Abstract
Classification is the science that arranges organisms in groups according to their similarities and differences. In plant science, there are many aspects of classifications. For instance, there is morphological, anatomical, palynological, molecular, and chemical classification. All these types consume time, effort, and money. In this research, new technology is tested to identify the differences between plants. Spectroradiometer will help in classifying Prosopis juliflora (Sw.) DC in Bahrah region in Saudi Arabia. Spectroradiometer technology is applied to a sample of 40 taxa of P. juliflora in two different seasons. Within each sample site, measurements were taken at a high sun angle from 10:00 am to 2:00 pm. Results showed that spectroradiometer indicated the existence of significant differences among P. juliflora taxa. Correspondingly, the spectroradiometer engenders the spectral responses of the targeted species in the region between 400 and 2,500 nm wavelength. The spectral behavior of P. juliflora in four seasons was demonstrated as season dependent. The variance-based principal component analysis divided the investigated samples into two groups, either positively correlated or negatively correlated according to the seasonal data collection. Sample number 5 in the quantile’s slicing analysis maintained a stable behavior when it was exposed to 100% wavelength. P. juliflora behavior was stabilized in the infrared (IR) samples (4,5), the shortwave IR (SWIR) (3,4,5), and thermal IT (TIR) (3,4,5,6) at the quantile range of >75. While in the quantile range <25, we found the stability behavior in the IR samples (2,8,10), the SWIR (2,7,8,10), and in TIR (2,7,8,10). Therefore, this approved that the spectroradiometer is useful as the first classification process. More studies are needed to support this finding, such as chemical and molecular investigations.
1 Introduction
Remote sensing plays a role in understanding these phenomena. Remote sensing gives a lot of information about plants, and the definition illustrates the finding or measuring plant physical, biological, biochemical, or phonological attributes that denote a plant’s functional acclimatization, which otherwise reveal the underlying plant ecophysiological processes [1,2]. Other numerous features are pertinent to any discussion of identifying vegetation function with remote sensing, including spatial, spectral, temporal, and biological scopes.
Imaging spectrometers (instruments that gather hyperspectral data) breakdown the electromagnetic spectrum into sets of bands that categorize objects through their spectral properties on the surface of the earth. Hyperspectral data consist of various bands, approximately hundreds of bands, which also include the electromagnetic spectrum [3,4,5]. Hyperspectral remote sensing, also referred to as imaging spectroscopy, is recently investigated by researchers and professionals to find and identify the terrestrial flora [6,7,8]. Several ecological applications can benefit from hyperspectral remote sensing, for instance, measuring chlorophyll, leaf water, cellulose, pigments, lignin along with other uses in agriculture, astronomy, chemical imaging, remote sensing [9,10,11].
Components of biodiversity, which are widely varied in vegetations cover form related biological systems in the Saudi Arabia welfare structure. Studies have indicated contrasts in plants of one physical category because of the distinction of substance and physical properties inside the plant [12,13]. The vegetation structure gave a few contrasts in its spreading conduct in various places in the Kingdom, which can be related to climatic condition changes, water sources, and anthropogenic weights along the rising slope, as reported by Hegazy et al. [14].
Hyperspectral remote sensing applications were continuously developed over the past four decades to add more insights into the natural vegetation behaviors and agricultural practices [15]. Recently, significant scholarly works describe in detail the concept of the ground-based and handheld remote sensing platforms that improved natural vegetation mapping [16,17,18,19,20]. Moreover, data dimensionality and data redundancy are not limiting factors in using hyperspectral data as it was before which led to swift enhancements in hyperspectral remote sensing applications [21,22]. Band selection in hyperspectral data mining is an essential prerequisite to optimize data efficiency and reduce the computational timing [23,24].
Several publications had discussed the hyperspectral sensors on different platforms and their applications. Specifically, handheld spectroradiometers such as analytical spectral devices (ASD) were used extensively in natural vegetation mapping, among other several applications [18,25,26]. ASD spectroradiometers operate generally from 400 to 2,500 nm in a very narrow range of 1 nm bandwidth interval (high-resolution ASD) up to 100 nm bandwidth intervals (low-resolution ASD). Detailed and accurate mapping of natural vegetation and plant taxonomical models was achieved using the thermal infrared (TIR) spectrum [27,28]. The new generation of the hyperspectral sensors such as spatially enhanced broadband array spectrograph system will expand the resources and the interpretation of the hyperspectral remote sensing data [29,30].
In line with Alfarhan [31] and Thomas et al. [32], vegetation species in Saudi Arabia are divided into three general categories, namely, species of the Sudano–Deccanian zone, Saharo–Sindian zone, and Tropical Indian–African categories. The annual average rainfall in the northwestern regions of Saudi Arabia differs from 30 mm in the northern areas to 90 mm in the northeast. Rainfall records in the central region of the Kingdom, mainly in the Riyadh region, indicate that rainfall is increasing from South to North and from East to west, ranging between 100 and 85 mm annually. Generally, the annual average rainfall is less than 100 mm and most of it is in December, January, February, and March and considerably helps for the growth of short-lived vegetation.
Many scholarly works had been published on the flora of Saudi Arabia. According to El-Sheikh and Yousef [33], Mandaville and Mandaville [34], and Thomas et al. [35], the most comprehensive works are two flora books: the first is Flora of Saudi Arabia written by Migahid et al. [36] and published four times. The second is the Flora of the Kingdom of Saudi Arabia written by Chaudhary [37]. Several studies were conducted in different regions of Saudi Arabia such as Batanouny [38] and Aldhebiani et al. [39] who studied the vegetation and floras of the sabkhas, hillocks, and other prominent mountains of the Najd region, such as Tuwaiq, Aja, and Salma. Considerable efforts have also been made toward the elucidation of vegetation–environmental relationships in the ecosystems “raudhas” or depressions [40,41,42]. The plant communities of Wadis have been addressed in some studies such as Wadi Al-Ammaria [43] and Wadi Hanifa [44]. The Prosopis juliflora species, in the Kingdom of Saudi Arabia, is endangered due to their limited genetic range and geographical variety, minor population size, short density, threatening ecological conditions, and unselective tree cutting, regardless of the truth that these species have a great reproductive ability [45,46,47].
