This study aimed to assess the health of the Kalaji watershed based on relative and absolute approaches and highlight their differences. First, the sub-watersheds' status was evaluated regarding geomorphological, hydrological, water quality, and landscape criteria using five indicators: specific erosion, specific flood, landslide density, specific sediment, and the percentage of natural land uses. The overall health index was calculated by combining the weights (by AHP) and values of the indicators. The findings indicate a significant difference in the results of the two approaches. The minimum, maximum, and average of the health index of sub-watersheds are 0.302, 0.758, and 0.601 respectively in the relative approach, while they are equal to 0.194, 0.753, and 0.308 respectively in the absolute approach. The results also showed that the relative approach has a higher health index and more healthy class than the absolute approach. The findings emphasize that the appropriate approach should be chosen according to the desired goals before assessing the watershed's health. Overall, this study provides a better understanding of the two approaches to watershed health assessment, especially the absolute ones.

  • Watershed health was assessed based on relative and absolute approaches.

  • The relative approach gives a higher index of watershed health than the absolute approach.

  • The health status of the Kalaji watershed is not satisfactory and should be improved.

  • The appropriate approach should be selected before assessing the watershed's health.

Watersheds provide services to living organisms, referred to as watershed services (Porras 2008). Watershed services have a vast wide scope and can be classified into four general categories: providing services, regulating services, cultural services, and supporting services (Hamel et al. 2018). Watershed health is a term used to describe the ecological condition of a watershed (Jones et al. 2002). A healthy watershed has a structure and function that supports its ecosystems and has appropriate services for the relevant biological communities (Ahn & Kim 2019). In a healthy watershed, the quality of water and habitat is suitable to support native species, and the amount of natural cover is such that its geomorphological and hydrological processes are within normal limits (Ahn & Kim 2017). Since the level of watershed services has a direct relationship with the level of watershed health, checking the health status of watersheds is very important (Jones et al. 2002).

During the last few decades, the rapid growth of the population and the need to provide food have put excessive pressure on all types of renewable resources, including water, soil, and natural vegetation (Hou et al. 2016). Excessive pressure on watershed resources has taken the hydrogeomorphic processes of watersheds out of the natural range and reduced the health of watersheds. The drying up of wetlands (Tussupova et al. 2020), the drop in the level of underground water tables (Madani 2014), severe erosion (Mosaffaie & Talebi 2014), the occurrence of numerous floods (Karimi Sangchini et al. 2022), the intensification of desertification (Rashvand et al. 2013), the increase of dust centers (Soltani et al. 2023), and the reduction of the area of natural habitats (Holland et al. 2016) are among the signs of the deteriorating health of watersheds (Mosaffaie & Salehpour Jam 2021; Jam et al. 2022).

To apply effective management to watersheds, first of all, it is necessary to determine the correct management policy including maintaining the status quo or revitalization based on the health status of the watershed (Jam & Mosaffaie 2023). In recent years, a variety of research has been conducted on watershed health assessment (Sadeghi & Hazbavi 2017; Hazbavi et al. 2018; Alilou et al. 2019; Hazbavi et al. 2019; Sadeghi et al. 2019; Mirchooli et al. 2021; Mosaffaie et al. 2021; Chamani et al. 2023; Gatgash & Sadeghi 2024). Two features are noteworthy in past research: (1) wide variety in sub-indices of watershed health and (2) relativity of the assessments.

Finding indicators that will be both valid and feasible is often the most challenging design issue in a monitoring system or evaluation (Gari et al. 2015). Watershed health sub-indices used in past research can be divided into two general categories: (1) indicators that directly represent the status of watershed health (hydrological, geomorphological, and habitat criteria) and (2) indicators that do not directly represent the status of watershed health but can potentially affect it. Sub-indices such as soil erosion rate, flood potential, groundwater loss, water quality, and habitat condition are among the indicators that can directly provide an overview of different criteria for watershed health (Tsai et al. 2021). Among the sub-indices of the second category are mean annual precipitation, mean annual evapotranspiration, population density, area of agricultural land with slope >25%, the area under anthropogenic activity, environmental sensitive area index, the slope of contribution area in runoff generation, landscape diversity index, normalized difference vegetation index, landscape dominance index, rangelands area ratio, landscape fragmentation index, and drainage density, which do not directly represent the status of watershed health criteria but can potentially affect them. In addition to confusion, the large number and variety of watershed health sub-indices may prevent obtaining a correct view of the watershed health status if they are not related or if there is colinearity with other sub-indices.

In addition to the wide variety of sub-indices, another characteristic of past research has been the relativity of assessments. In almost all past research, temporal or spatial variations in watershed health have been assessed relatively. In the relative approach, the detailed assessment of the situation of the subject under study (watershed health) is not relevant, but different treatments are only compared in terms of the subject in question (Linkov et al. 2006; Podviezko & Podvezko 2014). Although the information obtained from relative assessment is suitable for prioritizing watersheds for protection programs, there is a need to employ an absolute approach, the results of which indicate the actual health status of the watershed, rather than measuring the status of the sub-units relative to each other. Therefore, this research aims to assess the health of the Kalaji watershed (as a pilot watershed) using the key and direct indicators based on two relative and absolute approaches and to highlight the differences in the results obtained from the application of these two approaches. The results of this research provide a better understanding of the relative and absolute assessments of watershed health and can be considered as a preliminary for the development of absolute models of watershed health assessment.

