华北平原(曲周)盐碱地区地下水资源现状研究  

Groundwater Resources of Salt Lick and Alkaline Soil in Quzhou County of North China Plain

作　　者：严云[1] 曾宪竞[1] 王雁萍[1] 牛建国 

机构地区：[1]中国农业大学资源与环境学院,北京100094 [2]河北省曲周县农牧局土肥站,河北曲周057250

出　　处：《农业环境科学学报》2007年第B03期188-192,共5页Journal of Agro-Environment Science

摘　　要：华北平原曲周地区曾经是典型的盐碱地区,在对该地区的农用机井情况进行大量实地调查的基础上,总结了该地区目前的地下水埋深状况,并根据研究统计资料与30 a前的地下水埋深状况进行了比较分析。研究发现,曲周地区的潜水层埋深以0.7 m.a-1的速度直线下降,进一步分析了当地地下水埋深下降的主要原因,为当地加快节水农业,保持水资源的可持续利用提供依据。As the district of Quzhou of Huabei Plain is a typical alkaline land, we investigated distribution of wells, researched groundwater resource situation in the region, and made a comparison between the present status of water resource and the status of 30 years ago, according to the statistical data of this study. The result showed that the present depth of free - water layer of Quzhou County descend with a velocity of 0.7 m · a^-1. Based on these work, this paper then analyzed three main reasons of the descending velocity of the ground water table and provided several references for quickening development of agriculture based on saving water and realizing sustainable use of water resource.

关 键 词：盐碱地 地下水埋深 下降速度 

分 类 号：X523[环境科学与工程—环境工程]