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1)  downrange of groundwater depth
地下水位降幅
1.
The results showed that:(1)most of oases lied in 20~30 m of the downrange of groundwater depth which were decreased as circus from north to south in study area;(2)there were the sensitive region in 5~8 m and severe decline area over 10 m;(3)distributing region of nature vegetation countermarched from southwest to northeast,and its reduced area was clo.
综合运用RS、GIS及地理统计学的理论、技术,监测干旱区地下水位降幅对天然植被衰退过程的影响。
2.
Results showed that: data obeyed normal distribution characteristic,structure was up to spherical model, special data was second trend; Most of oases lied in 20-30metres of the downrange of groundwater depth which were decreased as circus from north to south in study area.
基于GIS和地理统计学的理论、方法对所取观测井地下水位降幅数据进行空间分布特征分析。
2)  decline of groundwater level
地下水下降幅度
1.
And the major role causing the decline of groundwater level was calculated on the basis of the above simulations.
同时,由反映农作物灌溉耗水量与地下水埋深变化之间关系的公式得知:灌溉粮食作物引起的地下水下降幅度最大,占总下降幅度的70。
3)  down groundwater
降地下水位
4)  water table depression
地下水水位下降
5)  drawdown [groundwater]
水位下降(地下水)
6)  groundwater level recession
地下水位下降
1.
This paper deals with the essential problems of environmental geology in Zunyi City: pollution, groundwater level recession, land collapse, drought, flood and water logging, and other geological harzards, and provides the measures of prevention and cure for these problems.
本文论述了遵义市的主要环境地质问题:污染、地下水位下降和地面塌陷、干旱和洪涝等。
补充资料:地下水水位观测(见水位观测)


地下水水位观测(见水位观测)


d ixiashui shuiwei guanee地下水水位观测见水位观测。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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