生态补水背景下融合SWOT等多源数据的北京潮白河地表水-地下水-地表形变的时空效应分析OACHSSCD
Spatiotemporal analysis of surface water-groundwater-surface deformation in Beijing's Chaobai River under ecological water replenishment using SWOT and multi-source data
在新水情背景下,结合新型多源遥感监测数据,识别气候水文过程与人工生态补水共同作用下地表水-地下水-地表形变系统的响应特征,对于深化区域水文过程认识和优化水资源调控具有重要意义.本研究以潮白河顺义段为案例进行分析探讨,通过集成 SWOT卫星、InSAR、实测地下水位、卫星观测气象水文数据等,构建地表水-地下水-地表形变协同分析框架,识别时空响应特征.主要结果表明:SWOT 能够有效获取开阔水库和窄河道的河段尺度水位变化,潮白河水面高程呈现显著的沿程分异,上段升高、中段相对稳定、下段总体下降.研究区地表形变以近稳定模式为主,同时存在持续沉降、阶段性转换和持续回弹等演化模式,形成稳定、沉降与回弹并存的空间格局.气象水分盈亏对土壤水、水库水位和河道水位的响应具有不同时间尺度,地表水对地下水的影响表现出明显的河段选择性和含水层差异,近河非承压水响应较强,而承压水的距离效应不明显.地下水位与 InSAR 累计位移之间的相关性具有显著空间异质性,形变效应受到含水层结构、历史压密和滞后固结等因素共同制约.多源遥感与地面观测的综合集成能够有效提炼二元水循环调控下地表水-地下水-地表形变系统的河段响应、含水层响应和形变模式.相关认识可为生态补水成效评价、地下水恢复监测以及地面沉降风险防控提供参考.
Against the new water regime,identifying the response characteristics of the surface water-groundwater-surface deformation system to the combined effects of climatic and hydrological processes and anthropogenic ecological water replenishment,using new multi-source remote-sensing observations,is important for improving our understanding of regional hydrological processes and optimizing water-resources regulation.Here,the Shunyi reach of the Chaobai River was selected as a case study.By integrating SWOT satellite,InSAR,in situ groundwater levels,and satellite-based meteorological and hydrological data,we established a coordinated analysis framework for surface water-groundwater-surface deformation-identified their spatiotemporal responses.The main results are as follows.SWOT effectively captured reach-scale water-level variations in both open reservoirs and narrow river channels.The water surface elevation of the Chaobai River showed pronounced longitudinal differentiation,increasing in the upper reach,remaining relatively stable in the middle reach,and declining overall in the lower reach.Land deformation in the study area was dominated by a near-stable mode,while persistent subsidence,transitional evolution,and persistent uplift also occurred,forming a spatial pattern in which stability,subsidence,and uplift coexisted.Climatic water balance affected soil moisture,reservoir water levels,and river water levels at different timescales.The influence of surface water on groundwater exhibited clear reach dependence and aquifer contrasts:unconfined groundwater near the river responded more strongly,whereas confined groundwater showed no clear distance effect.The correlation between groundwater levels and InSAR-derived cumulative displacement was strongly heterogeneous in space,and the resulting deformation response was jointly controlled by aquifer structure,historical compaction,and delayed consolidation.The integration of multi-source remote sensing and ground observations effectively revealed reach-specific,aquifer-specific,and deformation-mode-specific responses within the surface water-groundwater-surface deformation deformation system under dual water cycle regulation.These findings provide a reference for evaluating ecological water replenishment,monitoring groundwater recovery,and mitigating land subsidence risk.
宫辉力;王永康;李紫嫣;林何平;王海刚;陈蓓蓓;周超凡;高博
首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048||中国地质环境监测院,北京 100081首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048首都师范大学城市环境过程和数字模拟教育部重点实验室培育基地,北京 100048||首都师范大学资源环境与旅游学院,北京 100048||首都师范大学地面沉降机理与防控教育部重点实验室,北京 100048
天文与地球科学
二元水循环生态补水SWOT卫星地表形变地下水恢复合成孔径雷达干涉测量潮白河
dual water-cycleecological water replenishmentSWOT satelliteland deformationgroundwater recoverysynthetic aperture radar interferometryChaobai River
《上海国土资源》 2026 (3)
29-40,12
国家自然科学基金面上项目(42201081/D0104)
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