国家地下水监测工程数据在地下水动态月报评价中的应用效果浅析
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摘要
地下水动态月报是水利部门定期发布地下水情的重要平台之一,传统的地下水监测数据收集方法使得月报发布存在滞后明显的现象。国家地下水监测工程(水利部分)的建设为月报编制工作提供了更加及时、覆盖面更广的监测网络和数据信息。选取江苏北部平原区与辽宁中部平原区为代表,对比分析了国家地下水监测工程监测数据与传统人工上报地下水数据,定量描述了两类数据表达区域地下水埋深空间分布特征的差异。研究表明,国家地下水监测工程的地下水监测站点分布和数量要优于历史人工测站的分布情况。
The monthly report of groundwater dynamics is an important production showing the groundwater regimen in the main plains of the North China released by Ministry of Water Resources.The traditional method of manual collecting made serious delay of the monthly report publication.Parts of the national groundwater monitoring project,constructed by Ministry of Water Resources,provide a more extensively monitoring network and timely groundwater monitoring data.In this paper,the northern plain of Jiangsu and the central plain of Liaoning were selected as two cases.The two kinds of data sources of the monitoring data collected from the national groundwater monitoring project and the traditional method were comprehensively analyzed,and the differences in the spatial distribution of the groundwater depth were quantitatively described.This research shows that the spatial distribution and quantity of the groundwater monitoring stations in the national groundwater monitoring project are better than those derived from the manual stations.
The monthly report of groundwater dynamics is an important production showing the groundwater regimen in the main plains of the North China released by Ministry of Water Resources.The traditional method of manual collecting made serious delay of the monthly report publication.Parts of the national groundwater monitoring project,constructed by Ministry of Water Resources,provide a more extensively monitoring network and timely groundwater monitoring data.In this paper,the northern plain of Jiangsu and the central plain of Liaoning were selected as two cases.The two kinds of data sources of the monitoring data collected from the national groundwater monitoring project and the traditional method were comprehensively analyzed,and the differences in the spatial distribution of the groundwater depth were quantitatively described.This research shows that the spatial distribution and quantity of the groundwater monitoring stations in the national groundwater monitoring project are better than those derived from the manual stations.
引文
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[3]张远东,王策.地下水取用水总量与水位双重控制刍议[J].中国水利,2014,(9):7-9.(ZHANG Yuandong,WANG Ce.Dual control on total volume and level of groundwater consumption[J].China Water Resources,2014,(9):7-9-66.(in Chinese))
[4]高志.国家地下水监测工程站网布设浅析[J].地下水,2012,34(5):71-72.(GAO Zhi.Analysis of network layout of national groundwater monitoring project[J].Ground Water,2012,34(5):71-72.(in Chinese))
[5]朱金峰,章树安,戴宁,等.地下水水资源量监测分析技术应用探讨[J].水文,2017,37(3):58-62.(ZHU Jinfeng,ZHANG Shuan,DAI Ning,et al.Application of groundwater resources monitoring and analysis technology[J].Journal of China Hydrology,2014,37(3):58-62.(in Chinese))
[6]中华人民共和国水利部.水利部2010年政府信息公开工作年度报告[R].2011.(Ministry of Water Resources of the People's Republic of China.2010 annual report of government information disclosure by Ministry of Water Resources[R].2011.(in Chinese))
[7]严宇红,周政辉.国家地下水监测工程站网布设成果综述[J].水文,2017,37(5):74-78.(YAN Yuhong,ZHOU Zhenghui.Introduction to network layout of national groundwater monitoring project[J].Journal of China Hydrology,2017,37(5):74-78.(in Chinese))
[8]吕连宏,张征,迟志淼.等.地质统计学在环境科学领域的应用进展[J].地球科学与环境学报,2006,28(1):101-105.(LV Lianhong,ZHANG Zheng,CHI Zhimiao,et al.Application and development of geostatistics in environmental sciences[J].Journal of Earth Sciences and Environment,2006,28(1):101-105.(in Chinese))
[9]陶月赞,郑恒强,汪学福.用Kriging方法评价地下水监测网密度[J].水文,2003,23(2):46-48.(TAO Yuezan,ZHENG Hengqiang,WANG Xuefu.Assessment for density of groundwater network using kriging[J].Journal of China Hydrology,2003,23(2):46-48.(in Chinese))
[10]鲁程鹏,束龙仓,张颖,等.稀疏数据插值问题的回归克里格方法[J].水电能源科学,2009,27(1):81-84.(LU Chengpeng,SHU Longcang,ZHANG Ying,et al.Regression kriging method for sparse data interpolation[J].Water Resources and Power,2009,27(1):81-84.(in Chinese))