Study area

The Kalaji watershed with a drainage area of 50,368 ha is located in the east of Golestan province (north of Kalaleh city) of Iran (Figure 1). The maximum and minimum elevations of the watershed are 821 and 81 m above sea level, respectively. The average slope of the watershed is 18.5% and the dominant aspects of the slopes are southeast and east. In general, the topography of the watershed is characterized by a complex combination of hills (55%), mountains (27%), plateaus, and upper terraces (18%). The major land uses include rangeland (87%), agriculture (12%), and residential (1%). This watershed supports an economy based on agriculture (76% of the population), and livestock husbandry (24% of the population), and contains wildlife habitats.
Figure 1

Location map of the Kalaji watershed in Iran.

Figure 1

Location map of the Kalaji watershed in Iran.

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The average annual precipitation equal to 434.9 mm and the average annual temperature equal to 16.9 have brought a semi-arid climate (according to the Demartini method) to this watershed. According to the ambrothermic curve, the driest months range from May to October. The lithological units of the basin include green to gray shale (Ks), glauconitic sandstone (Kat), Quaternary loess (Qgeh), new river sediments (Qal), and old alluvium (Qf1). Due to the large extent of thick-layered loess, various geomorphological facies and erosion types, including sheet, rill, piping, badland, and gully, can be seen in the area. Agricultural activities and livestock grazing, regardless of soil limitations and ecological capacity, have aggravated erosion in the region. These features have also caused many landslides in the study area. Sediments caused by severe soil erosion have decreased the water quality of waterways and also reduced the useful capacity of the Bustan Dam reservoir located downstream of the watershed. The Soil and Water Conservation Bureau and the Council of Agriculture both focus on increasing vegetative land cover and stream conservation.

Methods

This research assessed the health status of 25 sub-watersheds based on relative and absolute approaches. The structure of this research consists of three main stages including (1) establishment of the watershed health criteria and indicators, (2) collecting data and calculating the weights of indicators, and (3) applying relative and absolute approaches to assess watershed health. Figure 2 shows the visual summary of the research stages.
Figure 2

Flowchart of the study.

Figure 2

Flowchart of the study.

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Establishment of the watershed health criteria and indicators

The establishment of indicators depends on the definition of what one wants to indicate (Bosch 1967). The choice of key indicators can make a critical difference in the results of an evaluation (Gari et al. 2015; Czúcz et al. 2021). In this research, watershed health indicators were selected according to the concept of watershed health. Therefore, according to the definition of a healthy watershed, five criteria, including erosion status, flood status, landslide status, water quality, and habitat status, were chosen to explain the geomorphological, hydrological, water quality, and habitat conditions of the sub-watersheds.

Good indicators are simple, variable, valid, clearly defined, measurable, reliable, and quantifiable (Bosch 1967). The number of indicators should not be too numerous to clutter the overview nor too few to prevent the provision of sufficient information (Czúcz et al. 2021). Therefore, in this research, six indicators, including specific erosion, specific peak flood discharge (return period = 50 years), landslide density ratio (Ldr) (used only in the relative approach), the area percentage of landslide hazard class higher than medium (used only in the absolute approach), specific sediment yield, and the percentage of natural cover were selected as watershed health indicators. In the following, the data collection method for each of the indicators is explained.

Collecting data and weighting the indicators

Data collection
The soil erosion status is one of the most important indicators that represent the geomorphological condition of the watershed (Mosaffaie et al. 2015; Hazbavi et al. 2019). So in this research, the erosion potential method (EPM) was used to estimate the erosion rate and sediment yield of the watershed (Gavrilovic 1988). This method (also called the Gavrilović method) is characterized by high security in the calculation of sediment production, transport, and accumulation (Tangestani 2006). This method can effectively and quickly estimate the potential erosion rates and sediment yield at the watershed scale (ZIA & Ahmadi 2011; Sakuno et al. 2020). According to the EPM, the annual volume of soil erosion is calculated using the following equation.
(1)
where Wsp represents the specific annual soil erosion (m3/km2/yr), t is the mean annual temperature (°C), H is the mean annual precipitation (mm), and Z is the erosion coefficient, which reflects the erosion intensity and is calculated using the following equation.
(2)
where Y is the coefficient of rock and soil resistance to erosion ranging from 0.25 to 2, Xa is the coefficient of land use ranging from 0.05 to 1, φ is the coefficient of type and extent of erosion ranging from 0.1 to 1, and I is the average slope of area (%).
The flooding status is one of the most important indicators that represent the hydrological condition of the watershed (Mosaffaie 2015, 2016; Chamani et al. 2024). So in this research, the specific peak flood discharge was chosen as an indicator to represent the flooding status of each sub-watershed. Fuller's formula (Equations (3) and (4)) was used to estimate the special flood peak discharge with a return period of 50 years (Fuller 1914). This formula relates the peak to the maximum mean daily flow and the drainage area (Sangal 1983).
(3)
(4)
where Qmax is the maximum flood discharge (m3/s), A is the sub-watershed area (km2), Qp is the maximum daily discharge (m3/s), T is the return period (year), and C is the regional coefficient ranging from 0.3 to 2.8 depending on the region characteristics.
Landslides also represent the geomorphological condition of the watershed and are one of the most important environmental hazards that threaten the optimal services of watersheds (Mosaffaie et al. 2023; Salehpour Jam et al. 2023). Based on this, the landslide condition of each watershed can be considered as a measure of the health of the watershed. So in this research, the Ldr indicator (Lee & Pradhan 2007) which represents the ratio of landslide density in each sub-watershed to landslide density in the whole study area was calculated using the following equation.
(5)
where Si is the landslide area within the ith sub-watershed, and Ai is the area of the ith sub-watershed.

