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1)  Inner Lake
内湖
1.
The Inner Lake in Zhenjiang City was taken as an research area.
以镇江内湖为例,基于洪、枯两季典型全日潮野外同步实测结果,运用灰色系统理论,定量计算了内湖水体透明度与相关环境因子的灰关联度,分析研究了不同时间尺度下内湖透明度的主要影响因子。
2.
Through comparative analysis of cage fish culture effects, the paper proved that the fish species that have high request for water quality can suit for river cage fish-culture and that the fish species that can endure low level oxygen can suit for rich inner lake fish culture.
通过网箱养殖效果的比较分析 ,证实对水质要求较高的鱼种适合江河网箱养殖 ,而耐低氧的鱼类 ,则适合肥沃的内湖
2)  inland lakes
内陆湖泊
1.
Starting with the opinion on the variation of climate and environment, it comments and introduces the current situation of the research on forecast of variation of water level of inland lakes affecting the safety of railway operation, and forecasts the future work as well.
本文从气候和环境变化的观点着手,对威胁铁路安全运营的达布逊湖等内陆湖泊水位变化预测的研究现状加以评述,并对今后的工作予以展望。
3)  Inland lake
内陆湖泊
1.
Inland lake water quality remote sensing differs from ocean color remote sensing, which demands remote sensing data with high spatial & spectral resolution and complex inversion algorithm.
介绍了内陆湖泊水质遥感监测的特点及遥感监测水质的机理,总结了国内外近年来用于内陆湖泊水质参数反演的 3种常用方法:经验模型、生物光学模型和神经网络模型,并分析了 3种模型的优缺点;同时指出了影响内陆湖泊水质遥感监测精度的关键因素;提出了内陆湖泊水质遥感监测研究重点和方向。
2.
According to the measured data of typical inland lakes in northwest China, this research has revealed the characteristics of lake evolution and their mechanismduring the past 40 years.
利用40年来的实测数据研究揭示了西北典型内陆湖泊的演化特点及机制。
4)  harnessing of the lake water
湖内治理
5)  Inland lake buffering
内湖调蓄
6)  flows-in lake basin
内流湖盆
1.
The physical geography environment,the forming and distributing of the water resource in Ali area of Tibet are analyzed,basing on the difference of the groundwater resource forming environment,the water circulation system can be divided into alluvium and diluvium groundwater of rivervale in south and flows-in lake basin groundwater in north.
分析了西藏阿里地区自然地理环境、水资源形成和分布及其利用状况,基于区内地下水资源形成环境条件的差异,本区地下水资源体系可分为南部河谷冲洪积层地下水系统和北部内流湖盆地下水系统。
补充资料:内湖

bay, laguna de

菲律宾最大的湖泊。面积922平方公里(356平方哩)。位於吕宋岛,马尼拉东南,湖长约51公里(32哩),呈新月型。可能由於火山喷出物将原为马尼拉湾深入内地水域堵塞分离而成。有很多溪流注入,湖盆淤积变浅。湖水经巴石河(pasig river,长16公里〔10哩〕)排入马尼拉湾。雨季暴雨时,湖区低地常被洪水淹没。北岸有两个半岛;湖中多岛屿,其中面积最大、人口最多的塔利姆(talim)岛长14公里(9哩),宽1.6公里(1哩)。湖南岸的圣克鲁斯(santa cruz)、比尼扬(binan)和卡兰巴(calamba)是繁荣的城镇。

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