华北平原深层地下水可更新性与水位管控探讨OA
Discussion on renewability of deep aquifer and water level control in the North China Plain
结合已有研究,讨论大规模开发利用作用下,华北平原深层地下水循环及补排路径的变化,并从山前侧向量现场试验、浅层和深层地下水水位变化同步性、咸淡水界面下移、地下水年龄和水化学分析等方面,论证了深层地下水在开采条件下具有一定可更新性.辨析了可更新性与可开采性的关系,认为尽管具有一定可更新性,但华北平原深层地下水开采仍应严格管控以避免地质环境风险.研究提出现阶段必要开采时深层地下水水位控制阈值,以期为现阶段深层地下水开发利用和保护提供参考借鉴.
Based on the existing researches,discussions are made on the changes of deep aquifer circulation and recharge and drainage paths in the North China Plain under the effect of large-scale development and utilization.It demonstrates that deep aquifer has certain renewability under mining conditions from the aspects of vector field test in front of mountains,synchronization of shallow and deep groundwater level changes,downward movement of salt and fresh water interface,groundwater age and hydrochemical analysis.With analysis of relationship between renewability and exploitability,it is found that although the aquifer has certain renewability,the exploitation of groundwater in the North China Plain should be strictly controlled to avoid geological environmental risks.The study proposes a threshold for controlling the water level of deep aquifer when groundwater extraction is necessary,so as to provide insights for the utilization and protection of deep aquifer.
陆垂裕;赵勇;刘蓉;刘淼;吴初;严聆嘉
中国水利水电科学研究院 流域水循环模拟与调控国家重点实验室,100038,北京河北省水利科学研究院,050057,石家庄
水利科学
深层地下水可更新性可开采性低风险开采华北平原
deep aquiferrenewabilitymineabilitylow risk miningthe North China Plain
《中国水利》 2024 (007)
22-27 / 6
国家重点研发计划(2023YFC3206501);水利部重大科技项目(SKR-2022054).
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