The Ldr indicator is only applicable in the relative approach because it represents the density of landslides in each sub-watershed only compared to the entire study area. So, for the absolute approach, the landslide hazard map of the watershed was prepared using the Haeri–Sameie method (Armin et al. 2019). This method has been developed for the Golestan and Mazandaran provinces of Iran where the study watershed is located. The formula of this method calculates the landslide hazard index from the combination of thematic maps of seven factors, including lithology, slope, fault length, road and river length, precipitation, rainfall intensity, and earthquake acceleration. The resulting landslide hazard map was classified into seven classes (Sarfaraz et al. 2021). The other factors that are required by this method are documented in the literature (Armin et al. 2019; Sarfaraz et al. 2021).

The biggest threat to biodiversity to date has been anthropogenic activities, which have transformed natural habitats into agricultural, industrial, residential, mining, and other unnatural land uses (Prakash & Verma 2022). In this research, the percentage of natural cover was used as an indicator to show the status of the habitat criterion. In this regard, among the land uses in the watershed, ranges, and river terraces were considered land uses with natural cover, and agricultural lands, orchards, and residential areas were considered areas without natural cover.

Weighting the indicators

The analytic hierarchy process (AHP) was used to calculate the contribution (weight) of each indicator (Saaty 1980). The AHP technique has a particular application in weighing factors based on multiple criteria and pairwise comparisons (Saaty 2008). The weighting process of this research can be summarized in four steps: creating a matrix to compare indicators; making pairwise comparisons of indicators using a scale of 1–9 (conducted by the opinions of 10 environmental experts); calculating the weights of indicators, and eventually checking the consistency of the evaluations.

Analyses and software

In this research, the health of the 25 sub-watersheds of Kalaji was assessed based on two relative and absolute approaches. In this regard, the Watershed Health Index (WHI) was calculated according to relative and absolute methods (below subsections). To better discriminate the differences of WHI resulting from each approach, the ArcGIS 10.8 software was applied to categorize the range of WHI [0, 1] using an equal interval method into five classes where (0.00–0.20), (0.21–0.40), (0.41–0.60), (0.61–0.80), and (0.81–1.00), respectively, represent unhealthy, relatively unhealthy, moderately healthy, relatively healthy, and healthy watersheds.

Relative approach
In the relative approach of watershed health assessment, the range of index values is limited to the values within the studied watershed, and the index values in the areas outside the study area are not included in the analysis. Therefore, in this approach, the index values of the sub-watersheds are only compared with each other and not with the index values outside the study area. In this research, the index values of the sub-watersheds were standardized into comparable values by using the maximum difference normalization method (Equations (6) and (7) for indicators which, respectively, have direct and reverse relationships with the watershed health concept).
(6)
(7)
where Z is the standardized index value, X is the indicator value, and max (X) and min (X) are, respectively, the maximum and minimum values of indicators within the study area.

By these equations, the maximum and minimum values of each indicator were standardized to 1, and zero, respectively, and the rest of the values were standardized between zero and one.

In the next step, the relative WHI was calculated using the following equation for each sub-watershed.
(8)
where Zi is the standardized value of indicators and Wi is the weight of each indicator. The WHI value ranges in [0, 1] where the greater its value, implies the healthier sub-watershed.
Absolute approach

In the absolute approach of watershed health assessment, the range of index values is not limited to the values within the studied watershed and includes values that are recorded even outside the study area. Therefore, in this approach, the values of the sub-indices of the study area are compared with the values of a larger scale (in this research with the values recorded in the whole of Iran). For this purpose, Table 1 was developed to assign a health score for the indicator values of the watershed compared to national ranges of indicators. In this regard, the results of flooding rate classification (Porhemmat 2018; Sharifi 2022), soil erosion rate classification (Sharifi 2015), and sediment yield classification (Sharifi 2017) were collected for Iran's watersheds. The percentage of area under more than medium classes of landslide hazards (Haeri–Sameie method) was also used to index the landslide criterion.

