control network is considered superior for all measurement tasks, including the cases when the investment project is implemented on more accurate autonomous networks. The issue of aligning control networks of variable accuracy is solved with the use of Hausbrandt’s posttransformation correction [3,4,5]. It should also be noted here that any corrections of the coordinates of individual geodetic control points is only possible if the entire control network undergoes an upgrade or an update measurement [1].
Class 3 control network is functional if it meets the requirements related to the accuracy of coordinates of control points and the density of monuments in the field. According to the applicable technical regulations [1], the mean error of adjusted position of a class 3 network point for control formerly classified as class II should be mp ≤ 0.05 m and for control points formerly classified as class III, mp ≤ 0.10 m. The coordinates of control points in PL-2000 coordinates system were determined by transforming the “1965” coordinates system. Due to local deformations and errors of the original system, as well as its operating time, the currently available data may be – and, as practice shows, frequently are – substandard.
The requirement on the density of monuments provided in the relevant technical regulations is imprecisely formulated. On the developed area, the density of class 3 control network points should be at least 1 point on 20 hectares [2]. In practice, control points are expected to be placed not further than 200–300 m from each other. The actual condition is verified as a part of the control network upgrades. The recommendation provided in the applicable technical regulations that the control network’s condition should be inspected and the control points’ coordinates should be updated on as-needed basis is correct from a factual and technical standpoint, but ambiguous. The lack of a clearly defined criterion is often exploited by the local authorities. The inspection intervals are extended for economic reasons.
The assessment of functionality of class 3 control networks requires
formulating the measures of a global assessment of the control network functionality,
standardizing the procedure of examining the control network degradation process, and
developing a method of predicting the control network degradation process and planning the update measurements.
The model of assessment of control network functionality presented herein is based on the reliability approach. Only the reliability-based model allows combining variables of different properties. In the issue under consideration herein, accuracy is provided in metric units, while the technical condition and the availability of monuments are without unit. The theoretical background of the functionality model is provided in ref. [6]. An example of the application of the model in studying vertical control networks is provided in ref. [7]. In this study, the reliability model is used in the analysis of the horizontal controls degradation process. As in all considerations of reliability of a structure, an important element of the study is the statistical analysis of functionality of horizontal controls. The authors have been conducting this study since 2016 on control nets located in different parts of the Lodz and Kielce regions.
2 Data acquisition in horizontal control network functionality studies
In the proposed functionality analysis method, the control network “wear” process is described by two variables: usability and stability [6,7]. The geodetic control points stabilized in the field with monuments perform their task provided that they are in good working condition and the coordinates are stable. In practice, good working condition does not always qualify a control point as meeting the measurement requirements. This is the case for control points established close to the walls, in forests, shrubbery, marshes, restricted areas, on considerable depth, etc. It should be pointed out that in the case of doubt or the need to conduct additional measurements using traditional methods, a surveyor usually seeks another control point. In this context, usability is a more generalized feature than the working condition, as it provides for both the condition of the monument and the possibility of taking a measurement. Consequently, for the reliability-based approach, qualification is arbitrary and, in each case, binary.
Stability data are acquired from the results of the control measurement. This type of measurement is usually taken using kinematic techniques (RTK and RTN) on at least two geodetic control points located not farther than 5 km from the measured control points. The line vector of coordinate’s difference fXY, determined based on the control measurement, must not exceed 0.12 m [2]. The result of the control measurement is affected by the error or primary and current measurements and various other factors that are usually impossible to identify. In the study results presented herein, the impact of the measurement error was ignored, arguing that for the RTK GNSS measurement, the error does not exceed 1–3 cm, with the acceptable fXY deviation of 0.12 m.
3 Theoretical background of the functionality study outcomes analysis
In the technical analysis, reliability is usually defined as the probability that an object meets specified criteria over a period of time [t0, t] of system operation [8,9,10]. The concision of assessment of the quality of the whole system with a single characteristic is one of the key advantages of the reliability-based model. A less advantageous feature of this approach is the need to gather data through research tests conducted on large sets.
