Land-use/land-cover change (LUCC) in China's seven major basins (SMBs) had a significant impact on the ecosystems, resulting in increasingly prominent contradictions between ecological protection and economic benefits in provinces located upstream and downstream. Therefore, it is urgent to establish inter-basin ecological compensation (EC) mechanisms between provinces in the SMB. Based on five periods of LUCC from 1980 to 2020, the equivalent factor method was applied to evaluate the ecosystem service value (ESV) of the LUCC, and ecological compensation priority sequence (ECPS), horizontal EC (HEC), and vertical EC (VEC) were determined. We found that: (1) The total ESV fell from 11,522 billion yuan (BY) in 1980 to 11,375 BY in 2020. (2) The elasticity index indicated that 1% of LUCC in the SMB resulted in a change of 0.34% in ESV. (3) The province with the highest ECPS was Xizang, with higher ECPS in the SMB southwest and northeast regions. (4) The total VEC was 357.5 BY, with Songhua River Basin and Inner Mongolia having the highest VEC of 134.13 and 97.13 BY, respectively. (5) The total HEC was 103.78 BY. The maximum HEC in the Songhua River Basin was 31.12 BY. Heilongjiang undertook the highest HEC, 31.09 BY.

  • Land-use/land-cover changes (LUCC) in basins from 1980 to 2020 were calculated.

  • Changes in the ecosystem service value (ESV) caused by LUCC were quantified.

  • Inter-basin ecological compensation (EC) between provinces was quantified.

  • Elasticity indicated that 1% of LUCC resulted in an average change of 0.34% in ESV.

  • The total amount of vertical/horizontal EC is 357.5/103.78 billion yuan.

BY

billion yuan

EC

ecological compensation

ECPS

ecological compensation priority sequence

ESV

ecosystem service value

GLP

Global Land Project

HEC

horizontal ecological compensation

IGBP

International Geosphere-Biosphere Programme

IHDP

International Human Dimension Programme on Global Environmental Change

LUCC

land-use/land-cover change

PEB

payment for ecological benefit

PES

payment for ecological services

SDGs

Sustainable Development Goals

SMB

seven major basins

VEC

vertical ecological compensation

The land served not only as a foundation for natural ecosystem processes but was also utilized by humans for diverse purposes (Hao et al., 2012). Land-use/land-cover change (LUCC) encompassed the alterations in land cover resulting from human activities, including land use and management practices (Meyfroidt et al., 2022), which represented the most immediate evidence of human influence on the earth's surface system (Mooney et al., 2013). During the 1990s, driven by the International Geosphere-Biosphere Programme (IGBP) and International Human Dimension Programme on Global Environmental Change (IHDP), LUCC emerged as a crucial aspect of global environmental change (Howells et al., 2013; Magliocca et al., 2015) and sustainable development (Magliocca et al., 2015). With the intensification of global human activities, the early 21st century saw the launch of the Global Land Project (GLP) by the IGBP and IHDP, highlighting the issues of vulnerability and resilience in global LUCC (Popp et al., 2014; Newbold et al., 2015; Meyfroidt et al., 2022). The impact of global LUCC on biodiversity surpassed the planetary boundaries (Steffen et al., 2015; Newbold et al., 2016). The United Nations Sustainable Development Goals (SDGs) 2030 underscored LUCC's significance in achieving sustainable development (Gao & Bryan, 2017; Nagendra et al., 2018; Pretty et al., 2018). Creutzig (2017) advocated for orderly development, utilization, and land management as a global consensus. In China, rapid economic growth and certain land use policies led to particularly complex LUCC (Galic et al., 2012), especially in construction land (Wu et al., 2013b), resulting in significant ecological and environmental issues (Liu et al., 2014). LUCC affected the structure and function of natural elements through key environmental processes such as energy exchange and water cycling, leading to ecosystem changes (Houghton et al., 1999; Sala et al., 2000). As the primary focus of ecosystem change research (Modernel et al., 2016), accurately understanding the ecological and environmental effects of LUCC was crucial for addressing related problems (Liu et al., 2014).

Ecosystems provide essential material and non-material resources necessary for human survival and development (Costanza et al., 1997). Ecosystem services denoted the benefits humans receive from the various functions of ecosystems (Holdren & Ehrlich, 1974; Costanza et al., 1997) and included both direct and indirect contributions to human well-being (Faber & van Wensem, 2012). Assessing and quantifying these ecosystem services (Kang et al., 2016) enhanced our understanding of their functions and the state of sustainable development (Su et al., 2014). Current evaluations of ecosystem service value (ESV) employed diverse perspectives and methodologies, including direct market methods, alternative market methods, hypothetical market valuation, emergy analysis, dynamic modeling evaluation, and the equivalent factor method (Costanza et al., 1997; Wu et al., 2013a; Luo & Zhang, 2014; Zadehdabagh et al., 2022; Li et al., 2023). The equivalent factor method, noted for its simplicity and broad evaluation scope (Sannigrahi et al., 2019), was widely adopted (Zhao & Su, 2022b) and applied to various ecosystems such as farmland, grassland, forest, wetland, and urban areas (Wang et al., 2019; Ping et al., 2021). However, the equivalence factors proposed by Costanza et al. (1997) were not suitable for China. Consequently, Xie et al. (2001) adapted the equivalent factor method to the Chinese context, establishing a localized ESV evaluation system. Chinese scholars have extensively used this localized method to evaluate ESV across different regions and scales (Luo & Zhang, 2014), becoming a standard approach in ESV assessments (Liu & Yang, 2019; Zhao & Mo, 2022a; Zhao et al., 2023).