Table 1

Classification of sub-indicators of watershed health in Iran

IndicatorHealth scoreFlooding rate (m3/s/km2)Erosion rate (t/h/yr)Landslide (area of high-hazard classes (%))Sediment yield (t/h/yr)Natural land uses (%)
0.0–0.24 0–2 0–20 <1 80–100 
0.75 0.24–0.32 2–5 20–40 1–2 60–80 
0.5 0.32–0.55 5–10 40–60 2–4 40–60 
0.25 0.55–0.7 10–15 60–80 4–10 20–40 
0.7 < 15 < 80–100 10 < 0–20 
IndicatorHealth scoreFlooding rate (m3/s/km2)Erosion rate (t/h/yr)Landslide (area of high-hazard classes (%))Sediment yield (t/h/yr)Natural land uses (%)
0.0–0.24 0–2 0–20 <1 80–100 
0.75 0.24–0.32 2–5 20–40 1–2 60–80 
0.5 0.32–0.55 5–10 40–60 2–4 40–60 
0.25 0.55–0.7 10–15 60–80 4–10 20–40 
0.7 < 15 < 80–100 10 < 0–20 

Then, the values of each sub-index in each sub-watershed were compared with the related classification and the corresponding health score was assigned. Finally, the absolute health index was calculated by the following equation for each sub-watershed.
(9)
where hi is the health score of sub-indicators and Wi is the weight of each indicator. The WHI value ranges in [0, 1] where the greater its value, implies the healthier sub-watershed.

Some of the main parameters and indicator values at 25 sub-watersheds of the study area are presented in Table 2.