The functionality model is defined by three functions, i.e., the reliability function R(t), the failure risk function (hazard function)
Function R(t) is related to function F(t), which defines the random stability life of the object [6].
where tN is the time of operation of the object. By definition, the function takes the following form:
After transformation (3), the risk function λ(t) is defined by the relation:
On the model identification stage, depending on the type and the properties of the available data, one of the functions above is applied, i.e., R(t), F(t) or λ(t). The most frequently determined function is the risk function λ(t), whereby in practice, it is usually assumed that:
The assumption that λ = const is a simplification, as the intensity of the destruction process varies in different periods of time. However, in the case of a study of the control network functionality, we have only one information, i.e., the total number of geodetic monuments that meet the usability and stability criteria in the period of time since the last upgrade. The value of variable λ is determined after transforming the survival function R(t).
The model is identified in two ways. In the first way, the functionality of the individual control points is assessed based on the statistical set in which each element is the resultant of usability and stability. In such cases, the value of risk λ is determined from the following relation:
where Tp is the period of study from baseline (no. of years), Np is the number of geodetic control points according to the catalogue, and np is the number of control points that meet the requirement of both usability and stability.
An alternative method is based on separating the stability and usability tests [6,7]. In such case, the outcome of the test are two independent data sets and the probability of meeting the criteria of usability Pu and stability Ps determined on the basis thereof. Since the system is functional, if both conditions are met at the same time, the following equation is obtained [10]:
After taking the log of equation (8) and considering the relation (7), the resultant risk value λp is determined as the sum of the components λu (usability) and λp (stability).
In this case, the components λu and λs are determined separately based on the probabilities Pu and Ps.
In practice, the method based on separate testing of usability and stability is less frequently used.
From a practical standpoint, the key element of the functionality analysis is the determination of the number of years Tkr after which the control network no longer meets the functionality criteria. In the authors’ opinion, two critical functionality states should be distinguished, i.e., the first “warning” state when R(Tkr1) = Pkr1 = 75% and the second when R(Tkr2) = Pkr2 = 50%. The value of Tkr is determined by the following relation:
4 Example of functionality analysis of the class 3 control network
4.1 Survey results
The analysis procedure was illustrated using the example of a class 3 control network located in the southern part of the Lodz Region. The upgrade and update measurement of the network were performed in 2007. The functionality analysis tests were performed in 2017 on 124 control points. The results of the survey for the purpose of the usability assessment are presented in Table 1.
Class 3 control network survey results
No. of points according to catalogue | Control points existing in the field | Destroyed control points | ||
---|---|---|---|---|
Identified control points | Unavailable control points | Control points in good working condition | ||
124 | 90 | 0 | 90 | 34 |
On the geodetic control points, which were in good working condition, the control measurement of coordinates was performed using the RTK GNSS method and the VRSnet reference stations net. It was determined that a substantial portion of the control network, i.e., 26 control points, failed to meet the criterion of acceptable deviation fXY ≤ 0.12.
4.2 Control network functionality prediction and critical states
Of the initial number of control points Np = 124, the requirement of both usability and stability was met by 64 points. The risk value λ was determined from formula (7) for Tp = 10 years, Np = 124, np = 64, λ = 0.0631/year.
Based on the survival function (3)
the prediction of the degradation process of the control network in question was determined for three subsequent 5 year operation periods (Table 2, columns 3–5).
