1.
Mechanism Analysis of the Contributing Factors of Salt SubterraneanWater in Alar Area and Ways to Obtain Fresh Water
阿拉尔地下咸水淡化处理的机理分析
2.
Key Techniques Research of CO_2 Storage in Salinity Aquifer
地下咸水层封存CO_2的关键技术研究
3.
CHEMICAL COMPOSITION CHARCATER AND APPLICATION IN AQUACULTURE OF SALT GROUNDWATER IN JIAOZHOU AREA
地下咸水的化学特征及其在水产养殖中的应用
4.
Research of the Optimization on Restoration Schemes of Saline Groundwater at the Low Reach of Dagu River;
大沽河下游地下咸水恢复方案的优化研究
5.
Numerical Simulation of Underground Salt water Changes at the Lower Area of Dagu River in Qingdao
青岛大沽河下游地下咸水体变化的数值模拟
6.
Numerical Analysis of the Saline Groundwater Restoration Scheme in Ligezhuang Region
李哥庄地区地下咸水恢复方案的数值分析
7.
Study on the Dynamic Distribution Characteristic and the Feasibility of Remediation in Coastal Salt Groundwater
滨海地下咸水分布动态特征与治理可行性研究
8.
Discussion of vertical variations of saline groundwater and mechanism in North China Plain
华北平原地下咸水垂向变化及机理探讨
9.
Experiment on the Cultivation of Fugu obscurus in Mixing Underground Brackish Water and Fresh Water
地下咸水兑淡培育暗纹东方鲀仔鱼试验
10.
Exploiting and utilizing saline groundwater can also vacate underground capacity, increase rainfall infiltration, freshen saline groundwater and improve eco-environment.
还可腾出地下库容,增大降雨入渗,淡化地下咸水,改善生态环境。
11.
Subterranean water in Alar area is salty, with high total salinity, and surface water becomes less salty orsaltier with seasonal rhythm.
阿拉尔地区地下水矿化度含量高、咸,地表水也随季节变化时咸时淡。
12.
A study of the characteristics of groundwater circulation and the formation of bitter and saline groundwater in the Qingshuihe Basin in the southern Ningxia
宁南清水河盆地地下水循环特征与苦咸水成因
13.
Effects of brackish water irrigation on soil and crop under different groundwater depths
地下水作用下微咸水灌溉对土壤及作物的影响
14.
Relation between formation of salt-fresh water and water-bearing medium in the plain of Su Bei
苏北平原地下咸淡水形成与含水介质的关系
15.
Research on Exploitation and Utilization of Shallow Groundwater inside Plain Containing Saline-Water
平原有咸水区浅层地下水开发利用研究
16.
Subterranean water in Alar area is salty,with high total salinity,and surface water becomes less salty orsaltier with seasonal rhythm.
阿拉尔地区地下水矿化度含量高、水咸,地表水也随季节变化时咸时淡。
17.
Numcrical Simulation Study of Groundwater Based on FEFLOW and GIS Technology in Xianyang City
基于FEFLOW和GIS技术的咸阳市地下水数值模拟研究
18.
Study on the Irrigation of Summer Maize with Underground Brackish Water from Different Buried Depths
不同埋深地下微咸水用于夏玉米灌溉研究