In the study area considered in this research, Bahrah, west of Saudi Arabia, no studies have been endeavored to classify P. juliflora species using different wavelengths. The current study addressed the consideration of hyperspectral data in intraspecific variation in P. juliflora (Sw.) DC, Saudi Arabia, to identify the significance of different responses of the P. juliflora taxa to different spectral wavelengths such as visible spectrum, short-wavelength IR, long-wavelength IR, and TIR. The study goal is to investigate the impact of different wavelengths on different leaf samples collected from different P. juliflora taxa to study their spectral signature behavior and to appraise the impact of these different wavelengths on these species’ occurrence.
2 Materials and methods
2.1 Study area description
The climate of Saudi Arabia is classified as an “arid climate” within Thornthwaite’s global climatic classification, and as “dry climates” in Koppen’s classification [48,49]. According to Juneidi and Huss [50], relative humidity is normally low excluding the coastal areas, where it touches above 90%. The annual average temperature is virtually 33.4 and 14°C in summer and winter, respectively. Hot weather describes the Kingdom’s climate for the larger part of the year. The north winds move from the eastern Mediterranean in the direction of the Arabian Gulf with some extensive variations [51]. Spectral data are gathered in the Bahrah region, 21.392245°N, and 39.472352°E. Bahrah is located on Tihama plateau closer to Wadi Fatima between Jeddah and Makkah (Figure 1). The climate in Bahrah Dafi is mild in summer and rainy in winter. The average summer temperature is reported as 33°C and the average rainfall is 520 mm. The greatest amount of rainfall is in January and the lowest amount is in July [52]. Inside the study region, different sites have been chosen as samples in an exploration tour preceding the beginning of the arena campaign for the gathering of spectral data. The arena campaign commonly has a multitemporal framework, gathering spectra from diverse sorts of plants at diverse phenological periods and different periods of the year [39].

The location of the study area sampling site disclosed Bahrah area.
2.2 Field sampling
The spectroradiometer is plugged into the Ethernet cable and ends with a pistol to measure the spectrum and wave oriented. The Spectralon® White Reference panel [53] is installed for utilization and handling of the diverse segments, and the panel is in black to decrease the scattering of the related radiance (Figure 2).

Pictures showing the mechanism of work (1) plant leaves, (2) black plate, (3) spectroscopy, (4) white reflector, (5) measured by pistol, and (6) transfer of data to the laptop.
The leaves of P. juliflora were cut from several trees in different seasons where the tree is about 2 m long. More than 40 samples in every sample site were calculated at a high sun angle, from 10 am to 2 pm by spectroradiometer technology. The following are the fundamental steps followed in undertaking two experiments on P. juliflora species:
P. juliflora leaves were collected from 10 trees of which two samples were taken at different seasons.
Other samples were collected from the plant to chemically measure them in addition to the soil.
Leaves of the plant were weighed in the wet content and then dried. After drying, the leaves were weighed in dry wax to determine the water content.
Dry leaves were measured by spectroradiometer, and data collected from the files of spectral data were transferred as a format of ASCII text by applying the software of ASD ViewSpec Pro.
2.3 Hyperspectral data processing
Spectral varieties with extreme noise at the final point of the spectrum, from 2,350 to 2,500 nm, and with obvious robust climatic intervention, that is 1,351–1,449 nm and 1,801–2,029 nm, were discarded from the investigation. Accordingly, the spectral data were modified for steps, i.e., sudden alterations of the noted reflectance that took place in the spectral signatures at 1,000 nm, which is typical for the instrument utilized, as a result of the instrument sensitivity drift. The shortwave IR (SWIR) portion of the spectrum, ranging from 1,000 to 1,800 nm, was considered as a corrections’ reference since it is constant to the instrument’s sensitivity drift [54,55]. To conclude, the spectral data are saved with the auxiliary metadata in a uniform, accessible to track method [56].
Figure 3 shows the behavior of the natural vegetation to different electromagnetic wavelengths. For the visible spectrum, that is, from 1 to 395, the plant taxa do not reveal any significant difference. For the long-wavelength IR, that is from 442 to 1,079, the taxa reveal a significant difference among the species. In its response to the SWIR, that is, from 1,128 to 1,569, the plant taxa reveal only one sample differs from others. For the TIR, that is, from 1,618 to 2,108, the trees reveal that two of the samples are similar in their behavior to the TIR and one sample differs from them in its response to the TIR wavelength.

Vegetation behavior subjected to a different spectrum of a different wavelength.
2.4 Principal component analysis (PCA)
The PCA is used to transform a set of likely correlated to unlikely correlated variables. The principal component number is less than or equal to the variables’ original number. According to Lorenz [57] and Jolliffe and Cadima [58], the PCA’s fundamental equations are described as follows:
To maximize variance, the first weight vector w (1) thus has to be satisfied equivalently, and writing this in matrix form gives
Since w (1) has been defined to be a unit vector, it also equivalently satisfies to be calculated as follows:
The Kaplan–Meier estimator, also known as the product-limit estimator, is a nonparametric statistic used to estimate the survival function from lifetime data, survival estimates, exploratory plots with optional parameter estimates, and a comparison of survival curves when there is more than one group, using designated sample data table [59,60]. The summary report gives estimates for the mean survival time as follows:
With t i is the time when at least one event happened, d i the number of events that happened at time t i , and n i the individuals known to have survived (have not yet had an event or been censored) up to time t i .