Destruction process prediction for the control network in question and the critical states of functionality thereof
Initial state | Control measurement | Functionality prediction | Critical states | ||||
---|---|---|---|---|---|---|---|
2007 | 2017 | 2022 | 2027 | 2032 | Pkr1 | Pkr2 | |
1 | 2 | 3 | 4 | 5 | 6 | 7 | |
T [years] | 0 | 10 | 15 | 20 | 25 | ||
R(t) | 0 | 0.532 | 0.388 | 0.283 | 0.207 | 0.75 | 0.50 |
Number of functional control points | 124 | 66 | 48 | 35 | 26 | 93 | 62 |
4.3 Statistical interpretation of the control measurement results
The statistical analysis of the results of measurement of the coordinates of the control points is not an integral element of the functionality assessment. It is cognitive in nature, and its purpose is to identify the statistical properties in the set of deviations fX, fY determined as the differences between the PL-2000 system coordinates and the results of the control measurement.
Conducting a statistical analysis is justified only for data meeting the requirement of fXY ≤ 0.12. The values that failed to meet the requirement were removed from the data set. Table 3 presents the frequency distribution of linear deviation fl vectors after separating eight class intervals.
Summary of the mean values of azimuths and modules of linear deviations fXY
Interval | Interval range (g) | Number of data points in an interval | Mean azimuth value (g) | Mean fXY module (m) |
---|---|---|---|---|
1 | 2 | 3 | 4 | 5 |
1 | 0–49.9 | 4 | 31.4717 | 0.0562 |
2 | 50–99.9 | 5 | 78.7921 | 0.0774 |
3 | 100–149.9 | 6 | 123.4944 | 0.0704 |
4 | 150–199.9 | 6 | 176.8879 | 0.0595 |
5 | 200–249.9 | 19 | 219.5562 | 0.0774 |
6 | 250–299.9 | 26 | 272.7967 | 0.0754 |
7 | 300–349.9 | 22 | 318.4120 | 0.0603 |
8 | 350–399.9 | 2 | 358.7792 | 0.0750 |
The data presented in Table 3 and the radar charts plotted on the basis thereof (Figure 1) show the distribution of the vectors of linear deviations fXY. The distribution of linear deviations fXY vectors is not even; the number of observations in the 200–300 G azimuths interval is much higher than in other sectors. Such a prominent difference in the number of data points indicates a systematic error. However, the conclusion of the significant impact of the systematic factor is not supported by the radar chart. The mean values of fXY modules calculated for individual sectors do not show significant differences (Table 3, column 5).

Histograms of azimuths of fXY vectors and their mean values.
To identify the statistical properties of the data set, a correlative dependence analysis was performed. The following were determined:
mean values and standard deviations of variables fX, fY,
correlation coefficient from the value of variables fX, fY,
linear regression functions, and
standard deviation ellipse.
The results of the analysis are presented in Table 4 and Figure 2.
Statistical analysis of the results of the control measurement
Statistical value | fX (m) | fY (m) |
---|---|---|
Mean value (m) | −0.012 | −0.020 |
Standard deviation (m) | 0.044 | 0.057 |
Linear regression function coefficients | 0.0852 | 0.14445 |
Correlation coefficient | 0.112 | |
Standard deviation ellipse (m) | b = 0.045, a = 0.055 |

Standard deviation ellipse of fX, fY vectors meeting the requirement of fXY ≤ 0.12.
The analysis shows that deviations fX and fY are not correlated although the observations have a minor systematic error. Once the error has been filtered out, the data will have the properties of random variables. The standard deviation ellipses before and after transformation are virtually identical.
5 Class 3 control networks functionality studies in the Lodz and Kielce Regions
The class 3 control network functionality studies conducted by the authors aims, on the one hand, to determine the scale of the destruction issue, and, on the other hand, to identify the patterns of this process relevant for surveying practice. The studies are conducted since 2017 in the Lodz and Kielce Regions (Figure 3) and follow a single program using a sample of 70–170 control points. Table 5 provides the basic information on the studied control networks, i.e., the object code (col. 1), measurement dates: initial and control measurement (col. 2), the number of control points: the number of points in the catalogue/number of points on which the control measurement was performed/the number of points meeting the requirements of fXY ≤ 0.12 (col. 3), the urbanization of the area in which the studied control network is located (col. 4) and the reference stations net (col. 5).