Ecological compensation (EC), also termed ‘payment for ecological services (PES)’ or ‘payment for ecological benefit (PEB)’ (Pascual et al., 2014; Grima et al., 2016; Wang et al., 2019), was a crucial economic policy tool aimed at internalizing the external costs associated with river water pollution within watershed ecological protection efforts (Yu et al., 2023). By using financial incentives, EC encouraged the maintenance and preservation of ecosystem services, addressing the externalities of environmental benefits resulting from market failures and promoting social development fairness, ultimately achieving ecological protection and benefit goals (Engel et al., 2008). Research on EC primarily focused on theoretical connotations, spatiotemporal allocation, effective fund allocation, willingness to pay, compensation effect evaluation, biodiversity compensation, fairness, and market mechanisms (Wünscher et al., 2008; Börner et al., 2009). Determining EC standards was essential for quantifying EC, requiring rigorous and scientific methods to evaluate the ESV of regions participating in EC schemes (Costanza et al., 2014). Methods for calculating EC amounts included the willingness to pay method (Eskandari-Damaneh et al., 2020; Ren et al., 2020; Zhu et al., 2023), the ESV method (Sheng et al., 2017; Zhong et al., 2020), the opportunity cost method (Engel et al., 2008; Adhikari et al., 2017; Souza et al., 2021), the ecological footprint method (Yang et al., 2020, 2021b), the value theory method (Sheng et al., 2017), the environmental protection total cost method (Adhikari et al., 2017; Zheng et al., 2019), the water resource value method (Wan et al., 2022), the combination accounting method (Alarcon et al., 2017; Costanza, 2020), the game negotiation method (Yi et al., 2021, 2022), the travel cost method (Mäntymaa et al., 2021), the conditional value method (Jiang et al., 2022), the choice experiment method (Sinclair et al., 2021), the market substitution method (Liu et al., 2021), and the equivalent factor method (Costanza et al., 1997, 2014; Wang et al., 2014; Gao et al., 2021). ESV was a critical indicator reflecting regional economic development and ecological environment quality (Hu et al., 2020) and was pivotal in resolving EC issues between basin regions (Liu et al., 2018; Gao et al., 2021). Calculating EC standards based on the ESV method allowed for a comprehensive valuation of regional ecosystems and was highly recognized in EC research (Dai et al., 2020). This was because (1) ESV assessment provided insights into ecosystem structure and function (Li et al., 2022), (2) changes in ESV were closely linked to socioeconomic development (Zhang et al., 2021), and (3) the method incorporated objective LUCC and was suitable for assessing ecological function value in regional and large-scale areas (Wang et al., 2014). Thus, the ESV effectively addressed basin EC issues (Gao et al., 2021).

In 2016, the ‘Guiding Opinions on Accelerating the Establishment of a Horizontal Ecological Protection Compensation Mechanism for the Upstream and Downstream of Basin’ was issued (Ministry of Finance, Ministry of Ecology and Environment, Development and Reform Commission, and Ministry of Water Resources, 2016). The 14th Five-Year Plan for National Economic and Social Development of the People's Republic of China and the Outline of Long-Range Objectives for 2035 highlighted the need to improve the ecological protection compensation mechanism and implement horizontal EC (HEC) in basins (Chinese Government website, 2021). For the Yangtze River Basin, the Ministry of Finance released the ‘Guiding Opinions on Establishing and Improving a Long-Term Mechanism for Ecological Compensation and Protection in the Yangtze River Economic Belt’ in 2018 (Ministry of Finance, 2018). In 2022, the ‘Guiding Opinions on Promoting the Establishment of the Ecological Protection Compensation Mechanism in the Taihu Lake Basin’ was issued (National Development and Reform Commission, Ministry of Ecology and Environment and Ministry of Water Resources, 2022). Regarding the Yellow River Basin, a pilot plan to support and guide the establishment of a HEC mechanism for the entire basin was introduced in 2020 (Ministry of Finance, Ministry of Ecology and Environment, Ministry of Water Resources, and National Forestry and Grassland Administration, 2020). Additionally, in 2022, the ‘Yellow River Basin Ecological Environment Protection Plan’ was published by the Ministry of Ecology (Ministry of Ecology and Environment, National Development and Reform Commission, Ministry of Natural Resources, and Ministry of Water Resources, 2022), along with the ‘Implementation Rules on Establishing a Horizontal Ecological Compensation Mechanism in the Yellow River Basin within the Province’ (Henan Provincial Department of Finance and Henan Provincial Department of Ecology and Environment, 2022). Therefore, it was imperative to establish EC in seven major basins (SMBs) in China.