Table 2

Main parameters and indicator values of the Kalaji sub-watershed

Sub-watershedArea (ha)Height (m)Slope (%)Annual precipitation (mm)Curve numberSediment Delivery Ratio (SDR) (Ru)Erosion coefficient (Z)Landslide density ratio (Ldr)Density of landslide high-risk classes (ha)Vegetation cover (%)Natural landuse (%)Soil erosion (Wsp) (t/ha/yr)Sediment production (Gsp) (t/ha/yr)Qmax(50) (m3/s/km2)
G1 894 419 23.9 450 77 0.36 0.6 0.26 304 69 95.1 14 5.1 0.60 
G2 1,071 358 27.7 456 79 0.43 0.6 2.33 477 69 92.2 13.1 5.7 0.56 
G3 1,850 521 31.4 445 78 0.4 0.8 0.32 1,333 69 94.4 19.9 7.9 0.46 
G4 1,630 405 28.1 448 77 0.52 0.8 9.20 955 69 98.3 25.1 13.2 0.48 
G5 3,542 344 30.4 429 77 0.38 1.1 0.00 1,558 52.7 95.8 38.2 14.5 0.36 
G6 3,794 513 30.3 497 78 0.43 0.9 0.09 1,643 69 96.3 24.8 10.7 0.36 
GT1 4,086 292 17.2 416 82 0.52 1.1 3.47 311 60.1 85.7 38.3 20.1 0.35 
GT2 1,671 374 13.4 440 77 0.37 0.9 0.32 381 59.7 98.8 23.9 8.8 0.48 
K11 1,780 387 14.4 471 77 0.29 0.62 1,319 62.5 100 31.9 9.1 0.46 
K12 751 365 18.8 442 77 0.34 0.64 377 41.4 88.5 33.1 11.3 0.64 
K13 3,950 371 19.2 521 78 0.3 1.1 0.23 3,620 61.7 95.6 35.9 10.9 0.35 
K14 832 333 19 465 77 0.33 1.4 0.93 513 35.2 99.7 50.3 16.4 0.61 
K15 1,613 472 17.5 435 77 0.4 1.6 0.30 962 35.2 99.3 58.9 23.5 0.48 
K1T1 3,729 305 12.4 518 78 0.44 0.9 0.85 3,266 54.5 89.4 26.6 11.6 0.36 
K1T2 3,263 354 17 409 80 0.37 1.3 0.05 505 36.7 87.3 41.7 15.4 0.38 
K21 2,380 293 19.3 410 77 0.41 0.64 1,037 63.5 99.2 30.2 12.3 0.42 
K22 1,888 295 17.2 411 77 0.4 0.07 458 60.1 100 28.9 11.5 0.45 
K23 962 231 13.9 380 77 0.31 0.9 3.35 511 35.3 68.8 24.5 7.5 0.58 
K24 986 262 17.8 395 77 0.37 1.1 2.53 597 35.2 84.7 32.1 11.8 0.58 
K25 1,224 156 5.1 343 80 0.28 0.7 0.30 396 35.2 1.2 13.5 3.8 0.53 
K26 1,848 200 11.4 364 79 0.37 0.8 0.31 926 39.4 32.2 17.9 6.1 0.46 
K27 1,141 203 5.8 366 77 0.32 0.2 0.36 288 50.6 3.1 0.55 
K28 1,313 169 3.6 349 77 0.27 0.2 0.00 221 37.4 1.6 0.4 0.52 
K2T1 3,315 228 12.5 378 78 0.37 0.35 1,444 35.2 40.7 25.3 9.3 0.37 
K2T2 853 118 6.3 324 82 0.21 0.9 0.00 385 35.2 18.6 0.61 
Total 50,368 344 18.6 435 78 0.45 1.00 23,786 55 78.2 28.3 12.8 0.15 
Min 750.9 118 3.6 324 77 0.21 0.2 0.00 221 35.2 1.6 0.4 0.3 
Max 4,086.2 521 31.4 521 82 0.52 1.6 9.20 3,620 69 100 58.9 23.5 0.6 
Average 2,014.7 320 17.4 423 78 0.37 0.9 1.10 1,830 51 74 26.9 10.1 0.5 
Sub-watershedArea (ha)Height (m)Slope (%)Annual precipitation (mm)Curve numberSediment Delivery Ratio (SDR) (Ru)Erosion coefficient (Z)Landslide density ratio (Ldr)Density of landslide high-risk classes (ha)Vegetation cover (%)Natural landuse (%)Soil erosion (Wsp) (t/ha/yr)Sediment production (Gsp) (t/ha/yr)Qmax(50) (m3/s/km2)
G1 894 419 23.9 450 77 0.36 0.6 0.26 304 69 95.1 14 5.1 0.60 
G2 1,071 358 27.7 456 79 0.43 0.6 2.33 477 69 92.2 13.1 5.7 0.56 
G3 1,850 521 31.4 445 78 0.4 0.8 0.32 1,333 69 94.4 19.9 7.9 0.46 
G4 1,630 405 28.1 448 77 0.52 0.8 9.20 955 69 98.3 25.1 13.2 0.48 
G5 3,542 344 30.4 429 77 0.38 1.1 0.00 1,558 52.7 95.8 38.2 14.5 0.36 
G6 3,794 513 30.3 497 78 0.43 0.9 0.09 1,643 69 96.3 24.8 10.7 0.36 
GT1 4,086 292 17.2 416 82 0.52 1.1 3.47 311 60.1 85.7 38.3 20.1 0.35 
GT2 1,671 374 13.4 440 77 0.37 0.9 0.32 381 59.7 98.8 23.9 8.8 0.48 
K11 1,780 387 14.4 471 77 0.29 0.62 1,319 62.5 100 31.9 9.1 0.46 
K12 751 365 18.8 442 77 0.34 0.64 377 41.4 88.5 33.1 11.3 0.64 
K13 3,950 371 19.2 521 78 0.3 1.1 0.23 3,620 61.7 95.6 35.9 10.9 0.35 
K14 832 333 19 465 77 0.33 1.4 0.93 513 35.2 99.7 50.3 16.4 0.61 
K15 1,613 472 17.5 435 77 0.4 1.6 0.30 962 35.2 99.3 58.9 23.5 0.48 
K1T1 3,729 305 12.4 518 78 0.44 0.9 0.85 3,266 54.5 89.4 26.6 11.6 0.36 
K1T2 3,263 354 17 409 80 0.37 1.3 0.05 505 36.7 87.3 41.7 15.4 0.38 
K21 2,380 293 19.3 410 77 0.41 0.64 1,037 63.5 99.2 30.2 12.3 0.42 
K22 1,888 295 17.2 411 77 0.4 0.07 458 60.1 100 28.9 11.5 0.45 
K23 962 231 13.9 380 77 0.31 0.9 3.35 511 35.3 68.8 24.5 7.5 0.58 
K24 986 262 17.8 395 77 0.37 1.1 2.53 597 35.2 84.7 32.1 11.8 0.58 
K25 1,224 156 5.1 343 80 0.28 0.7 0.30 396 35.2 1.2 13.5 3.8 0.53 
K26 1,848 200 11.4 364 79 0.37 0.8 0.31 926 39.4 32.2 17.9 6.1 0.46 
K27 1,141 203 5.8 366 77 0.32 0.2 0.36 288 50.6 3.1 0.55 
K28 1,313 169 3.6 349 77 0.27 0.2 0.00 221 37.4 1.6 0.4 0.52 
K2T1 3,315 228 12.5 378 78 0.37 0.35 1,444 35.2 40.7 25.3 9.3 0.37 
K2T2 853 118 6.3 324 82 0.21 0.9 0.00 385 35.2 18.6 0.61 
Total 50,368 344 18.6 435 78 0.45 1.00 23,786 55 78.2 28.3 12.8 0.15 
Min 750.9 118 3.6 324 77 0.21 0.2 0.00 221 35.2 1.6 0.4 0.3 
Max 4,086.2 521 31.4 521 82 0.52 1.6 9.20 3,620 69 100 58.9 23.5 0.6 
Average 2,014.7 320 17.4 423 78 0.37 0.9 1.10 1,830 51 74 26.9 10.1 0.5 

The value range of each sub-indicator in the study area was classified into five categories based on the equal interval method (Figure 3). With this figure, it is possible to get immediate knowledge about the status of various health sub-indices in the studied watershed. These classified sub-indicator maps have been colored according to the direct or indirect relationship of the sub-indicator with the WHI. As can be inferred from the order of colors in the legends of these maps, the percentage of natural land uses is the only indicator that has a direct relationship with the WHI. Other sub-indices have an inverse relationship with the overall WHI.
Figure 3

The classified maps of watershed health sub-indicators are (a) erosion, (b) flooding, (c) sediment production, (d) landslide density, (e) landslide hazard, and (f) natural land use.

