测绘通报 ›› 2026, Vol. 0 ›› Issue (2): 24-30.doi: 10.13474/j.cnki.11-2246.2026.0205

• 水陆环境监测与资源评估 • 上一篇    下一篇

塔里木河流域地下水储量的时空演变及其驱动机制

牛芳鹏, 卢震林, 曹彪, 寇靖, 马雪燕   

  1. 新疆维吾尔自治区水利水电科学研究院, 新疆 乌鲁木齐 830049
  • 收稿日期:2025-07-10 发布日期:2026-03-12
  • 通讯作者: 卢震林。E-mail:59963111@qq.com
  • 作者简介:牛芳鹏(1995—),男,硕士,工程师,主要研究方向为水文水资源及地理信息系统与遥感应用研究。E-mail:niufp0225@163.com
  • 基金资助:
    新疆维吾尔自治区公益性科研院所基本科研业务费(KY2024086);中央引导地方科技发展资金(ZYYD2025QY03);新疆维吾尔自治区重大科技专项(2023A02002-4)

Dynamics and driving mechanisms of groundwater storage in the Tarim River basin

NIU Fangpeng, LU Zhenlin, CAO Biao, KOU Jing, MA Xueyan   

  1. Xinjiang Uygur Autonomous Region Water Resources and Hydropower Science Research Institute, Urumqi 830049, China
  • Received:2025-07-10 Published:2026-03-12

摘要: 本文针对我国西北干旱区塔里木河流域水资源稀缺与地下水过度开采等问题,基于遥感与地面观测数据,通过水储分量分解技术构建了该区域地下水储量的精确估算模型,旨在为区域水资源可持续管理提供科学依据。研究整合了陆地水储量(TWS)与地表水等多源数据,经预处理与空间重采样构建统一时空数据集,系统分析了2002—2024年间地下水储量的长期变化趋势、季节波动特征及空间分布差异。结果表明,塔里木河流域地下水储量整体呈显著下降趋势,年均下降速率为-8.6 mm/a(p<0.01),累计亏损量超过198 mm,相当于全流域约2340亿m3 的水量损失。空间上,喀什绿洲、库尔勒灌区和台特玛湖区域地下水消耗尤为严重,年平均下降速率普遍超过-10 mm/a。本文研究为干旱区地下水动态监测与水资源合理配置提供了数据支持,且对后续相关研究具有参考意义。

关键词: 塔里木河流域, 陆地水储量, 地表水储量, 地下水储量, GRACE, 水资源管理

Abstract: This study addresses the issues of water scarcity and groundwater over-exploitation in the Tarim River basin,an arid region in northwestern China.By integrating remote sensing and ground-based observation data,we developed an accurate estimation model for groundwater storage in the region using water storage component decomposition techniques,aiming to provide a scientific basis for sustainable regional water resource management.Multi-source data,including terrestrial water storage (TWS)and surface water,were consolidated into a spatiotemporally consistent dataset through preprocessing and spatial resampling.A systematic analysis was conducted to examine the long-term trends,seasonal variations,and spatial distribution of groundwater storage from 2002 to 2024.The results reveal a significant declining trend in groundwater storage across the Tarim River basin,with an average annual reduction rate of -8.6 mm/a(p<0.01).The total cumulative loss over the study period exceeded 198 mm,equivalent to approximately 234 billion m3 of groundwater depletion for the entire basin.Spatially,the groundwater decline was most severe in the Kashgar Oasis,Korla Irrigation District,and Taitema Lake area,where the average annual loss rates generally exceeded -10 mm/a.This study provides critical data support for dynamic groundwater monitoring and rational water resource allocation in arid regions,while also offering a reference for future related research.

Key words: Tarim River basin, terrestrial water storage, surface water storage, groundwater storage, GRACE, water resource management

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