Research on LUCC primarily examined various administrative scales, including basins, economic zones, and natural regions (Sun, 2012; Yang et al., 2017b; John et al., 2019). LUCC and ESV influenced and limited one another (Luo et al., 2021). Although studies on ESV have been conducted globally (Costanza et al., 1997; de Groot et al., 2012), national (Li et al., 2016), provincial and city (Han et al., 2016), county (Li et al., 2016; Lu et al., 2017), and township levels (Hu et al., 2015), research focusing on the basin scale was relatively scarce. Basins served as vital centers of human civilization, rich in natural resources, and crucial for functions such as climate regulation and soil protection (Cheng & Li, 2015). This study aims to investigate ecological concerns in different regions of the SMB through the lens of ESV, with the following five objectives: (1) to analyze LUCC in SMB between 1980 and 2020; (2) to assess the changes in ESV in response to LUCC; (3) to evaluate the elasticity of ESV changes related to LUCC; (4) to identify inter-basin EC schemes among provinces; and (5) to quantify the amount of HEC and vertical EC (VEC) in the SMB.

This study centered on the provinces and municipalities directly administered by the central government in the SMB region of China as its primary research units (see Figure 1). ESV served as a methodological approach for measuring the ecological environment, relying on remote sensing data derived from the LUCC analysis (Mialhe et al., 2015; Ling et al., 2016). This study used the LUCC data of 1980, 1990, 2000, 2010, and 2020 (from http://www.resdc.cn/), geographic information (from http://bzdt.ch.mnr.gov.cn/), social and economic statistics of 1980–2020 (from the China Statistical Yearbook, the Provincial Statistical Yearbook and the National Economic and Social Development Statistical Bulletin, the China Economic Network statistical database), crop data of 1980–2020 (from the Compilation of National Agricultural Product Cost Benefit Data), and water consumption data of 1980–2020 (from the Provincial Water Resources Bulletin).
Fig. 1

Location of the study area.

Fig. 1

Location of the study area.

Close modal

Calculation of ESV

This study employed the methodology established by Costanza et al. (1997) and refined by Xie et al. (2008), which was tailored for application in China. The unit area ESV for terrestrial ecosystems in China was defined as the average annual value of various ecological service functions provided by different types of ecosystems on a per-unit-area basis. This measurement was essential for estimating the overall regional ESV (Cao et al., 2018). In line with the approaches of Xie et al. (2003, 2008, 2015), this study used the net profit from grain production per unit area of farmland ecosystems as the standard equivalent factor for ESV. The calculation method for ESV is outlined as follows:
(1)
(2)
(3)
where D (yuan/hm2) represents the one standard equivalent factor, Si (%) represents the percentage of the planting area of the ith crop to the total planting area of the three crops, including rice, wheat, and corn, Fi (yuan/hm2) represents the average net profit per unit area of the ith crop, Ai (hm2) is the area of type i ecosystem, ESij represents the ecological service function value of ecosystem category I, and ESVCR (%), ESVend, and ESVstart are the amplitude of change in ESV, the ESV in the end period, the ESV in the start period, respectively.

To assess and quantify the ecological impact of various ecosystem types, this study used national average data on the percentage and net profit per unit area for rice, wheat, and corn from 1990 to 2020. This data led to a D value of 1,404.05 yuan/hm². Using the ESV equivalents per unit area for Chinese ecosystems as proposed by Xie et al. (2008), we calculated the value equivalent for 1 hm² of each ecosystem (Table 1).

Table 1

The value per unit of ecosystem service in China's seven major basins (yuan/hm2/year).