2.5 Statistical functions
Quantile analysis is a binary form of spectral data classification, which Khan et al. [61] used to improve the algorithm performance as a functional gradient descent (FGD). The generic form of the FGD is valid to analyze high spectral data precisely throughout a direct data interpretation.
Where
Q τ (Y) is the τth quantile of Y,
ρ τ (r) is the conditional function
While the τth conditional quantile of Y given x be f(x) for a given quantile estimation:
The functions with Col prefix compute statistics for a column of numbers or expressions which specifically includes the mean, quantile, range, maximum, and minimum. The Col quantile functions of Bassett Jr and Koenke [62], represent the quantile percentage divided by 100. The 25% quantile, also called the lower quartile, corresponds to p = 0.25, and the 75% quantile, called the upper quartile, corresponds to p = 0.75. In general, to define the quantile that corresponds to the fraction p, linear interpolation between the two nearest pi is used. According to Ashkar and Ouarda [63], if p lies as a fraction of f from pi to pi+1, then pth quantile is defined as:
As special cases, define the median and quartiles by:
Median: Q (5)
Lower quartile: Q (25)
Upper quartile: Q (75)
The function Q defined in this way is called the quantile function.
3 Results and discussion
In the current study, the ASD spectroradiometer illustrates the different spectral signatures over the visible, near infra red (NIR), and SWIR spectral bands [64]. Correspondingly, the spectroradiometer engenders the spectral responses of the targeted species in the region between 400 and 2,500 nm wavelength. Figure 4 shows the spectral behavior of P. juliflora in four seasons and different periods in terms of wavelength against reflection by ASCII text accompanied by the software of ASD ViewSpec Pro.

The wavelength vs reflectance of Prosopis juliflora, (a) result collected in Feb. 2019, (b) result collected in Sep. 2019, (c) result collected in Nov. 2019, and (d) result collected in Feb. 2020.
The results of the PCA were illustrated in Figure 5. Principally, Figure 5a shows the variance-based PCA of the ten different sample indicators where the analysis was divided into two groups. The first group involves the positive samples of S4–S5–S6–S7–S9, and the negative group involves the samples S1–S2–S3–S8–S10. While Figure 5b shows the variance-based PCA collected in summer. The ten different sample indicators were divided into two groups: the first group involves the positive samples of S1–S5–S4, and the negative group involves the samples S2–S3–S6–S7–S8–S9–S10. Figure 5c shows the variance-based PCA where the ten different sample indicators were also divided into two groups. The first group involves the positive samples of S1–S3–S4–S5–S6, and the negative group involves the samples S2–S7–S8–S9–S10. Finally, Figure 5d shows the variance-based PCA collected in winter 2020, and the ten different sample indicators were divided into two groups according to the correlation coefficient value [65].

Principal component analysis. (a) Result collected in Feb. 2019, (b) result collected in Sep. 2019, (c) result collected in Nov. 2019, and (d) result collected in Feb. 2020.
Spectral information collected from the vegetative covers is generally indicated as a difference in the molecular character of the designated targets. Divergence data were a gradually changing wavelength function; therefore, it gives data that are not likely interconnected with any spectral calculations carried out in a system [66,67]. The analysis of the hyperspectral image, during the previous decade, had developed into one of the best potent and wildest rising technologies in the area of remote sensing [68,69].
The first group involves the positive samples of S1–S4–S5–S6, and the negative group involves the samples S2–S3–S7–S8–S9–S10. PCA is a statistical process that aims to increase the interpretation of information by using JMP Statistical software.
Classification of different indicators was possible because of PCA, which identifies the similarities and differences in all samples [70]. The abovementioned sample (a–d) represents the grouping to different indices according to PCA on covariance [71,72]. The samples were categorized into two positive and negative groups, but it was not precisely determining the behavior; and to ensure that a quantitative segmentation analysis of the samples was performed for further clarification [2].
Table 1 shows the quantiles’ slicing for the four periods (T1, T2, T3, and T4.) where the data was extracted by equations 5–7. The table was divided from 0.00% (min value) to 100% (max value), while the median specifies the 50% of the recorded reflection values. Interpreting the data in the tables maintained the stability behavior of the tested sample when it was exposed to different wavelengths reflecting from 0 to 100%; while between 75 and 25%, the targets had other interpretations that will not be further addressed.