Positions of the objects in the Lodz and Kielce regions.
Study objects
Object code | Dates of control network measurement | Number of control points | Area urbanization | Reference stations network |
---|---|---|---|---|
1 | 2 | 3 | 4 | 5 |
A | 2012/2018 | 70/62/49 | Municipal area | ASG-EUPOS |
B | 2007/2017 | 124/90/64 | Rural area | VRSnet |
C | 1981/2016 | 169/67/50 | Municipal area | TPI Net |
D | 2006/2018 | 107/66/59 | Municipal area | ASG-EUPOS |
E | 1977/2016 | 149/84/76 | Rural area | ASG-EUPOS |
F | 1998/2018 | 121/65/60 | Municipal area | ASG-EUPOS |
G | 1997/2017 | 156/100/59 | Rural area | VRSnet |
H | 2000/2017 | 158/80/65 | Municipal area | VRSnet |
The control measurements were performed using the RTK GNSS method, referencing various reference stations networks, as per the recommendations provided in the technical regulations [2]. In the event of unfavorable conditions, which could affect the reception of satellite signals, the measurement session was extended as appropriate. Furthermore, for the study purposes, for a number of control points, measurements were taken with reference to the reference stations net other than provided in Table 5. Both in the case of extended measurement sessions and the use of different reference systems, the maximum discrepancies of the satellite measurement results did not exceed 0.03 m.
The observation results then underwent analysis identical in terms of scope and method as applied to object B presented in item 4. First, the observations exceeding the linear deviation of 0.12 m were excluded from the analyzed set. It should be emphasized that such deviations were found in all analyzed data sets. The number of control points provided in column 4 in Table 5, e.g., 149/84/76 ,means that the control measurement could be performed only on 76 points.
The analysis results summarized in Table 6 and shown in Figure 4 show a number of statistical patterns:
In all cases, the mean values of deviations fY are negative. The data sets are shifted slightly westward. The result correlates with the size charts provided on the radar charts (Figure 4), whereby on the latter one, the systematic impact is much more prominent.
The variables fX and fY are not correlated. The correlation coefficient did not reach the value, indicating the presence of a correlative dependence in any of the analyzed samples.
The standard error calculated for variables fX and fY, and ellipse semi-axes show only minor differences.
Statistical analysis of the results of the control measurement
Object no. | Number of points | Mean values | Standard deviation | Correlation coefficient | Azimuth of semi-axis A (g) | Semi-axes of ellipses | |||
---|---|---|---|---|---|---|---|---|---|
fX (m) | fY (m) | σjX (m) | σjY(m) | A (m) | B (m) | ||||
A | 49 | −0.005 | −0.006 | 0.022 | 0.023 | −0.12 | −7.87 | 0.022 | 0.022 |
B | 64 | −0.012 | −0.020 | 0.044 | 0.057 | 0.11 | 7.31 | 0.045 | 0.055 |
C | 50 | 0.023 | −0.014 | 0.054 | 0.049 | 0.165 | 10.46 | 0.055 | 0.048 |
D | 59 | 0.013 | −0.008 | 0.049 | 0.043 | −0.19 | −12.28 | 0.050 | 0.041 |
E | 76 | 0.023 | 0.003 | 0.036 | 0.040 | 0.19 | 12.27 | 0.038 | 0.039 |
F | 60 | 0.005 | −0.029 | 0.035 | 0.039 | −0.10 | −6.07 | 0.035 | 0.038 |
G | 59 | 0.006 | −0.050 | 0.041 | 0.039 | 0.01 | 0.21 | 0.040 | 0.039 |
H | 65 | 0.012 | −0.030 | 0.039 | 0.038 | 0.12 | 7.48 | 0.040 | 0.037 |

Examples of standard error ellipses and frequency radar charts.