ValueServicesFunctionFarmlandForestGrasslandDesertWater
Market value Provisioning P1: Food production 1,404.05 463.34 603.75 28.07 744.15 
  P2: Raw material production 547.58 4,184.07 505.46 56.17 491.41 
Non-market value Regulating R1: Gas regulation 1,010.92 6,065.49 2,106.08 84.24 716.06 
  R2: Climate regulation 1,361.93 5,714.48 2,190.32 182.53 2,892.34 
  R3: Water conservation 1,081.12 5,742.56 2,134.16 98.29 26,353.99 
  R4: Waste disposal 1,951.63 2,414.97 1,853.34 365.05 20,850.13 
 Supporting S1: Soil formation and protection 2,063.94 5,644.27 3,145.08 238.69 575.66 
  S2: Biodiversity conservation 1,432.12 6,332.26 2,625.57 561.63 4,815.89 
 Cultural C1: Entertainment culture 238.69 2,920.43 1,221.52 336.98 6,233.97 
ValueServicesFunctionFarmlandForestGrasslandDesertWater
Market value Provisioning P1: Food production 1,404.05 463.34 603.75 28.07 744.15 
  P2: Raw material production 547.58 4,184.07 505.46 56.17 491.41 
Non-market value Regulating R1: Gas regulation 1,010.92 6,065.49 2,106.08 84.24 716.06 
  R2: Climate regulation 1,361.93 5,714.48 2,190.32 182.53 2,892.34 
  R3: Water conservation 1,081.12 5,742.56 2,134.16 98.29 26,353.99 
  R4: Waste disposal 1,951.63 2,414.97 1,853.34 365.05 20,850.13 
 Supporting S1: Soil formation and protection 2,063.94 5,644.27 3,145.08 238.69 575.66 
  S2: Biodiversity conservation 1,432.12 6,332.26 2,625.57 561.63 4,815.89 
 Cultural C1: Entertainment culture 238.69 2,920.43 1,221.52 336.98 6,233.97 

Elasticity of ESV change with LUCC

This study used the elasticity coefficient proposed by Song & Deng (2017) to calculate the relationship between LUCC and ESV. The elasticity coefficient was used to measure the percentage change in ESV caused by the percentage change in LUCC rate, and the calculation formula is as follows (Han et al., 2016; Song & Deng, 2017):
(4)
where EEL represents the elasticity, ΔLUTi denotes the area converted to LUCC type i, LUTi is the area of LUCC type i, and T is the period.

Calculation of ecological compensation priority sequence

Wang et al. (2010) introduced the ECPS to pinpoint the most effective areas for EC, considering both regional ESV and economic development levels. This system aimed to optimize the allocation of EC funds and improve overall environmental efficiency. The ECPS is defined as follows (Dai, 2010; Wang et al., 2010):
(5)
where VALN (yuan/hm2) is the non-market of ESV per unit area, and GDPN (yuan/hm2) is the regional gross domestic product per unit area. Provinces with ECPS > 1 are classified as ECPS, while provinces with ECPS < 1 are classified as non-ECPS (Gao et al., 2019).

Calculation of VEC

The central government provided the VEC to local authorities calculated using the formula outlined by Gao et al. (2018):
(6)
where VEC (billion yuan (BY)) is the total amount of EC, ESVnon-market refers to the non-market value of studying regional ESV, K is the conversion coefficient, taken as 15% (Gao et al., 2019).

Calculation of HEC

In a watershed, HEC involved transferring funds between regions without administrative ties. Following the principle of ‘whoever benefits should compensate’, neighboring provinces provided compensation to upstream and downstream areas, while provinces on either side of the basin shared compensation equally (Zhou et al., 2022). The actual benefits for water-receiving areas came from both the ESV associated with water resources transferred from source areas and the compensation due for ESV losses (Lautenbach et al., 2009; Blanchard et al., 2015; Zhu et al., 2017; Du & Gao, 2018; Liagre et al., 2021):
(7)
where HECtheoretically represents the ESV that downstream provinces should theoretically provide compensation, ESVwater is the total of ESV in upstream provinces, ESVwater conservation represents the ESV of four types of water conservation functions in upstream provinces, including forest, farmland, grassland, and desert, I represents the forest interception rate (with a value of 0.25), S represents the evaporation rate of forest land (with a value of 0), Qdownstream water consumption refers to the water consumption of downstream provinces, and Qtotal water consumption refers to the water consumption of the entire watershed.
The amount of HEC funds obtained solely based on ESV assessment in water-receiving areas may make it difficult to gain public recognition and acceptance. Therefore, in determining HEC funds, it was also necessary to consider the economic development level of the water-receiving area and calculate the ESV adjustment coefficient. Due to the close correlation between public awareness and willingness to pay and social development level, the adjustment coefficient of ESV was calculated based on the pearl growth curve model (Pan, 2014):
(8)
(9)
where L is the ESV adjustment coefficient, and En is the Engel coefficient. Finally, the total amount of HEC for downstream provinces can be obtained by multiplying the ESV that should be compensated for in the receiving area by the adjustment coefficient.
Based on all the methods and contents mentioned above, determine the overall framework of this article, as shown in Figure 2.
Fig. 2

Framework for calculating the amount of inter-basin EC between provinces in China based on the ESV.

Fig. 2

Framework for calculating the amount of inter-basin EC between provinces in China based on the ESV.