Quantiles slicing analysis of Prosopis juliflora
(a) Result collected in Feb. 2019 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
T1 | S1 | S2 | S3 | S4 | S5 | S6 | S7 | S8 | S9 | S10 | |
100.0% | Max | 0.75998 | 0.65156 | 0.81047 | 0.90976 | 0.95114 | 0.80032 | 0.69253 | 0.64990 | 0.73011 | 0.62004 |
99.50% | 0.75986 | 0.64914 | 0.80926 | 0.90113 | 0.94337 | 0.79788 | 0.69114 | 0.64752 | 0.72403 | 0.61734 | |
97.50% | 0.75751 | 0.63724 | 0.80447 | 0.86081 | 0.92110 | 0.79377 | 0.68352 | 0.63778 | 0.70568 | 0.60085 | |
90.00% | 0.74176 | 0.62384 | 0.78557 | 0.82587 | 0.89004 | 0.78389 | 0.66912 | 0.62448 | 0.67442 | 0.59059 | |
75.00% | Quartile | 0.68538 | 0.57103 | 0.68073 | 0.69554 | 0.77031 | 0.72146 | 0.59955 | 0.56141 | 0.56621 | 0.53662 |
50.00% | Median | 0.50901 | 0.43752 | 0.59829 | 0.58616 | 0.68110 | 0.55920 | 0.45518 | 0.41819 | 0.43792 | 0.44694 |
25.00% | Quartile | 0.27738 | 0.23438 | 0.34390 | 0.33800 | 0.39047 | 0.35005 | 0.23090 | 0.20595 | 0.27646 | 0.24444 |
10.00% | 0.10298 | 0.06157 | 0.09557 | 0.08594 | 0.14111 | 0.06420 | 0.04543 | 0.04423 | 0.07407 | 0.05090 | |
2.50% | 0.05642 | 0.03849 | 0.06217 | 0.06146 | 0.06687 | 0.04089 | 0.02963 | 0.02855 | 0.04530 | 0.03594 | |
0.50% | 0.04618 | 0.03064 | 0.05156 | 0.05295 | 0.05663 | 0.03183 | 0.02248 | 0.02212 | 0.03889 | 0.02796 | |
0.00% | Min | 0.04553 | 0.02985 | 0.05081 | 0.05233 | 0.05564 | 0.03116 | 0.02163 | 0.02136 | 0.03823 | 0.02685 |
(b) Result collected in Sep. 2019 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
T2 | S1 | S2 | S3 | S4 | S5 | S6 | S7 | S8 | S9 | S10 | |
100.0% | Max | 0.85986 | 0.74088 | 0.82104 | 0.87244 | 0.90438 | 0.80695 | 0.79689 | 0.75318 | 0.76183 | 0.74386 |
99.50% | 0.85618 | 0.73629 | 0.81603 | 0.87002 | 0.90112 | 0.80318 | 0.79209 | 0.74861 | 0.76152 | 0.74307 | |
97.50% | 0.83777 | 0.71558 | 0.79027 | 0.85714 | 0.88149 | 0.77987 | 0.77022 | 0.72552 | 0.75886 | 0.73995 | |
90.00% | 0.81402 | 0.69792 | 0.76500 | 0.84262 | 0.86035 | 0.75707 | 0.75066 | 0.70841 | 0.74938 | 0.73010 | |
75.00% | Quartile | 0.76526 | 0.65510 | 0.70466 | 0.80040 | 0.80343 | 0.70779 | 0.70554 | 0.66460 | 0.69998 | 0.67204 |
50.00% | Median | 0.53300 | 0.53123 | 0.55533 | 0.62498 | 0.63333 | 0.56750 | 0.57015 | 0.52076 | 0.53018 | 0.52696 |
25.00% | Quartile | 0.26287 | 0.29614 | 0.29430 | 0.33539 | 0.36001 | 0.34301 | 0.31755 | 0.28662 | 0.29306 | 0.29006 |
10.00% | 0.09844 | 0.07719 | 0.06424 | 0.08227 | 0.09017 | 0.07800 | 0.07326 | 0.06695 | 0.06972 | 0.06493 | |
2.50% | 0.04116 | 0.04605 | 0.04242 | 0.05441 | 0.05710 | 0.04742 | 0.04468 | 0.04469 | 0.04062 | 0.03314 | |
0.50% | 0.03790 | 0.03979 | 0.03490 | 0.04422 | 0.04892 | 0.03970 | 0.03770 | 0.03614 | 0.03420 | 0.03029 | |
0.00% | Min | 0.03778 | 0.03934 | 0.03376 | 0.04273 | 0.04826 | 0.03862 | 0.03695 | 0.03514 | 0.03365 | 0.03015 |
(c) Result collected in Nov. 2019 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
T3 | S1 | S2 | S3 | S4 | S5 | S6 | S7 | S8 | S9 | S10 | |
100.0% | Max | 0.70374 | 0.73011 | 0.81047 | 0.81435 | 0.95114 | 0.90370 | 0.79675 | 0.67049 | 0.90976 | 0.78604 |
99.50% | 0.70338 | 0.72403 | 0.80926 | 0.81014 | 0.94337 | 0.89480 | 0.78988 | 0.66374 | 0.90113 | 0.77687 | |
97.50% | 0.70129 | 0.70568 | 0.80447 | 0.79981 | 0.92110 | 0.86173 | 0.75803 | 0.63576 | 0.86081 | 0.74285 | |
90.00% | 0.68940 | 0.67442 | 0.78557 | 0.77506 | 0.89004 | 0.82969 | 0.73032 | 0.60741 | 0.82587 | 0.71325 | |
75.00% | Quartile | 0.65968 | 0.56621 | 0.68073 | 0.68779 | 0.77031 | 0.72237 | 0.64245 | 0.50801 | 0.69554 | 0.64945 |
50.00% | Median | 0.52984 | 0.43792 | 0.59829 | 0.61097 | 0.68110 | 0.62747 | 0.55300 | 0.40682 | 0.58616 | 0.54060 |
25.00% | Quartile | 0.30735 | 0.27646 | 0.34390 | 0.38138 | 0.39047 | 0.37521 | 0.32332 | 0.24635 | 0.33800 | 0.30468 |
10.00% | 0.10666 | 0.07407 | 0.09557 | 0.11010 | 0.14111 | 0.12386 | 0.12237 | 0.07546 | 0.08594 | 0.08705 | |
2.50% | 0.06388 | 0.04530 | 0.06217 | 0.07043 | 0.06687 | 0.07701 | 0.06541 | 0.05327 | 0.06146 | 0.06216 | |
0.50% | 0.05347 | 0.03889 | 0.05156 | 0.05549 | 0.05663 | 0.06555 | 0.05936 | 0.04695 | 0.05295 | 0.05353 | |
0.00% | Min | 0.05279 | 0.03823 | 0.05081 | 0.05310 | 0.05564 | 0.06495 | 0.05911 | 0.04650 | 0.05233 | 0.05281 |
(d) Result collected in Feb. 2020 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
T4 | S1 | S2 | S3 | S4 | S5 | S6 | S7 | S8 | S9 | S10 | |
100.0% | Max | 0.69234 | 0.58137 | 0.75280 | 0.81979 | 0.88688 | 0.76428 | 0.75530 | 0.57925 | 0.71348 | 0.60727 |
99.50% | 0.69011 | 0.58013 | 0.74885 | 0.81572 | 0.88415 | 0.75961 | 0.75159 | 0.57562 | 0.71106 | 0.60582 | |
