1) saltwater intrusion
咸水入侵
1.
Technology of groundwater recharge against saltwater intrusion: a case study on Guangrao County,Shandong Province;
地下水回灌补源防治咸水入侵技术研究——以山东省广绕县为例
2.
The Carrying Capacity of Water Resources in Changyi City on the Stress of Saltwater Intrusion;
咸水入侵胁迫下的昌邑市水资源承载能力研究
3.
Based on the correlative analysis of field data and one-dimensional numerical model for saltwater intrusion,the impact of water diversion from Xinanjiang Reservoir on river course silting and saltwater intrusion at Qiantang Estuary was discussed.
基于实测资料相关分析以及一维咸水入侵模型,分析了浙北引水对钱塘江河口段江道淤积和咸水入侵的影响。
2) salt water intrusion
咸水入侵
1.
Being the most seriously infected area by salt water intrusion in China,southern Laizhou Bay has a more complicated land use/coverage change and driving mechanism.
在自然因素方面,咸水入侵与土地利用结构特征及其变化方向具有相关性,它是可以综合反映自然驱动因素的代表性因子。
2.
Deterioration of water quality caused by salt water intrusion is the major problem met by development of fresh water resources in coastal zone.
本文选择黄河三角洲利津地区 ,利用三维地下水数值模型 ,分析预测了开采浅层地下淡水引起的地下水动力场的变化和咸水入侵的可能性。
3.
According to the chemical analyses data of the groundwater samples from 129 hydrogeologic drill-holes,and the groundwater mineralization degree data of 1200 wells tested in the field,the hydrochemical environments of the groundwater in the south coast plain of Laizhou Bay,especially the hydrochemical environments of the shallow groundwater in the salt water intrusion area,have been studied.
根据１２９个水文地质钻孔及其地下水水样的水质分析结果和１２００眼井的地下水矿化度野外实测资料，研究了莱州湾南岸平原的地下水水化学环境，尤其是咸水入侵区的浅层地下水水化学环境特
3) salt-water intrusion
咸水入侵
1.
Origin and characteristics of salt-water intrusion disaster in the downstream of Weihe River on the south coast of Laizhou Bay;
莱州湾南岸潍河下游地区咸水入侵灾害成因及特征
2.
This paper indicates the water environment response based on the analysis to the change of land use and land cover change (LUCC) in the salt-water intrusion area of Changyi City,which is located on the lower reaches of the Weihe River: Firstly,the water resource quantity decreases.
通过对潍河下游地区即昌邑市的咸水入侵地区土地利用状况分析,出现了一系列的水环境效应。
3.
The lower reach of Weihe River in the south plain of Laizhou Bay is one of the most typical areas of salt-water intrusion in China.
沉积特征的不同导致潍河以东地区咸水入侵发生早 ,后期变缓 ,为上淡下咸二层水文地质体 ;潍河以西地区咸水入侵主要是 2 0世纪 70年代末期以来在人类活动的干预下大规模的入侵 ,沿古河道入侵距离可达 9～ 10km ,为淡 -咸 -淡三层水文地质体。
4) seawater intrusion
咸水入侵
1.
Being the most seriously infected area by seawater intrusion in China, thedownstream of weihe river has a more complicated land use/cover change andlandscape ecological effects.
潍河下游滨海平原是我国地下咸水入侵灾害最严重的地区之一。
2.
Being the most seriously infected area by seawater intrusion in China, Laizhou Bay southern plain has a more complicated land use/cover change and driving mechanism.
莱州湾南岸平原是我国地下咸水入侵灾害最严重的地区之一。
5) sea salt water intrusion
海咸水入侵
1.
There are not only karst features under the natural conditions but also geological affection of human activity, that is influence and changes of sea salt water intrusion.
其中 ,既有自然环境条件下形成的岩溶特征 ,又有人类活动的地质效应———海咸水入侵的影响和改造。
6) estuary salt water intrusion
河口咸水入侵
补充资料：送潘咸
【诗文】：
时时赍破囊，访我息闲坊。煮雪问茶味，当风看雁行。
心齐山鹿逸，句敌柳花狂。坚苦今如此，前程岂渺茫。
【注释】：
【出处】：
全唐诗：卷543-7
时时赍破囊，访我息闲坊。煮雪问茶味，当风看雁行。
心齐山鹿逸，句敌柳花狂。坚苦今如此，前程岂渺茫。
【注释】：
【出处】：
全唐诗：卷543-7
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