Close modal

LUCC patterns from 1980 to 2020 in the China basin

In 1980, the forest area was the largest among the SMB (35.38%), followed by farmland (31.27%) and grassland (23.85%), while the other three types of LUCC only accounted for 9.51% (Figure 3). Between 1980 and 2020, the area of water and urban increased, respectively, while farmland, forest, and desert decreased. By 2020, the area of water and urban increased by 1.22 and 72.40%, respectively, while farmland, forest, and desert decreased by 1.33, 3.16, and 11.16%, respectively.
Fig. 3

Spatiotemporal characteristics and transfer matrix of LUCC in SMB.

Fig. 3

Spatiotemporal characteristics and transfer matrix of LUCC in SMB.

Close modal

Spatiotemporal variation of the ESV

In 1980, the total ESV of SMB was 11,522 BY (Figure 4). In 2020, the ESV reached 11,375 BY, a decrease of 1.27% compared to 1980. The contributions of market value and non-market value to ESV were 11.07 and 88.93%, respectively. In the service functions type, regulatory services accounted for the largest proportion at 52.29%. Cultural services had the smallest proportion at 6.81%. In the service functions type, water conservation accounted for the largest proportion at 15.45%. Food production had the smallest proportion at only 3.34%. Among the SMB, YTRB had the highest ESV, with a mean of 4,455 BY (38.91%). HURB had the lowest proportion, with 4.12%. Among the five types of LUCC, forest had the highest ESV, with a mean of 6,930 BY (accounting for 60.53%). Desert had the smallest proportion, with 0.34%. Among the 29 provinces/cities, IM had the highest ESV, with a mean of 1,263 BY (accounting for 11.03%). SH had the smallest proportion, with a value of 0.05%. Overall, the ESV of the seven major watersheds showed relatively small changes in total, value type, service functions type, sub-type, basin, LUCC, and province/city from 1980 to 2020.
Fig. 4

Trends in ESV variation at total, value type, service functions type and sub-type, basin, LUCC, province/city from 1980 to 2020 (Anhui: AH, Beijing: BJ, Cultural services: CS, Fujian: FJ, Gansu: GS, Guangdong: GD, Guangxi: GX, Guizhou: GZ, Hainan: HAN, Hebei: HEB, Henan: HEN, Heilongjiang: HLJ, Hubei: HUB, Hunan: HN, Jilin: JL, Jiangsu: JS, Jiangxi: JX, Liaoning: LN, Inner Mongolia: IM, Ningxia: NX, Qinghai: QH, Provisioning Services: PS, Regulating Services: RS, Shandong: SD, Shanxi: SX, Shaanxi: SHX, Shanghai: SH, Sichuan: SC, Supporting Services: SS, Tianjin: TJ, Xizang: XZ, Xinjiang: XJ, Yunnan: YN, Zhejiang: ZJ, Chongqing: CQ).

Fig. 4

Trends in ESV variation at total, value type, service functions type and sub-type, basin, LUCC, province/city from 1980 to 2020 (Anhui: AH, Beijing: BJ, Cultural services: CS, Fujian: FJ, Gansu: GS, Guangdong: GD, Guangxi: GX, Guizhou: GZ, Hainan: HAN, Hebei: HEB, Henan: HEN, Heilongjiang: HLJ, Hubei: HUB, Hunan: HN, Jilin: JL, Jiangsu: JS, Jiangxi: JX, Liaoning: LN, Inner Mongolia: IM, Ningxia: NX, Qinghai: QH, Provisioning Services: PS, Regulating Services: RS, Shandong: SD, Shanxi: SX, Shaanxi: SHX, Shanghai: SH, Sichuan: SC, Supporting Services: SS, Tianjin: TJ, Xizang: XZ, Xinjiang: XJ, Yunnan: YN, Zhejiang: ZJ, Chongqing: CQ).

Close modal

Elasticity of ESV variation to LUCC

In the four decades, the elasticity relative to LUCC in SMB was 0.62, 0.23, 0.23, and 0.29, respectively, indicating that 1% land area conversion led to an average change in ecosystem value of 0.629, 0.23, 0.23, and 0.29% (Table 2). Among the seven watersheds, HURB had the highest elasticity coefficient, with a mean of 0.45 in the past 40 years. YTRB had the lowest elasticity coefficient, with a value of 0.22. Between 1980 and 2020, the elasticity coefficients of SHRB and PRB increased while other watersheds decreased. Although the elasticity coefficient fluctuates, the response of ecosystem services to LUCC was not significant.

Table 2

Elasticity of ESV variations in response to LUCCs in basins during the periods 1980–1990, 1990–2000, 2000–2010, and 2010–2020.