97.50% | 0.67469 | 0.57537 | 0.72466 | 0.78957 | 0.86611 | 0.73158 | 0.72878 | 0.55663 | 0.69281 | 0.59762 | |
90.00% | 0.66113 | 0.56421 | 0.70432 | 0.76716 | 0.84874 | 0.71266 | 0.70832 | 0.54513 | 0.67646 | 0.58834 | |
75.00% | Quartile | 0.63442 | 0.53596 | 0.65837 | 0.71827 | 0.79102 | 0.68320 | 0.63876 | 0.52099 | 0.64133 | 0.56869 |
50.00% | Median | 0.53035 | 0.41207 | 0.53566 | 0.61162 | 0.64247 | 0.57004 | 0.54949 | 0.38933 | 0.52360 | 0.44741 |
25.00% | Quartile | 0.29460 | 0.21123 | 0.29788 | 0.37216 | 0.34893 | 0.32017 | 0.31377 | 0.19212 | 0.29187 | 0.23656 |
10.00% | 0.13727 | 0.07522 | 0.08810 | 0.12950 | 0.12334 | 0.11725 | 0.10230 | 0.07843 | 0.10932 | 0.11082 | |
2.50% | 0.07223 | 0.05043 | 0.06347 | 0.08409 | 0.07496 | 0.07966 | 0.07260 | 0.05448 | 0.07742 | 0.05723 | |
0.50% | 0.06632 | 0.04378 | 0.05006 | 0.07126 | 0.06707 | 0.06780 | 0.06573 | 0.04855 | 0.07085 | 0.05441 | |
0.00% | Min | 0.06620 | 0.04354 | 0.04908 | 0.06992 | 0.06689 | 0.06697 | 0.06553 | 0.04842 | 0.07060 | 0.05424 |
Table 2 shows the spectral signature stability behavior of P. juliflora as clarified in the previous tables, since the spectrum behavior was stabilized in (T1) in the IR samples (4,5), the SWIR (3,4,5), and TIR (3,4,5,6) at the quantile range >75. While in the quantile range <25, we found that the stability behavior in the IR samples (2,8,10), the SWIR (2,7,8,10), and in TIR (2,7,8,10).
Spectral signature stability behavior of Prosopis juliflora
Quantiles range | Infrared | SWIR | Thermal IR | Stability behavior | |
---|---|---|---|---|---|
T1 | >75 | 4,5 | 3,4,5 | 3,4,5,6 | 4,5 |
75 > x < 25 | 1,3,6,7,9 | 1,6,9 | 1,9 | ||
<25 | 2,8,10 | 2,7,8,10 | 2,7,8,10 | 2,8,10 | |
T2 | >75 | 1,4,5 | 4,5 | 4,5 | 4,5 |
75 > x < 25 | 3,6,7,9 | 1,3,6,7 | 3,6,7,9 | ||
<25 | 2,8,10 | 2,8,9,10 | 1,2,8,10 | 2,8,10 | |
T3 | >75 | 4,5,6,9 | 4,5,6,9 | 4,5,6 | 4,5 |
75 > x < 25 | 1,3,7 | 1,3,7 | 1,3,7,9 | ||
<25 | 2,8,10 | 2,8,10 | 2,8,10 | 2,8,10 | |
T4 | >75 | 4,5 | 4,5 | 4,5 | 4,5 |
75 > x < 25 | 1,3,6,7,9 | 1,3,6,7,9 | 1,3,6,7,9 | ||
<25 | 2,8,10 | 2,8,10 | 2,8,10 | 2,8,10 |
In (T2) in the IR samples (1,4,5), the SWIR (4,5), and TIR (4,5) were at the quantile range of >75. In the quantile range of <25, the stability behavior in the IR samples was (2,8,10), the SWIR (2,8,9,10), and TIR (1,2,8,10). In (T3) at the quantile range of >75, the IR samples were (4,5,6,9), the SWIR (4,5,6,9), and TIR (4,5,6). In the quantile range of <25, the stability behavior in the IR samples was (2,8,10), the SWIR (2,8,10), and TIR (2,8,10). In (T4) at the quantile range of >75, the IR samples were (4,5), the SWIR (4,5), and TIR (4,5). In the quantile range of <25 the stability behavior in the IR samples was (2,8,10), the SWIR (2,8,10), and TIR (2,8,10).
This explains the significance of the difference in the chemical content, leaf content, or water content. This is confirmed by a study carried out by Hoshino et al. [73] and Vidhya et al. [71], which showed that the NIR reflectance of the P. juliflora leaves correlated significantly with a leaf content.
The common factor between wavelengths and reflectances is the stability behavior that was established in two groups: the first group >75, the samples were (4,5), and the second group <25 the samples were (2,8,10). These results confirm that the P. juliflora, under different ranges of wavelengths, exhibited different spectral behaviors, although there is a great similarity in the external appearance of the plant. This also confirms that the hyperspectral spectroradiometer is an effective device, as it gave a good result, and, therefore, it can be effectively used in plant classification [74].
The implementation of the FGD algorithm extended to a robust and reliable classification function of two overlapped plant samples. The plant materials under investigation belong to two different classes along the broad spectral wavelengths. The temporal analysis confirms the designation of the two groups (4 and 5, 2 and 8, and 10) which is a solid finding of the current research of P. juliflora spectral classification. The classification algorithm was performed based on labeling the class variables and the corresponding class quantiles to attain equality.
This is consolidated by the findings of the study carried by Suleiman et al. [75] which confirmed that the hyperspectral spectroradiometer is an effective device as the wavelength of numerous IR absorption bands is a definite category of chemical bonds in the leaf samples of plants [76,77] (Figures 6 and 7).

(a) The flower of Prosopis juliflora number 10, (b) the fruit (legume), (c) the leaf (compound), (d) the leaflet (compound), and (e) the tree of sample 4.

