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Assessment of the Irrigation Water Requirement and Water Supply Risk in the Tarim River Basin, Northwest China

Author

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  • Fei Wang

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
    University of Chinese Academy of Sciences, Beijing 100049, China)

  • Yaning Chen

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China)

  • Zhi Li

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China)

  • Gonghuan Fang

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China)

  • Yupeng Li

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
    University of Chinese Academy of Sciences, Beijing 100049, China)

  • Zhenhua Xia

    (State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China)

Abstract

Studying the relationship between agricultural irrigation water requirements (IWR) and water supply is significant for optimizing the sustainable management of water resources in Tarim River Basin (TRB). However, the related studies have not quantified the total IWR and the imbalance of irrigation water supply and requirements in the TRB. The study analyzed the spatial-temporal variations of IWR by a modified Penman–Monteith (PM) method during 1990–2015. Five major crops—rice, wheat, maize, cotton, and fruit trees—are chosen for calculating the IWR. It was found that the IWR increased significantly, from 193.14 × 10 8 m 3 in 1990 to 471.89 × 10 8 m 3 in 2015, for a total increase of 278.74 × 10 8 m 3 . For the first period (1990–2002), the total IWR remained stable at 200 × 10 8 m 3 but started to increase from 2003 onwards. Significantly more irrigation water was consumed in the oasis regions of the Tienshan Mountains (southern slope) and the Yarkand River (plains). Furthermore, there was an intensified conflict between IWR and water supply in the major sub-basins. The ratios of IWR to river discharge (IWR/Q) for the Weigan-Kuqa River Basin (WKRB), Aksu River Basin (ARB), Kaxgar River Basin (KGRB), and Yarkand River Basin (YRB) were 0.93, 0.68, 1.05, and 0.79, respectively. The IWR/Q experienced serious annual imbalances, as high flows occurred in July and August, whereas critical high IWR occurred in May and June. Seasonal water shortages further aggravate the water stress in the arid region.

Suggested Citation

  • Fei Wang & Yaning Chen & Zhi Li & Gonghuan Fang & Yupeng Li & Zhenhua Xia, 2019. "Assessment of the Irrigation Water Requirement and Water Supply Risk in the Tarim River Basin, Northwest China," Sustainability, MDPI, vol. 11(18), pages 1-16, September.
    • Handle: RePEc:gam:jsusta:v:11:y:2019:i:18:p:4941-:d:265872
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    References listed on IDEAS

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    1. Yang Wang & Shuai Zhang & Hui Zhen & Xueer Chang & Remina Shataer & Zhi Li, 2020. "Spatiotemporal Evolution Characteristics in Ecosystem Service Values Based on Land Use/Cover Change in the Tarim River Basin, China," Sustainability, MDPI, vol. 12(18), pages 1-16, September.
    2. Feng, Meiqing & Chen, Yaning & Duan, Weili & Fang, Gonghuan & li, Zhi & Jiao, Li & Sun, Fan & Li, Yupeng & Hou, Yifeng, 2022. "Comprehensive evaluation of the water-energy-food nexus in the agricultural management of the Tarim River Basin, Northwest China," Agricultural Water Management, Elsevier, vol. 271(C).
    3. Qi Liu & Yi Liu & Jie Niu & Dongwei Gui & Bill X. Hu, 2022. "Prediction of the Irrigation Area Carrying Capacity in the Tarim River Basin under Climate Change," Agriculture, MDPI, vol. 12(5), pages 1-14, April.

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