王子龙, 孙昌鸿, 姜秋香, 刘传兴, 单家珣. 中国东北三省地下水储量时空变化特征及其影响因素分析[J]. 水科学进展, 2023, 34(3): 360-373. DOI: 10.14042/j.cnki.32.1309.2023.03.004
引用本文: 王子龙, 孙昌鸿, 姜秋香, 刘传兴, 单家珣. 中国东北三省地下水储量时空变化特征及其影响因素分析[J]. 水科学进展, 2023, 34(3): 360-373. DOI: 10.14042/j.cnki.32.1309.2023.03.004
WANG Zilong, SUN Changhong, JIANG Qiuxiang, LIU Chuanxing, SHAN Jiaxun. Analysis of spatiotemporal variation characteristics of groundwater storage and their influencing factors in three provinces of Northeast China[J]. Advances in Water Science, 2023, 34(3): 360-373. DOI: 10.14042/j.cnki.32.1309.2023.03.004
Citation: WANG Zilong, SUN Changhong, JIANG Qiuxiang, LIU Chuanxing, SHAN Jiaxun. Analysis of spatiotemporal variation characteristics of groundwater storage and their influencing factors in three provinces of Northeast China[J]. Advances in Water Science, 2023, 34(3): 360-373. DOI: 10.14042/j.cnki.32.1309.2023.03.004

中国东北三省地下水储量时空变化特征及其影响因素分析

Analysis of spatiotemporal variation characteristics of groundwater storage and their influencing factors in three provinces of Northeast China

  • 摘要: 为完善区域地下水开发利用措施、规划区域地下水资源管理, 利用GRACE卫星评估2002—2017年中国东北三省地下水储量变化规律。结合GRACE和GLDAS估算地下水储量变化, 与实测地下水储量变化对比验证, 并探究其影响因素。结果表明: GRACE模拟地下水储量变化与实测地下水储量变化相关性较强, 为0.72; 地下水储量在2013年盈余最大, 2008年亏损最大, 平均增长率为2.23 mm/a, 秋冬两季有明显亏损, 夏季发生盈余; 地下水储量空间分布有明显差异性, 2013年前东北少西南多, 2013年后东北多西南少, 黑龙江省变化较为明显, 辽宁省和吉林省受旱灾影响亏损过多; 降水量和农业用水量变化与地下水储量变化极显著相关, 冬季地下水储量变化与降雪显著相关。研究东北三省地下水储量时空变化对中国乃至全球水资源优化配置和生态环境可持续发展具有参考价值。

     

    Abstract: In order to improve regional groundwater development and utilization measures and to aid regional groundwater resource management, groundwater storage variability characteristics were assessed using GRACE data in three provinces of Northeast China from 2002 to 2017. GRACE and GLDAS data were combined to estimate groundwater storage variations. The estimated groundwater storage variations were verified using measured groundwater storage variations and the factors influencing groundwater storage variations were explored. The results showed that the correlation between groundwater storage variations estimated by GRACE and the measured groundwater storage variations was strong, with a correlation coefficient of 0.72. Groundwater storage variations increased significantly at the end of 2011, and the average growth rate was 2.23 mm/a. The largest surplus in groundwater storage was at the end of 2013, and the largest deficit was at the beginning of 2008. There was an evident loss in groundwater storage in the winter and autumn, and an evident surplus in the summer. Furthermore, there were differences in the spatial distribution of groundwater storage. In 2002—2012, there was less groundwater storage in the northeast than in the southwest, and in 2013—2017 there was more groundwater storage in the northeast than in southwest. There were evident groundwater storage variations in Heilongjiang Province. Furthermore, due to drought, there were significant losses in groundwater storage in Liaoning Province and Jilin Province. Groundwater storage variations were strongly correlated with changes in precipitation and had the strongest correlation with agricultural irrigation, with a correlation coefficient of 0.58. In the winter, groundwater storage variations were the most significantly correlated with snowfall, with a correlation coefficient of up to 0.426. By studying the spatiotemporal variability characteristics of groundwater storage in three provinces of Northeast China, this study aims to provide a reference for the optimal allocation of water resources and the sustainable development of the environment in China and globally.

     

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