(a) The flower length of Prosopis juliflora number 5, (b) the fruit (Legume), (c) the leaf (compound), (d) the leaflet (compound), and (e) the tree of sample 5.
4 Conclusions and recommendations
The extended use of remote sensing concepts in the form of hyperspectral data analysis plays an important role in plant taxonomy. The overlapped plant species are usually distinguished in more complicated gene-level classification to retain their separability. In the current research study, the hyperspectral data of P. juliflora collected by temporal screening using the functional gradient decent classification algorithm, which successfully distinguished two separable groups based on the spectral reflectance obtained from different wavelengths.
Prosopis trees play a vital part in the ecology and the economy of many arid and semi-arid zones. They play an integral part in several sustainable lands while preventing further soil degradation and assisting land reclamation use systems that are improving the livelihoods of rural desert populations. Most of the silvicultural constraints to arid zone development have already been overcome, particularly in plantation and establishment nursery, making the most of the best genetic material available, with so many Prosopis trees already planted and often spreading widely by natural regeneration.
P. juliflora is one of the rare wood-producing plant species capable of developing in the Arabian Peninsula. The following are some recommendations stated by the researcher in this study. It is the tree best recommended for reclaiming sand dunes in Saudi Arabia in sandy areas. It is a natural source of wood, fuel, and coal. It contributes to regulating bowel movement and helps preventing constipation because it absorbs water, which causes the intestine to normally work. Finally, it is recommended that more research is performed to study about this very important tree, focusing on other aspects such as the medicinal values of the seeds, fruits, flowers, and leaves.
Acknowledgment
This project was funded by the Deanship of Scientific Research (DSR), King Abdulaziz University, Jeddah, under grant no. G-423-247-1440. The authors, therefore, acknowledge with thanks to DSR’s technical and financial support.
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- Research on the traditional zoning, evolution, and integrated conservation of village cultural landscapes based on “production-living-ecology spaces” – A case study of villages in Meicheng, Guangdong, China
- A prediction method for water enrichment in aquifer based on GIS and coupled AHP–entropy model
- Earthflow reactivation assessment by multichannel analysis of surface waves and electrical resistivity tomography: A case study
- Geologic structures associated with gold mineralization in the Kirk Range area in Southern Malawi
- Research on the impact of expressway on its peripheral land use in Hunan Province, China
- Concentrations of heavy metals in PM2.5 and health risk assessment around Chinese New Year in Dalian, China
- Origin of carbonate cements in deep sandstone reservoirs and its significance for hydrocarbon indication: A case of Shahejie Formation in Dongying Sag
- Coupling the K-nearest neighbors and locally weighted linear regression with ensemble Kalman filter for data-driven data assimilation
- Multihazard susceptibility assessment: A case study – Municipality of Štrpce (Southern Serbia)
- A full-view scenario model for urban waterlogging response in a big data environment
- Elemental geochemistry of the Middle Jurassic shales in the northern Qaidam Basin, northwestern China: Constraints for tectonics and paleoclimate
- Geometric similarity of the twin collapsed glaciers in the west Tibet
- Improved gas sand facies classification and enhanced reservoir description based on calibrated rock physics modelling: A case study
- Utilization of dolerite waste powder for improving geotechnical parameters of compacted clay soil
- Geochemical characterization of the source rock intervals, Beni-Suef Basin, West Nile Valley, Egypt
- Satellite-based evaluation of temporal change in cultivated land in Southern Punjab (Multan region) through dynamics of vegetation and land surface temperature
- Ground motion of the Ms7.0 Jiuzhaigou earthquake
- Shale types and sedimentary environments of the Upper Ordovician Wufeng Formation-Member 1 of the Lower Silurian Longmaxi Formation in western Hubei Province, China
- An era of Sentinels in flood management: Potential of Sentinel-1, -2, and -3 satellites for effective flood management
- Water quality assessment and spatial–temporal variation analysis in Erhai lake, southwest China
- Dynamic analysis of particulate pollution in haze in Harbin city, Northeast China
- Comparison of statistical and analytical hierarchy process methods on flood susceptibility mapping: In a case study of the Lake Tana sub-basin in northwestern Ethiopia
- Performance comparison of the wavenumber and spatial domain techniques for mapping basement reliefs from gravity data
- Spatiotemporal evolution of ecological environment quality in arid areas based on the remote sensing ecological distance index: A case study of Yuyang district in Yulin city, China
- Petrogenesis and tectonic significance of the Mengjiaping beschtauite in the southern Taihang mountains
- Review Articles
- The significance of scanning electron microscopy (SEM) analysis on the microstructure of improved clay: An overview
- A review of some nonexplosive alternative methods to conventional rock blasting
- Retrieval of digital elevation models from Sentinel-1 radar data – open applications, techniques, and limitations
- A review of genetic classification and characteristics of soil cracks
- Potential CO2 forcing and Asian summer monsoon precipitation trends during the last 2,000 years
- Erratum
- Erratum to “Calibration of the depth invariant algorithm to monitor the tidal action of Rabigh City at the Red Sea Coast, Saudi Arabia”
- Rapid Communication
- Individual tree detection using UAV-lidar and UAV-SfM data: A tutorial for beginners
- Technical Note
- Construction and application of the 3D geo-hazard monitoring and early warning platform
- Enhancing the success of new dams implantation under semi-arid climate, based on a multicriteria analysis approach: Case of Marrakech region (Central Morocco)
- TRANSFORMATION OF TRADITIONAL CULTURAL LANDSCAPES - Koper 2019
- The “changing actor” and the transformation of landscapes
Articles in the same Issue
- Regular Articles
- Lithopetrographic and geochemical features of the Saalian tills in the Szczerców outcrop (Poland) in various deformation settings