Figure 3

The classified maps of watershed health sub-indicators are (a) erosion, (b) flooding, (c) sediment production, (d) landslide density, (e) landslide hazard, and (f) natural land use.

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Figure 4 shows the weighting chart of watershed health sub-indices obtained from the AHP technique. The highest (0.36) and lowest (0.07) weights are assigned to sub-indices of erosion and landslide, respectively. This survey of 10 experts (collective wisdom), if there is consistency among the opinions of experts, can be reliable and trusted. The calculated consistency ratio (0.021) is less than 0.1 (CR ≤ 0.1), which implies the acceptability of paired comparisons.
Figure 4

Weights of sub-indicators resulted from the AHP technique (CR = 0.021).

Figure 4

Weights of sub-indicators resulted from the AHP technique (CR = 0.021).

Close modal

Table 3 shows normalized values and partial health scores of sub-indicators that have been used to calculate the relative and absolute WHI, respectively.

Table 3

Normalized values and partial health scores of sub-indicators

UnitNormalized indicator values
WHI (relative)Partial health scores
WHI (absolute)
QmaxLdrWspGspNatural landuseQmaxLdrWspGspNatural landuse
G1 0.14 0.97 0.78 0.80 0.95 0.640 0.25 0.75 0.25 0.25 0.366 
G2 0.27 0.75 0.80 0.77 0.92 0.659 0.25 0.5 0.25 0.25 0.349 
G3 0.62 0.96 0.68 0.68 0.94 0.711 0.5 0.25 0.25 0.310 
G4 0.55 0.00 0.59 0.45 0.98 0.555 0.5 0.5 0.281 
G5 0.94 1.00 0.36 0.39 0.96 0.635 0.5 0.5 0.281 
G6 0.97 0.99 0.59 0.56 0.96 0.758 0.5 0.5 0.281 
GT1 1.00 0.62 0.36 0.15 0.86 0.570 0.5 0.315 
GT2 0.56 0.97 0.61 0.64 0.99 0.667 0.5 0.75 0.25 0.344 
K11 0.60 0.93 0.47 0.62 1.00 0.622 0.5 0.25 0.25 0.310 
K12 0.00 0.93 0.45 0.53 0.89 0.420 0.25 0.5 0.212 
K13 0.99 0.98 0.40 0.55 0.96 0.689 0.5 0.247 
K14 0.08 0.90 0.15 0.31 1.00 0.302 0.25 0.25 0.195 
K15 0.54 0.97 0.00 0.00 0.99 0.323 0.5 0.5 0.281 
K1T1 0.96 0.91 0.56 0.52 0.89 0.724 0.5 0.247 
K1T2 0.90 0.99 0.30 0.35 0.87 0.586 0.5 0.315 
K21 0.75 0.93 0.50 0.49 0.99 0.650 0.5 0.5 0.281 
K22 0.63 0.99 0.52 0.52 1.00 0.636 0.5 0.75 0.298 
K23 0.20 0.64 0.60 0.69 0.69 0.518 0.25 0.5 0.25 0.75 0.230 
K24 0.21 0.73 0.47 0.51 0.85 0.463 0.25 0.25 0.195 
K25 0.37 0.97 0.79 0.86 0.01 0.613 0.5 0.75 0.25 0.5 0.371 
K26 0.62 0.97 0.72 0.76 0.32 0.670 0.5 0.5 0.25 0.25 0.245 
K27 0.32 0.96 0.97 0.98 0.08 0.694 0.25 0.75 0.75 0.75 0.530 
K28 0.41 1.00 1.00 1.00 0.00 0.728 0.5 0.753 
K2T1 0.91 0.96 0.59 0.61 0.41 0.687 0.5 0.5 0.25 0.5 0.272 
K2T2 0.10 1.00 0.70 0.85 0.00 0.506 0.25 0.5 0.5 0.194 
Total 1.66 0.89 0.53 0.46 0.78 0.884 0.50 0.50 0.00 0.00 0.75 0.254 
Min 0.00 0.00 0.00 0.00 0.00 0.302 0.25 0.00 0.00 0.00 0.00 0.194 
Max 1.00 1.00 1.00 1.00 1.00 0.758 0.50 1.00 1.00 1.00 1.00 0.753 
Average 0.55 0.88 0.56 0.58 0.74 0.601 0.42 0.53 0.10 0.18 0.78 0.308 
UnitNormalized indicator values
WHI (relative)Partial health scores
WHI (absolute)
QmaxLdrWspGspNatural landuseQmaxLdrWspGspNatural landuse
G1 0.14 0.97 0.78 0.80 0.95 0.640 0.25 0.75 0.25 0.25 0.366 
G2 0.27 0.75 0.80 0.77 0.92 0.659 0.25 0.5 0.25 0.25 0.349 
G3 0.62 0.96 0.68 0.68 0.94 0.711 0.5 0.25 0.25 0.310 
G4 0.55 0.00 0.59 0.45 0.98 0.555 0.5 0.5 0.281 
G5 0.94 1.00 0.36 0.39 0.96 0.635 0.5 0.5 0.281 
G6 0.97 0.99 0.59 0.56 0.96 0.758 0.5 0.5 0.281 
GT1 1.00 0.62 0.36 0.15 0.86 0.570 0.5 0.315 
GT2 0.56 0.97 0.61 0.64 0.99 0.667 0.5 0.75 0.25 0.344 
K11 0.60 0.93 0.47 0.62 1.00 0.622 0.5 0.25 0.25 0.310 
K12 0.00 0.93 0.45 0.53 0.89 0.420 0.25 0.5 0.212 
K13 0.99 0.98 0.40 0.55 0.96 0.689 0.5 0.247 
K14 0.08 0.90 0.15 0.31 1.00 0.302 0.25 0.25 0.195 
K15 0.54 0.97 0.00 0.00 0.99 0.323 0.5 0.5 0.281 
K1T1 0.96 0.91 0.56 0.52 0.89 0.724 0.5 0.247 
K1T2 0.90 0.99 0.30 0.35 0.87 0.586 0.5 0.315 
K21 0.75 0.93 0.50 0.49 0.99 0.650 0.5 0.5 0.281 
K22 0.63 0.99 0.52 0.52 1.00 0.636 0.5 0.75 0.298 
K23 0.20 0.64 0.60 0.69 0.69 0.518 0.25 0.5 0.25 0.75 0.230 
K24 0.21 0.73 0.47 0.51 0.85 0.463 0.25 0.25 0.195 
K25 0.37 0.97 0.79 0.86 0.01 0.613 0.5 0.75 0.25 0.5 0.371 
K26 0.62 0.97 0.72 0.76 0.32 0.670 0.5 0.5 0.25 0.25 0.245 
K27 0.32 0.96 0.97 0.98 0.08 0.694 0.25 0.75 0.75 0.75 0.530 
K28 0.41 1.00 1.00 1.00 0.00 0.728 0.5 0.753 
K2T1 0.91 0.96 0.59 0.61 0.41 0.687 0.5 0.5 0.25 0.5 0.272 
K2T2 0.10 1.00 0.70 0.85 0.00 0.506 0.25 0.5 0.5 0.194 
Total 1.66 0.89 0.53 0.46 0.78 0.884 0.50 0.50 0.00 0.00 0.75 0.254 
Min 0.00 0.00 0.00 0.00 0.00 0.302 0.25 0.00 0.00 0.00 0.00 0.194 
Max 1.00 1.00 1.00 1.00 1.00 0.758 0.50 1.00 1.00 1.00 1.00 0.753 
Average 0.55 0.88 0.56 0.58 0.74 0.601 0.42 0.53 0.10 0.18 0.78 0.308 