ElasticitySHRBLRBHRBYRBHURBYTRBPRBAverage
1980–1990 0.04 0.49 0.69 0.90 1.40 0.54 0.31 0.62 
1990–2000 0.31 0.25 0.21 0.43 0.24 0.12 0.05 0.23 
2000–2010 0.18 0.56 0.30 0.26 0.12 0.10 0.10 0.23 
2010–2020 0.90 0.24 0.07 0.10 0.07 0.13 0.50 0.29 
Average 0.36 0.38 0.32 0.42 0.45 0.22 0.24 0.34 
ElasticitySHRBLRBHRBYRBHURBYTRBPRBAverage
1980–1990 0.04 0.49 0.69 0.90 1.40 0.54 0.31 0.62 
1990–2000 0.31 0.25 0.21 0.43 0.24 0.12 0.05 0.23 
2000–2010 0.18 0.56 0.30 0.26 0.12 0.10 0.10 0.23 
2010–2020 0.90 0.24 0.07 0.10 0.07 0.13 0.50 0.29 
Average 0.36 0.38 0.32 0.42 0.45 0.22 0.24 0.34 
Table 3

Inter-basin vertical ecological compensation between provinces in China (BY).

BasinProvince/CityAmount of ECBasinProvince/CityAmount of ECBasinProvince/CityAmount of EC
SHRB HLJ 56.52 YRB IM 13.54 YTRB HUB 4.70 
SHRB JL 9.88 YRB NX 1.15 YTRB HN 7.13 
SHRB LN 0.04 YRB QH 32.31 YTRB JS 0.10 
SHRB IM 67.69 YRB SD 0.05 YTRB JX 7.32 
Total 134.13 YRB SX 2.73 YTRB QH 30.86 
LRB HEB 0.09 YRB SHX 2.51 YTRB SHX 2.31 
LRB JL 2.20 YRB SC 0.37 YTRB SH 0.00 
LRB LN 3.45 Total 66.54 YTRB SC 18.67 
LRB IM 14.83 HURB AH 0.34 YTRB XZ 8.18 
Total 20.58 HURB HEN 0.34 YTRB YN 9.63 
HRB BJ 0.03 HURB HUB 0.05 YTRB ZJ 0.06 
HRB HEB 2.09 HURB JS 0.12 YTRB CQ 1.12 
HRB HEN 0.05 HURB SD 0.34 Total 104.13 
HRB LN 0.07 Total 1.19 PRB FJ 0.25 
HRB IM 1.07 YTRB AH 1.05 PRB GD 1.88 
HRB SD 0.06 YTRB FJ 0.02 PRB GX 15.73 
HRB SX 1.62 YTRB GS 6.00 PRB GZ 3.24 
HRB TJ 0.02 YTRB GD 0.01 PRB HN 0.20 
Total 5.00 YTRB GX 0.51 PRB JX 0.22 
YRB GS 13.59 YTRB GZ 6.18 PRB YN 4.41 
YRB HEN 0.28 YTRB HEN 0.27 Total 25.94 
Grand total 357.50 
BasinProvince/CityAmount of ECBasinProvince/CityAmount of ECBasinProvince/CityAmount of EC
SHRB HLJ 56.52 YRB IM 13.54 YTRB HUB 4.70 
SHRB JL 9.88 YRB NX 1.15 YTRB HN 7.13 
SHRB LN 0.04 YRB QH 32.31 YTRB JS 0.10 
SHRB IM 67.69 YRB SD 0.05 YTRB JX 7.32 
Total 134.13 YRB SX 2.73 YTRB QH 30.86 
LRB HEB 0.09 YRB SHX 2.51 YTRB SHX 2.31 
LRB JL 2.20 YRB SC 0.37 YTRB SH 0.00 
LRB LN 3.45 Total 66.54 YTRB SC 18.67 
LRB IM 14.83 HURB AH 0.34 YTRB XZ 8.18 
Total 20.58 HURB HEN 0.34 YTRB YN 9.63 
HRB BJ 0.03 HURB HUB 0.05 YTRB ZJ 0.06 
HRB HEB 2.09 HURB JS 0.12 YTRB CQ 1.12 
HRB HEN 0.05 HURB SD 0.34 Total 104.13 
HRB LN 0.07 Total 1.19 PRB FJ 0.25 
HRB IM 1.07 YTRB AH 1.05 PRB GD 1.88 
HRB SD 0.06 YTRB FJ 0.02 PRB GX 15.73 
HRB SX 1.62 YTRB GS 6.00 PRB GZ 3.24 
HRB TJ 0.02 YTRB GD 0.01 PRB HN 0.20 
Total 5.00 YTRB GX 0.51 PRB JX 0.22 
YRB GS 13.59 YTRB GZ 6.18 PRB YN 4.41 
YRB HEN 0.28 YTRB HEN 0.27 Total 25.94 
Grand total 357.50 

Calculation of EC

Prioritization of EC

The provinces with higher ECPS included Xizang, Qinghai, Inner Mongolia, Yunnan, and Fujian, which were mainly distributed in the YTRB, the YRB, the PRB, the LRB, and the SHRB (Figure 5). For basins whose source was not in plateau areas, the ECPS for the Haihe and Huaihe rivers was relatively low. The ECPS in China's developed coastal areas and provinces along the delta of the YTRB, PRB, and YRB economic belt was relatively low. The ECPS was higher in the southwest (XZ, QH, and YN) and northeast areas (IM and HLJ). The ECPS in regions with higher levels of economic development was lower than in areas with relatively lower levels of economic development (Zhong & Mi, 2013).
Fig. 5

Priority of inter-basin EC between provinces in SMB.