- Spatiotemporal change of land use for deceased in Beijing since the mid-twentieth century
- Geomorphological immaturity as a factor conditioning the dynamics of channel processes in Rządza River
- Modeling of dense well block point bar architecture based on geological vector information: A case study of the third member of Quantou Formation in Songliao Basin
- Predicting the gas resource potential in reservoir C-sand interval of Lower Goru Formation, Middle Indus Basin, Pakistan
- Study on the viscoelastic–viscoplastic model of layered siltstone using creep test and RBF neural network
- Assessment of Chlorophyll-a concentration from Sentinel-3 satellite images at the Mediterranean Sea using CMEMS open source in situ data
- Spatiotemporal evolution of single sandbodies controlled by allocyclicity and autocyclicity in the shallow-water braided river delta front of an open lacustrine basin
- Research and application of seismic porosity inversion method for carbonate reservoir based on Gassmann’s equation
- Impulse noise treatment in magnetotelluric inversion
- Application of multivariate regression on magnetic data to determine further drilling site for iron exploration
- Comparative application of photogrammetry, handmapping and android smartphone for geotechnical mapping and slope stability analysis
- Geochemistry of the black rock series of lower Cambrian Qiongzhusi Formation, SW Yangtze Block, China: Reconstruction of sedimentary and tectonic environments
- The timing of Barleik Formation and its implication for the Devonian tectonic evolution of Western Junggar, NW China
- Risk assessment of geological disasters in Nyingchi, Tibet
- Effect of microbial combination with organic fertilizer on Elymus dahuricus
- An OGC web service geospatial data semantic similarity model for improving geospatial service discovery
- Subsurface structure investigation of the United Arab Emirates using gravity data
- Shallow geophysical and hydrological investigations to identify groundwater contamination in Wadi Bani Malik dam area Jeddah, Saudi Arabia
- Consideration of hyperspectral data in intraspecific variation (spectrotaxonomy) in Prosopis juliflora (Sw.) DC, Saudi Arabia
- Characteristics and evaluation of the Upper Paleozoic source rocks in the Southern North China Basin
- Geospatial assessment of wetland soils for rice production in Ajibode using geospatial techniques
- Input/output inconsistencies of daily evapotranspiration conducted empirically using remote sensing data in arid environments
- Geotechnical profiling of a surface mine waste dump using 2D Wenner–Schlumberger configuration
- Forest cover assessment using remote-sensing techniques in Crete Island, Greece
- Stability of an abandoned siderite mine: A case study in northern Spain
- Assessment of the SWAT model in simulating watersheds in arid regions: Case study of the Yarmouk River Basin (Jordan)
- The spatial distribution characteristics of Nb–Ta of mafic rocks in subduction zones
- Comparison of hydrological model ensemble forecasting based on multiple members and ensemble methods
- Extraction of fractional vegetation cover in arid desert area based on Chinese GF-6 satellite
- Detection and modeling of soil salinity variations in arid lands using remote sensing data
- Monitoring and simulating the distribution of phytoplankton in constructed wetlands based on SPOT 6 images
- Is there an equality in the spatial distribution of urban vitality: A case study of Wuhan in China
- Considering the geological significance in data preprocessing and improving the prediction accuracy of hot springs by deep learning
- Comparing LiDAR and SfM digital surface models for three land cover types
- East Asian monsoon during the past 10,000 years recorded by grain size of Yangtze River delta
- Influence of diagenetic features on petrophysical properties of fine-grained rocks of Oligocene strata in the Lower Indus Basin, Pakistan
- Impact of wall movements on the location of passive Earth thrust
- Ecological risk assessment of toxic metal pollution in the industrial zone on the northern slope of the East Tianshan Mountains in Xinjiang, NW China
- Seasonal color matching method of ornamental plants in urban landscape construction
- Influence of interbedded rock association and fracture characteristics on gas accumulation in the lower Silurian Shiniulan formation, Northern Guizhou Province
- Spatiotemporal variation in groundwater level within the Manas River Basin, Northwest China: Relative impacts of natural and human factors
- GIS and geographical analysis of the main harbors in the world
- Laboratory test and numerical simulation of composite geomembrane leakage in plain reservoir
- Structural deformation characteristics of the Lower Yangtze area in South China and its structural physical simulation experiments
- Analysis on vegetation cover changes and the driving factors in the mid-lower reaches of Hanjiang River Basin between 2001 and 2015
- Extraction of road boundary from MLS data using laser scanner ground trajectory
- Research on the improvement of single tree segmentation algorithm based on airborne LiDAR point cloud
- Research on the conservation and sustainable development strategies of modern historical heritage in the Dabie Mountains based on GIS
- Cenozoic paleostress field of tectonic evolution in Qaidam Basin, northern Tibet
- Sedimentary facies, stratigraphy, and depositional environments of the Ecca Group, Karoo Supergroup in the Eastern Cape Province of South Africa
- Water deep mapping from HJ-1B satellite data by a deep network model in the sea area of Pearl River Estuary, China
- Identifying the density of grassland fire points with kernel density estimation based on spatial distribution characteristics
- A machine learning-driven stochastic simulation of underground sulfide distribution with multiple constraints
- Origin of the low-medium temperature hot springs around Nanjing, China
- LCBRG: A lane-level road cluster mining algorithm with bidirectional region growing
- Constructing 3D geological models based on large-scale geological maps
- Crops planting structure and karst rocky desertification analysis by Sentinel-1 data
- Physical, geochemical, and clay mineralogical properties of unstable soil slopes in the Cameron Highlands
- Estimation of total groundwater reserves and delineation of weathered/fault zones for aquifer potential: A case study from the Federal District of Brazil
- Characteristic and paleoenvironment significance of microbially induced sedimentary structures (MISS) in terrestrial facies across P-T boundary in Western Henan Province, North China