The health class maps (relative and absolute approaches) of the Kalaji watershed have been presented in Figure 5. According to this figure, in the relative approach, most of the watershed is under the relatively healthy class (green) and two classes, including healthy and unhealthy, do not exist in the watershed. This is while in the absolute approach, most of the watershed is under the relatively unhealthy class (brown), and only the healthy class does not exist in the watershed. Figure 6 also shows the distribution of the number and percentage of sub-watersheds in various health classes. This figure indicates that in the relative approach, the class of relatively healthy with 16 watersheds (64%) is dominant, while, in the absolute approach, the class of relatively unhealthy with 20 watersheds (80%) is dominant.
Figure 5

Maps of watershed health classes.

Figure 5

Maps of watershed health classes.

Close modal
Figure 6

Distribution of the number of sub-watersheds in various health classes: (a) relative approach and (b) absolute approach.

Figure 6

Distribution of the number of sub-watersheds in various health classes: (a) relative approach and (b) absolute approach.

Close modal

In this research, the selection of watershed health criteria and indicators were established based on indicators that directly represent the status of various aspects (geomorphological, hydrological, and habitat) of watershed health. In addition to confusion, employing numerous sub-indices may prevent a correct view of the health status of the watershed if they are not related or if there is colinearity with other sub-indices. So, indicators such as population density, water consumption, climate change, and other indicators that do not directly represent the health status of the watershed were not included in the analysis. This is while most previous studies (Hazbavi & Sadeghi 2017; Hazbavi et al. 2020; Sadeghi et al. 2023) employed a complex of direct and indirect indicators to investigate watershed health. Entering indirect indicators can cause the results to deviate from the reality of watershed health, although these indicators can affect watershed health in the future. Since the establishment of indicators should be based on the concept of watershed health (what one wants to indicate (Gari et al. 2015)), the authors suggest the use of indicators that only directly represent the status of watershed health.

