Spatial heterogeneity and integrated management of ecosystem service supply-demand in the tarim river basin

The Tarim River Basin (TRB)—China's largest dryland watershed—was evaluated at 1-km resolution for five benchmark years (2000–2020) to quantify the coupled dynamics of water yield (WY), carbon sequestration (CS) and food provision (FP). CS supply remained essentially unchanged at ≈ 5.5 t hm −2 , yet demand rose from 0.126 to 1.354 t hm −2 , driving the CS supply-demand index (CS_SDI) from 0.955 to 0.605. WY supply peaked at 230.8 m 3 hm −2 in 2005 but fell to 119.6 m 3 hm −2 by 2020, leaving WY_SDI persistently negative (−0.286 to −0.217). FP supply climbed from 0.025 to 0.033 t hm −2 and FP_SDI from 0.351 to 0.473. Spatially, high-supply–low-demand (HL) cells dominate CS (57.8 %) and WY (56.4 %), whereas FP is overwhelmingly low-supply–low-demand (62.8 %), underscoring the disconnect between mountain-front production zones and desert-edge oases. Correlation analysis reveals a strong WY–FP trade-off at city scale (r = −0.66) that weakens or reverses at county (r = −0.19) and grid scales (FP–CS r = +0.30) as crop area expands from 24 537 km 2 to 39 008 km 2 . Overlaying resource pressure, ecological intent and management urgency yields twelve composite zones. The Water-yield × Enhancement × High-priority (WEH) class alone spans 389306 km 2 (43.71 %), identifying where drip-irrigation retrofits, aquifer recharge and river-corridor restoration should be front-loaded. Two further classes—WEM (11.35 %) and CPM (9.00 %)—form a second tier requiring efficiency upgrades and carbon-sink protection. These multi-scale diagnostics provide a basin-wide, data-driven template for reallocating water rights, restoration funds and carbon offsets. • CS demand jumped × 10 (2000–2020), pushing CS_SDI from 0.96 to 0.61 in the TRB. • WY supply fell 48 % after a 2005 peak, from 230.8 to 119.6 m 3 hm −2 by 2020. • HL cells dominate: CS 57.8 %, WY 56.4 %; FP is LL across 62.8 % of the basin. • Cross-scale shifts: WY–FP r = −0.66 (city) but WY–CS r = 0.68 (county). • WEH zone (43.7 %, 389 306 km 2 ) prioritised for drip irrigation and recharge.

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Publication Details

Journal
Environmental and Sustainability Indicators
Published
2025-08-09
DOI
https://doi.org/10.1016/j.indic.2025.100849
Citations
1
Primary Topic
Water Resources and Management
Type
article
Field-Weighted Citation Impact
1.72

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article

Spatial heterogeneity and integrated management of ecosystem service supply-demand in the tarim river basin

Lijuan Jin, Yao Wang, Jiani Li, Denghui Xu et al.
1 citations
Environmental and Sustainability Indicators
Water Resources and Management
1.72
article

Spatial heterogeneity and integrated management of ecosystem service supply-demand in the tarim river basin

Lijuan Jin, Yao Wang, Jiani Li, Denghui Xu, Zhonglin Xu, Tongsheng Fan
article en
1 citations

Abstract

The Tarim River Basin (TRB)—China's largest dryland watershed—was evaluated at 1-km resolution for five benchmark years (2000–2020) to quantify the coupled dynamics of water yield (WY), carbon sequestration (CS) and food provision (FP). CS supply remained essentially unchanged at ≈ 5.5 t hm −2 , yet demand rose from 0.126 to 1.354 t hm −2 , driving the CS supply-demand index (CS_SDI) from 0.955 to 0.605. WY supply peaked at 230.8 m 3 hm −2 in 2005 but fell to 119.6 m 3 hm −2 by 2020, leaving WY_SDI persistently negative (−0.286 to −0.217). FP supply climbed from 0.025 to 0.033 t hm −2 and FP_SDI from 0.351 to 0.473. Spatially, high-supply–low-demand (HL) cells dominate CS (57.8 %) and WY (56.4 %), whereas FP is overwhelmingly low-supply–low-demand (62.8 %), underscoring the disconnect between mountain-front production zones and desert-edge oases. Correlation analysis reveals a strong WY–FP trade-off at city scale (r = −0.66) that weakens or reverses at county (r = −0.19) and grid scales (FP–CS r = +0.30) as crop area expands from 24 537 km 2 to 39 008 km 2 . Overlaying resource pressure, ecological intent and management urgency yields twelve composite zones. The Water-yield × Enhancement × High-priority (WEH) class alone spans 389306 km 2 (43.71 %), identifying where drip-irrigation retrofits, aquifer recharge and river-corridor restoration should be front-loaded. Two further classes—WEM (11.35 %) and CPM (9.00 %)—form a second tier requiring efficiency upgrades and carbon-sink protection. These multi-scale diagnostics provide a basin-wide, data-driven template for reallocating water rights, restoration funds and carbon offsets. • CS demand jumped × 10 (2000–2020), pushing CS_SDI from 0.96 to 0.61 in the TRB. • WY supply fell 48 % after a 2005 peak, from 230.8 to 119.6 m 3 hm −2 by 2020. • HL cells dominate: CS 57.8 %, WY 56.4 %; FP is LL across 62.8 % of the basin. • Cross-scale shifts: WY–FP r = −0.66 (city) but WY–CS r = 0.68 (county). • WEH zone (43.7 %, 389 306 km 2 ) prioritised for drip irrigation and recharge.

Environmental and Sustainability IndicatorsVol. 27
China Meteorological Administration (CN), Beijing Municipal Ecological and Environmental Monitoring Center (CN), Nanning Normal University (CN), Xinjiang University (CN)
Natural Science Foundation of Xinjiang Province, Key Technologies Research and Development Program, National Key Research and Development Program of China
Openalex Percentile: Top 15%
Water Resources and Management
1.72
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