- Experimental study on the behavior of MSE wall having full-height rigid facing and segmental panel-type wall facing
- Prediction of total landslide volume in watershed scale under rainfall events using a probability model
- Toward rainfall prediction by machine learning in Perfume River Basin, Thua Thien Hue Province, Vietnam
- A PLSR model to predict soil salinity using Sentinel-2 MSI data
- Compressive strength and thermal properties of sand–bentonite mixture
- Age of the lower Cambrian Vanadium deposit, East Guizhou, South China: Evidences from age of tuff and carbon isotope analysis along the Bagong section
- Identification and logging evaluation of poor reservoirs in X Oilfield
- Geothermal resource potential assessment of Erdaobaihe, Changbaishan volcanic field: Constraints from geophysics
- Geochemical and petrographic characteristics of sediments along the transboundary (Kenya–Tanzania) Umba River as indicators of provenance and weathering
- Production of a homogeneous seismic catalog based on machine learning for northeast Egypt
- Analysis of transport path and source distribution of winter air pollution in Shenyang
- Triaxial creep tests of glacitectonically disturbed stiff clay – structural, strength, and slope stability aspects
- Effect of groundwater fluctuation, construction, and retaining system on slope stability of Avas Hill in Hungary
- Spatial modeling of ground subsidence susceptibility along Al-Shamal train pathway in Saudi Arabia
- Pore throat characteristics of tight reservoirs by a combined mercury method: A case study of the member 2 of Xujiahe Formation in Yingshan gasfield, North Sichuan Basin
- Geochemistry of the mudrocks and sandstones from the Bredasdorp Basin, offshore South Africa: Implications for tectonic provenance and paleoweathering
- Apriori association rule and K-means clustering algorithms for interpretation of pre-event landslide areas and landslide inventory mapping
- Lithology classification of volcanic rocks based on conventional logging data of machine learning: A case study of the eastern depression of Liaohe oil field
- Sequence stratigraphy and coal accumulation model of the Taiyuan Formation in the Tashan Mine, Datong Basin, China
- Influence of thick soft superficial layers of seabed on ground motion and its treatment suggestions for site response analysis
- Monitoring the spatiotemporal dynamics of surface water body of the Xiaolangdi Reservoir using Landsat-5/7/8 imagery and Google Earth Engine
- Research on the traditional zoning, evolution, and integrated conservation of village cultural landscapes based on “production-living-ecology spaces” – A case study of villages in Meicheng, Guangdong, China
- A prediction method for water enrichment in aquifer based on GIS and coupled AHP–entropy model
- Earthflow reactivation assessment by multichannel analysis of surface waves and electrical resistivity tomography: A case study
- Geologic structures associated with gold mineralization in the Kirk Range area in Southern Malawi
- Research on the impact of expressway on its peripheral land use in Hunan Province, China
- Concentrations of heavy metals in PM2.5 and health risk assessment around Chinese New Year in Dalian, China
- Origin of carbonate cements in deep sandstone reservoirs and its significance for hydrocarbon indication: A case of Shahejie Formation in Dongying Sag
- Coupling the K-nearest neighbors and locally weighted linear regression with ensemble Kalman filter for data-driven data assimilation
- Multihazard susceptibility assessment: A case study – Municipality of Štrpce (Southern Serbia)
- A full-view scenario model for urban waterlogging response in a big data environment
- Elemental geochemistry of the Middle Jurassic shales in the northern Qaidam Basin, northwestern China: Constraints for tectonics and paleoclimate
- Geometric similarity of the twin collapsed glaciers in the west Tibet
- Improved gas sand facies classification and enhanced reservoir description based on calibrated rock physics modelling: A case study
- Utilization of dolerite waste powder for improving geotechnical parameters of compacted clay soil
- Geochemical characterization of the source rock intervals, Beni-Suef Basin, West Nile Valley, Egypt
- Satellite-based evaluation of temporal change in cultivated land in Southern Punjab (Multan region) through dynamics of vegetation and land surface temperature
- Ground motion of the Ms7.0 Jiuzhaigou earthquake
- Shale types and sedimentary environments of the Upper Ordovician Wufeng Formation-Member 1 of the Lower Silurian Longmaxi Formation in western Hubei Province, China
- An era of Sentinels in flood management: Potential of Sentinel-1, -2, and -3 satellites for effective flood management
- Water quality assessment and spatial–temporal variation analysis in Erhai lake, southwest China
- Dynamic analysis of particulate pollution in haze in Harbin city, Northeast China
- Comparison of statistical and analytical hierarchy process methods on flood susceptibility mapping: In a case study of the Lake Tana sub-basin in northwestern Ethiopia
- Performance comparison of the wavenumber and spatial domain techniques for mapping basement reliefs from gravity data
- Spatiotemporal evolution of ecological environment quality in arid areas based on the remote sensing ecological distance index: A case study of Yuyang district in Yulin city, China
- Petrogenesis and tectonic significance of the Mengjiaping beschtauite in the southern Taihang mountains
- Review Articles
- The significance of scanning electron microscopy (SEM) analysis on the microstructure of improved clay: An overview
- A review of some nonexplosive alternative methods to conventional rock blasting
- Retrieval of digital elevation models from Sentinel-1 radar data – open applications, techniques, and limitations
- A review of genetic classification and characteristics of soil cracks
- Potential CO2 forcing and Asian summer monsoon precipitation trends during the last 2,000 years
- Erratum
- Erratum to “Calibration of the depth invariant algorithm to monitor the tidal action of Rabigh City at the Red Sea Coast, Saudi Arabia”
- Rapid Communication
- Individual tree detection using UAV-lidar and UAV-SfM data: A tutorial for beginners
- Technical Note
- Construction and application of the 3D geo-hazard monitoring and early warning platform
- Enhancing the success of new dams implantation under semi-arid climate, based on a multicriteria analysis approach: Case of Marrakech region (Central Morocco)
- TRANSFORMATION OF TRADITIONAL CULTURAL LANDSCAPES - Koper 2019
- The “changing actor” and the transformation of landscapes