Due to the diversity and multiplicity of watershed health criteria and indicators, extensive environmental data and information (temporal and spatial) were collected. Also, to cover the data gap, various methods such as direct measurement, results of previous studies, experimental models, multicriteria decision-making, remote sensing, and statistical generalization from areas with data to areas without data were used. However, due to the lack of data and information, some criteria were indexed by indicators that do not directly express the status of these criteria. Among the most important of these criteria were water quality and habitat condition, which in this research were indexed by the sediment load and the percentage of natural land indicators, respectively. This limitation can potentially affect the results of watershed health assessment in both the relative and absolute approaches. So, designing and establishing a WHI monitoring system can remove such limitations and, as a result, promote the accuracy of the overall index of watershed health.

The results of watershed health assessment with two relative and absolute approaches indicate a significant difference in the results of these two approaches. Figure 6 implies that in the relative approach, the health class of the sub-watersheds was distributed in three classes so that healthy and unhealthy classes were not calculated for any of the sub-watersheds. This is while, in the absolute approach, the health class of the sub-watersheds was distributed in four classes, and the healthy class was not calculated for any of the sub-watersheds. The highest frequency in relative and absolute approaches belongs respectively to the relatively healthy (64%) and relatively unhealthy (80%) classes. The average health index for sub-watersheds in relative and absolute approaches were also calculated as 0.601 and 0.308, respectively. These findings imply that the relative approach has resulted in higher values for the overall WHI. The reason for this is the ranges of values of the sub-indices, which in the relative approach belong to the studied watershed (Kalaji), but in the absolute approach belong to a wide region (in this research, the whole country of Iran).

It should be kept in mind that the purpose and function of these two approaches are also different. The goal of the absolute approach, which can be used for even a single watershed, is to gain a correct understanding of the health status, and if there are several watersheds or sub-watersheds, they can also be prioritized based on the results. This is despite the fact that the function of the relative approach is only for prioritizing several sub-watersheds and with this approach, it is not possible to achieve a correct understanding of the health status unless the area under study is large enough to include both unhealthy and healthy sub-watersheds (reference watershed).

Therefore, choosing a disproportionate approach can cause deviation from the goal, and the difference in the results of watershed health can even affect the adoption of a suitable policy for watershed management. For example, based on the results of the absolute approach of this research, the health status of the Kalaji watershed is relatively unhealthy (0.308) which is not satisfactory and an improvement policy may be considered for this situation. Meanwhile, the results of the relative approach indicate a relatively healthy status (0.601) which is almost satisfactory, and the policy of maintaining the status quo may be considered for this situation. So, the difference in the results of the two approaches can lead to changes in the policies adopted for watershed management. The results of this research emphasize that before assessing the health of the watershed, the proportionate approach should be chosen according to the intended goals.

Finally, considering the unsatisfactory health status of the Kalaji watershed, it is suggested that necessary measures be taken to improve this situation. In this regard, the reasons for such status should be analyzed by a cause and effect model (such as drivers, pressures, state, impact, and response (or DPSIR) framework) and appropriate responses can be identified (Salehpour Jam et al. 2021b, 2021a).

There are two categories of watershed health assessment approaches: relative and absolute. Past research has often focused on the relative approach of watershed health. This research aimed to highlight the difference between the results obtained from the relative and absolute approaches of watershed health assessment. So the health status of 25 sub-watersheds of the Kalaji watershed (as a pilot watershed) was assessed based on these two approaches using the key indicators. However, the lack of a WHI monitoring system caused some limitations in the selection of indicators for some watershed health criteria, so some criteria (such as water quality and habitat condition) were indexed with somewhat indirect indicators.

The findings indicated a significant difference in the results of the two approaches. In general, the relative approach provided a higher health index and more healthy class than the absolute approach. In the relative assessment approach, a clear vision of the watershed health is not provided and the health of watersheds is only compared to each other. The results of the absolute approach imply that the health of the Kalaji watershed is not satisfactory and should be improved. So, it is suggested that future studies seek to determine appropriate responses to improve this situation by applying cause and effect analysis (such as DPSIR).

Therefore, the results of this research emphasize that due to the huge difference in the results obtained from the two approaches, it is necessary to be careful in the watershed health assessment process, so that the appropriate approach should be chosen according to the desired goal. Future research can also apply the two approaches presented in this research in other watersheds with different geographical and climatic conditions and highlight the differences in the results of the two approaches. Overall, this study provides a better understanding of the relative and absolute approaches of watershed health assessment and can be considered as a preliminary for the development of these models, especially the absolute ones.

This research which was conducted as a research project with code 124-29-29-018-01033-010622 was jointly supported by the Soil Conservation and Watershed Management Research Institute (SCWMRI) and Gorgan University of Agricultural Sciences and Natural Resources. The authors sincerely appreciate the members of the watershed management group at the SCWMRI for their valuable suggestions. The authors are also grateful to the anonymous referees for their valuable comments.

All relevant data are included in the paper or its Supplementary Information.

The authors have declared that there is no conflict of interest.

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