Fig. 5

Priority of inter-basin EC between provinces in SMB.

Close modal

Vertical ecological compensation

The total VEC for SMB in 2020 was 357.5 BY (Table 3). SHRB had the highest VEC at 134.13 BY (37.52%). HURB had the lowest VEC at 0.33%. In the HRB, Hebei had the largest VEC at 2.09 BY, accounting for 41.76%. In the HURB, Henan had the largest VEC at 0.34 BY (28.85%). In the YRB, Qinghai had the largest VEC at 32.31 BY (48.55%). In the LRB, Inner Mongolia had the largest VEC at 14.83 BY (72.08%). In the SHRB, Inner Mongolia had the largest VEC at 67.69 BY (50.47%). In the YTRB, Qinghai had the largest VEC at 30.86 BY (29.64%). In the PRB, Guangxi had the largest VEC at 15.73 BY (60.66%). Among the 29 provinces, IM had the highest VEC amount at 97.13 BY, accounting for 27.17%. SH, BJ, and TJ had the smallest VEC amount, accounting for less than 0.01%.

HEC between provinces

The total amount of HEC for SMB was 103.78 BY (Figure 6). The SHRB had the largest HEC amount of 31.12 BY, accounting for 29.99%. In the SHRB, the minimum net HEC amount in HLJ was −31.09 BY, while the maximum amount in IM was 19.81 BY. In the LRB, LN's lowest net HEC amount was −9.79 BY, while the highest amount in IM was 7.39 BY. In the HRB, the minimum net HEC amount in BJ was −5.21 BY, while the maximum amount in HEB was 3.56 BY. In the YRB, the minimum net HEC amount in NX was −3.51 BY, while the maximum amount in IM was 3.83 BY. In the HURB, the minimum net HEC amount in JS was −10.03 BY, while the maximum amount in SD was 6.65 BY. In the YTRB, the minimum net HEC amount in JS was −2.87 BY, while the maximum amount in GZ was 2.27 BY. In the PRB, the minimum net HEC in GD was −6.62 BY, while the maximum amount in GX was 2.92 BY.
Fig. 6

Inter-basin HEC between provinces in China.

Fig. 6

Inter-basin HEC between provinces in China.

Close modal

Among the 29 provinces/cities, HLJ undertook the highest HEC amount of 31.09 BY, followed by JS and AH with 13.4 and 9.79 BY, respectively. IM received the highest compensation amount of 31.94 BY, followed by JL and SD, with 13.56 and 7.28 BY, respectively. IM had the highest net HEC amount of 31.18 BY, followed by JL and SD, with 13.52 and 6.75 BY, respectively.

LUCC driving force analysis

LUCC was regarded as a primary driver of global change and a concentrated reflection of human activities on the land surface and environment (Mooney et al., 2013). LUCC influenced not only land productivity but also sustainable development (Mottet et al., 2006) and the global environment (Foley et al., 2005), as well as social and economic changes (Borrelli et al., 2017). Human activities were a significant cause of changes in the earth's ecosystem, with LUCC evolving into a global phenomenon (Tao et al., 2013). The integration of natural and human disciplines in LUCC research became a focal point in global environmental change studies (Yang et al., 2017a; Deng et al., 2018). Changes in land use, such as the conversion of agricultural land to forest land and urbanization, significantly impacted the global ecosystem (Rudel et al., 2005). Analyzing the driving forces behind LUCC was essential. Zhou et al. (2021) observed that from 1995 to 2015, China's farmland and urban areas increased by 1.88 × 106 and 3.41 × 106 km², respectively, with over 80% of urban expansion occurring at the expense of farmland. Between 2010 and 2015, China's built-up areas increased by 24.6 × 103 km², while cultivated land decreased by 4.9 × 103 km², and the total area of forest and grassland decreased by 16.4 × 103 km² (Ning et al., 2018). Kuang et al. (2022) noted that from 2015 to 2020, the total LUCC area in China was 4.50 × 104 km², with a net increase of 2 × 104 km² in urban areas and 1.14 × 103 km² in water areas and a net decrease of 6.51 × 103, 2.53 × 103, and 6.48 × 103 km² in farmland, forest, and grassland, respectively. These findings align with this study's results, showing an increase in water and urban areas by 1.22 and 72.40%, respectively (Figure 3). Rivers, as areas with high human activity, experienced more severe LUCC (Asnake et al., 2021). LUCC was the most direct and objective reflection of human activities on natural ecology. China's land policy evolution has transitioned from strict control of farmland utilization quotas to intensive land use, focusing on land use quality and comprehensive ecosystem protection (Wang et al., 2018). Economic growth, rural migration to cities, land-use management policy changes, ecological protection, restoration projects (such as the Grain for Green Project), and climate change have all driven LUCC in China. However, the main driving forces varied by land use type and geographical location (Zhou et al., 2021).