6 Prediction of the functionality destruction process of the analyzed class 3 control networks
Table 7 summarizes the outcomes of the functionality prediction calculated for three subsequent 5 year operation periods and the years in which functionality reaches critical values (11). It should be noted that the first state, i.e., the alarm critical state, was not exceeded only for object A. The second critical state was exceeded for all analyzed data sets.
Prediction of critical functionality states of analyzed objects
Object | λ | Initial measurement | Number of functional control points | Critical states | |||||
---|---|---|---|---|---|---|---|---|---|
Date | Number | 2018 | 2023 | 2028 | 2033 | 75% | 50% | ||
A | 0.059 | 2012 | 70 | 49 | 37 | 24 | 18 | 2020 | 2024 |
B | 0.063 | 2007 | 124 | 62 | 45 | 33 | 24 | 2015 | 2019 |
C | 0.035 | 1981 | 169 | 46 | 39 | 32 | 27 | 1995 | 2002 |
D | 0.056 | 2006 | 107 | 55 | 41 | 31 | 24 | 2015 | 2019 |
E | 0.017 | 1977 | 149 | 74 | 68 | 63 | 58 | 2006 | 2021 |
F | 0.056 | 1998 | 121 | 40 | 30 | 23 | 17 | 2007 | 2011 |
G | 0.047 | 1997 | 156 | 58 | 46 | 36 | 29 | 2008 | 2013 |
H | 0.054 | 2000 | 158 | 60 | 46 | 35 | 27 | 2009 | 2014 |
Based on the data in Table 6, a general conclusion can be drawn on the condition of the control networks and a detailed one on the intensity of the destruction process in different regions. The risk variable λ fluctuates around the mean value of 0.046 between the extreme values of 0.063 and 0.017. With the exception of the extreme values, the risk variable does not show significant variation. The significant deviation of object E can be explained by the exceptionally high local investment activity (central districts of Lodz city).
7 Final remarks and conclusions
7.1 Identification of the functionality model
The presented method of functionality assessment is a coherent solution in terms of the test purpose, an unambiguous criteria expressed in the form of probability interpreted according to the reliability engineering theory and data acquisition procedures as well. Only the reliability approach integrates different properties such as usability and stability in one model.
The critical state level is a questionable element of the method. The correct indication of critical probabilities provides a rational basis for the decision concerning the date of maintenance actions. The authors suggest introducing two critical functional states at the levels Pcr1 = 75% and Pcr2 = 50%.
The destruction of the control network is influenced by two factors. The main one is the physical destruction of network benchmarks. Since the cause of destruction is the investment activity necessary for the functioning of the economy, therefore, the solution to this problem depends on decisions made by regional surveying departments and local administration. Technically, the problem is solved by supplementing the existing network and new measurements.
The presented method of evaluating functionality can be used regardless of the structure and the number of points. An optimal solution is to make an inventory and control check measurement for all control network points stabilized in a specified area, e.g., in the area of a commune. In case of significant number of points, the survey may be of statistical nature. Authors' experience has shown that achieving a reliable result requires testing a minimum of 100 points. The measurement should be carried out with a standard error σp ≤ 0.03 m, i.e., at least twice as high as the accuracy of the coordinates specified in technical regulation [1,2].
According to the authors, the scope and the detail of the research carried out entitles to conclude that the presented procedure can be adopted as a standard procedure, useful in the assessment of the quality of regional geodetic resource databases.
7.2 Statistical properties of the destruction process of the class 3 control networks
The problem of evaluation of horizontal control networks functionality in the article is presented on the example of class 3 control networks, which in Poland are stabilized by means of permanent markings. The local characteristics of these networks follow from the fact that the current coordinates of points in the “2,000” system are the result of the transformation of coordinates originally calculated in another reference system (“65”). The main conclusion is that the level of network destruction is significant and is dependent on the exploitation period. Changes in coordinate values exceeding the critical values usually affect some percentage of points. But the resultant value of the risk parameter λ is always significant, on average λ = 0.046.
