1) observation well
观测井
1.
The vertical difference of water quality in the observation well is caused by three factors: change of water quality in aquifer during the pumping and injection, the oxidation of the water dody near the surface and the aquifer itself having the vertical hydrogeochemical zones, thus, a dispersion of different concentrations exists.
观测井水质垂向差异由三因素引起:抽、灌水过程中含水层水质改变、近井口表层水体氧化、含水层本身存在水质垂向分带。
2.
The relationship between the drawdown and the time variations defined by the Theis formula was treated as the theoretical true values of the water level changes outside the observation well.
文章针对无界承压含水层中完整井的非稳定流抽水试验,将Theis公式描述的水位降深与时间的变化关系作为观测井外水位变化的理论真值,考虑观测井内外达到水力平衡所引起的滞后时间因素,推导了观测井内水位变化的理论测量值,分析了测量值与真值之间的相对误差以及测量值接近真值所需要的观测时间。
2) cross-borehole observation
井间观测
1.
To cope with the limitation of cross-borehole observation angle, reflection wave is introduced in tomographic inversion.
为了克服井间有限观测角的限制，尝试在层析反演过程中引入反射波信息，并利用VSP观测系统与井间观测系统的相似性，设计了一套地面激发、双井与地面变炮间距接收的地震观测系统，弥补了常规VSP观测信息量不足的缺点，同时较大程度地增加了观测角。
4) borehole observation
井下观测
5) observation wells network
观测井网
1.
Using the Kriging equation, and basing on the data of existing groundwater observation wells, this paper discusses the optimal design of the observation wells network under given objectives.
本文比较系统地论述克立金方法的基本思想 ,结合数学规划方法 ,推导出克立金方程组 ,并以现有的神头电厂贮灰场地下水观测井网的质量评价为基础 ,考虑观测井网优化设计的目的和经费投入量 ,拟定备选方案 ,分别计算出估计误差方差分布 ,经比较分析 ,选取一个最佳方案。
6) observation well of earthquake indications
地震观测井
补充资料：大坝内部变形观测(见水工建筑物变形观测)
大坝内部变形观测(见水工建筑物变形观测)
daba neibubianxing guanCe大坝内部变形观测见水工建筑物变形观测。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条