Reasons for changes in ESV

Natural and socioeconomic factors influenced ESV. Natural factors included climate, elevation, terrain, and precipitation. Climate affected ecosystem services by regulating water and thermal conditions (Braun et al., 2019). Elevation influenced human activities and vegetation distribution, while terrain impacted ecosystem service functions through factors like water storage capacity and light intensity (Wang et al., 2021). Precipitation changes affected soil conservation and hydrological cycling. Socioeconomic factors include land use, population, and economy (Aziz, 2023). From 1990 to 2010, China's terrestrial ESV experienced a significant decline due to ecological protection policies, land development strategies, economic growth, rapid urbanization, and industrialization (Li et al., 2016). China's total ESV fluctuated downward from $3,265.3 billion in 1992 to $3,253.29 billion in 2018, with an annual decrease of $550 million. Human-driven factors had both positive and negative impacts on provincial ecosystems, with per capita GDP, road length, number of researchers, and crop planting area positively correlated with ESV growth, while remaining energy, population, infrastructure, and ecological restoration variables were negatively correlated (Yang et al., 2021a). From 1990 to 2020, the ESV of rivers, lakes, reservoirs, ponds, and swamps in China showed an overall upward trend, with reservoirs and ponds experiencing the most significant growth at 58% (Xu et al., 2023). This study found that the total ESV in SMB decreased from 11,522 BY in 1980 to 11,375 BY in 2020 (Figure 4), consistent with previous studies. Evaluating the ESV of basins was crucial for global ecosystem service evaluation, aiding in understanding ecological evolution and development and helping policymakers in resource allocation and ecosystem management.

Policy implications

In the YRB, Shandong and Henan, as well as Sichuan and Gansu, have established effective EC mechanisms similar to those in Hubei, Hunan, Jiangsu, and Anhui in the YTRB. Based on existing research, the following recommendations are proposed to facilitate EC: (1) Enhance the cross-provincial watershed EC guarantee mechanism, including financial guarantees, public participation, and third-party monitoring and evaluation. (2) Develop a big data platform for ecological environment management and a comprehensive decision-making platform using artificial intelligence and big data technologies to optimize information sharing and decision-making in water environment governance. (3) Create a horizontal transfer payment pathway for EC within basins, clarifying involved parties, compensation standards, and methods. (4) Foster communication and cooperation to build consensus and innovate organizational structures, establishing an authoritative cross-basin coordination agency. (5) Improve inter-provincial cooperation mechanisms, including joint environmental monitoring and unified river basin management systems. (6) Strengthen the legal framework for cross-regional water pollution control through comprehensive legislation.

In 1980, the SMB's largest land area was forest (35.38%), followed by farmland (31.27%) and grassland (23.85%), with other areas comprising 9.51%. By 2020, water and urban areas increased by 1.22 and 72.40%, respectively, while farmland, forest, and desert areas decreased by 1.33, 3.16, and 11.16%. The total ESV of SMB was 11,522 BY in 1980 and 11,375 BY in 2020, a 1.27% decrease over 40 years. 1% land area conversion led to an average ESV change of 0.629, 0.23, 0.23, and 0.29%, respectively. The ECPS was higher in the southwest and northeast regions. The total VEC for SMB in 2020 was 357.5 BY, with the SHRB having the highest VEC at 134.13 BY (37.52%), followed by YTRB and PRB at 104.13 BY (29.13%) and 66.54 BY (18.61%). The total HEC for SMB was 103.78 BY, with the SHRB receiving the most HEC at 31.12 BY (29.99%), followed by YTRB and PRB at 17.91 and 15.08 BY. To ensure effective EC implementation, suggestions include improving the EC guarantee mechanism, building data platforms, establishing transfer payment pathways, fostering communication, enhancing cooperation mechanisms, and strengthening legal frameworks.

The work is supported by the National Natural Science Foundation of China (52309092), the Yellow River Water Science Research Joint Fund (U2243214), the Yellow River Basin Ecological Protection and High-quality Development Joint Study (Phase I) (2022-YRUC-01-0202), the Science and Technology Development Fund of the Yellow River Institute of Hydraulic Research (202112, 202310), the Basic R&D Special Fund of Central Government for Non-profit Research Institutes (HKY-JBYW-2024-08, HKY-JBYW-2021-05), and the Major Science and Technology Project of Henan Province (231100320100, 232102320112).

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

The authors declare there is no conflict.

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