The measurement results presented in Table 6 and Figure 3 indicate that the coordinates are influenced by a systematic factor. Asymmetry of the distribution of the number of deviations fXY is visible in all test results. The direction of the translation vector is approximately consistent with the Y-axis. The value of translation and standard errors of the variables fX, fY confirm the opinion that the accuracy of transformation of the primary system to the system “2,000” is within the limits of 0.05 m. Since it is impossible to indicate whether the observed coordinate differences are the result of an invalid primary measurement or due to unrecognized factors, it is optimal to update the network in larger areas. Currently, such corrections are carried out locally in accordance to the investment tasks.
In the analysis of the functionality issue, a research workshop is important. The coordinates of network points were determined using the GPS kinematic technique combined with ASG-EUPOS, VRSnet and TPInet reference station networks. To estimate the accuracy of the determined coordinates, some of the points were observed with extended observation time or in connection with another reference network. The standard error determined on this basis is similar for all objects, approximately 0.02 m.
7.3 Modernization of control networks by means of satellite measurement techniques
The high level of destruction and maintenance costs of networks on the one side and the effectiveness of satellite measurements on the other become rational arguments for the lack of acceptance for static control nets [11,12]. Currently, in the opinion of the authors, this is a premature opinion, although optimization of the methods of design and maintenance of class 3 control networks is necessary and possible taking into account local conditions. On the one hand, databases of class 3 control networks available in Polish regional documentation centers are components of the state surveying and cartographic resource [3,4]. These databases have an important role in the functioning of various segments of economy and administration. On the other hand, from a technical point of view, permanent signs are necessary in areas beyond the range of permanent reference stations, in densely built-up areas, in areas where it is not possible to effectively distribute GPS adjustment corrections via the GSM network or due to significant land surpluses also the UHF radio communication, etc.
The results of this study confirm the necessity to rethink the approach to the problem of networks' functioning and indicate the directions of these changes. In the opinion of the authors, the modified approach should be complementary, i.e., take into account the network structure, number of points and coordinate measurement methods. The main postulate of the proposed concept is to replace the network with a set of autonomous points. Local connections of adjacent points would be made by means of classical measurements, but the latter would only have a check character. The planning of location and number of points should take into account the process of destruction. The level of destruction can be assumed on the basis of the analysis of critical states determined by means of a functionality model. Such assumption will significantly increase the number of network points.
An important element of the proposed concept is to measure the coordinates of network points. Within this task it is possible to use differential GNSS positioning, precise point positioning (PPP), linear-angle measurements and hybrid methods integrating different techniques. The presented research results show that at the stage of control measurements sufficient accuracy is provided by the kinematic technique. When establishing a network, measurements should be carried out using static methods in accordance with the recommendations [1], but practice proves that under favorable conditions, kinematic techniques are also satisfactory. In Poland, measurements using differential GNSS method are possible thanks to several systems of reference stations, mainly the ASG-EUPOS system.
An alternative to differential measurements is technique of precise satellite positioning using a global fixed station infrastructure [13,14,15]. The advantage of the absolute PPP method is its autonomy. The measurement is performed without the need to relate to regional reference stations, while access to the GNSS (IGS) data on GNS and GLONASS is necessary. The PPP method is still a subject of research, and its accuracy depends on the length of the session and IGS data [16] The results in the range of 0.02–0.03 cm achieved with sessions of about 2–3 h can be assumed as sufficient for class 3 network measurements. The accuracy requirements for coordinate measurements are also met by Smart Station technology integrating satellite measurements with classical measurements [17]. It can be assumed that this technique will be particularly useful at the stage of control measurements, as it gives the possibility to control both the station and the adjacent points.
Acknowledgments
The project is supported by the program of the Minister of Science and Higher Education under the name: “Regional Initiative of Excellence” in 2019–2022 project number 025/RID/2018/19 financing PLN 1,20,00,000.
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© 2020 Bogdan Wolski and Grzegorz Granek, published by De Gruyter
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- 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
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