1)saltwater intrusion咸潮入侵
1.Chlorosity,water level and river runoff from each saltwater intrusion observation station are collected in recent years(2004-2006) in Modaomen watercourse of Pear River Estary,south China,when the saltwater intrusion occurs.收集了2004-2006年珠江口磨刀门水道咸潮发生时测站(1~7)逐日定时观测的的含氯度、水位与流量数据,分析了各监测站含氯度与水位的日变化与年变化,导出了咸潮演变各过程中,含氯度与径流、潮流、河口地形等的关系式,建立了珠江口地区磨刀门水道咸潮入侵的经验模型。
2.Qingcaosha Reservoir is a large scale reservoir with the characteristics of special geographic location,complicated topographical and hydrodynamic conditions,intricate law of saltwater intrusion,etc.青草沙水库具有规模大、地理位置特殊、地形、水动力条件及咸潮入侵规律复杂等特点。
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
英文短句/例句
1.Prevention strategies of saltwater intrusion in Binzhou City山东省滨州市咸水入侵防治对策研究
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.Investigation and Studay of Salt Water Intrusion on the South Coast Plain of Laizhou Bay;莱洲湾南岸淄河下游咸水入侵调查与研究
4.3-D Numerical Model for Groundwater and Analysis on Salt Water Intrusion in Yellow River Delta黄河三角洲浅层地下水三维数值模型与咸水入侵分析预测
5.Response of Saltwater Intrusion on Land Use and Soil Quality in the South Coast of Laizhou Bay;土地利用与土壤质量对咸水入侵的响应及其机制研究
6.Retrieval of Land Surface Temperature and Its Response to LUCC and Salt Water Intrusion;基于遥感的地表温度对土地利用变化及咸水入侵的响应
7.The Relation Research of the Sedimentary Environmental Transformation and Saline Water Encroachment in Laizhou Bay South Sea Shore Plain;莱州湾南岸滨海平原沉积环境变化与咸水入侵关系研究
8.The Research of Land Ues Change and Its Ecological Effect in Southern Coastal Saltwater-intruded Area of Lai-zhou Bay莱州湾南岸咸水入侵影响区土地利用变化及其生态效应研究
9.The Evolution Trend of Salinity Intrusion and Analysis of Its Dynamic Factors in Pearl River Delta珠三角咸水入侵变化趋势及其动力因素影响分析
10.Analysis and Trend Forecast of Salt Water Intrusion in Coastal Plain of Laizhou Bay--A Case Study at Guangrao County of Shandong Province莱州湾滨海平原咸水入侵分析与趋势预测——以山东省广饶县为例
11.CHEMICAL COMPOSITION VARIATION IN GROUNDWATER CAUSED BY SALT BRINE WATER INTRUSION AND ITS AFFECTION TO ENVIRONMENT IN WEIFANG AREA潍坊咸-卤水入侵引起的地下水化学成分变化及其对环境的影响
12.STUDY ON THE ANCIENT CHANNELS AND THE RELATIONSHIP BETWEEN THE ANCIENT CHANNELS AND THE SEA (SALT) WATER INTRUSION OF THESOUTH COASTAL PLAIN OF LAIZHOU BAY莱州湾南岸平原古河道及其与海(咸)水入侵关系研究
13.ANALYSIS ON MAN-LAND SYSTEM MECHANISM OF ACTION AND IT S MODELING IN SEA(SALT) WATER INTRUSION ZONE--A CASE ON COAST OF LAIZHOU BAY IN SHANDONG PROVINCE;海(咸)水入侵区人地系统作用机制及调控分析——以山东省莱州湾沿岸地区为例
14.aggressive water腐蚀性水;侵进水;侵入水;侵蚀水;侵蚀性水
15.Soil Water and Salt Transport Features of Saline Water Intermittent Infiltration under Calcium Fertilizer Application施钙条件下微咸水间歇入渗土壤水盐运移特征
16.The drying Aral Sea needs an annual injection of five cubic kilometers of water逐渐干涸的咸海每年需注入五立方公里的水
17."They are related to the Bowfin and date Back to the Eocene Epoch. Gars are confined chiefly to fresh water, though some species enter Brackish or salt water."与弓鳍鱼近缘,在始新世就生活于欧洲和北美。主要栖于淡水,但有的种可降入半咸水甚至咸水。
18.Second, the water in the sea is salty.第二，海水是咸的。
相关短句/例句
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)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。
4)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。
5)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。
6)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。
延伸阅读
咸潮1.海潮。海水咸，故称。
