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The latest developments of the remote sensing of lake water quality, such as the mathematic methods for the remote sensing of water quality model, the water quality indicators with the most sensible wave band and applications of TM, SPOT, MODIS, MERIS, AVHRR, CASI etc., the satellite sensors and the airborn remote sensing, as well as reasons and solution which probably result in the errors of remote sensing of the lake water quality model, are explicated and analyzed.

详述了湖泊遥感水质最新发展动态,如遥感水质模型的数学方法、与水质指标最敏感的波段以及TM、SPOT、MODIS、MERIS、AVHRR、CASI等传感器的适用情况,并分析了可能导致湖泊水质遥感模型误差的原因和解决办法。

The article is passed laky to the world the introduction with saline resource, and the treatise that develops saline resource to the mankind, try to explain laky the main effect that be produced in salt industry and produces in human life.

本文通过对世界湖泊和盐湖资源的介绍,以及对人类开发盐湖资源的论述,试图说明湖泊在盐业生产和人类生活中所发挥的重要作用。

Wetlands could be classified into 6 types that they are marine, estuarine, lacustrine, riverine wetlands along rivers and streams, palustrine (wetlands in marshes, swamps and bogs and artificial.

湿地可分为6大类──海洋、河口三角洲、湖泊(包括与湖泊有关连的湿地)、河滨(包括与河溪相关连的湿地)、淡水(包括位於沼泽、草泽及苔地的湿地)和人工湿地。

The results showed that pH of the irradiated sediment core is higher than the unsterilized one,and microorganisms could have an effect on the pH of sediments.All the four sediments are in the strong reductive environment at the depth of 7~30 cm,and the values of Eh are quite closer,the main factor that affect the redox environment may be the compaction of the sediment.All the sediments had a cumulation of phosphorus at the surface layer,and the total phosphorus of the sediments at the depth of 4~10 cm are lower than the average.It is indicated that phosphorus had been redistributed at the suface layer.

本研究采集太湖梅梁湾沉积物,通过印Co.y射线辐照、添加可溶性淀粉等处理研究微生物活性对太湖沉积物pH,Eh及总磷分布影响,以揭示微生物在湖泊沉积物中的沉积后作用,为探索富营养化湖泊表层沉积物磷的归趋提供理论基础。1 材料与方法1.1 样品采集和处理2005年1 1月,采用自制的柱状采泥器采集太湖梅梁湾沉积物,采样位点为31.30.306 N.120.13.370 E,采集后立即带回实验室,其理化性质见表1。

Diaojiaohaizi is a thoroughly closed basaltic depression lake on the top of Daqing mountains which has many advantages when it is used in studding vegetational evolution and climatic changes of the Holocene.

调角海子为大青山顶部的一个全封闭的玄武岩洼地湖泊,冰后期积水成湖,其湖泊沉积物具有用来研究全新世植被和气候变化的许多独特优点。

Results The damp fans, rivers and lakes are main sedimentary systems in Yanqi Basin. They are funned from T(subscript 2-3) to J2, including Xiaoquangou, Badaowan, Sangonghe, Xishanyao and Toutunhe age. The rivers and lakes sedimentary systems are good development. The rivers sedimentary systems are divided into braided stream and meandering stream.

结果 潮湿扇、河流和湖泊沉积体系是焉耆盆地的主要沉积体系类型,它们形成于中晚三叠世至中侏罗世的小泉沟、八道湾、三工河、西山窑和头屯河期;其中的河流沉积体系和湖泊沉积体系较为发育,河流沉积体系分为辫状河和曲流河两种类型。

Although the lakes were probably created by volcanic activity, meteorite impacts or shifts in the orbit of the planet, they would have created warmer conditions leading to the melting of ice which would have created rives and filled lakes.

尽管这些湖泊可能产生自火山活动、陨石影响或星球运行轨迹的变更,但这些可能造就了温暖的环境,并导致冰的大量融化,从而产生了河流并填充了湖泊。

Up to now, people are still not clear on many problems, such as how does the contamination move and scavenge itself in lakes, and under what conditions will the pollutant that has been scavenged pollutes the water body again.

人们至今还无法彻底弄清楚污染物在湖泊水体中是如何迁移转化的,污染物又如何的发生自净化作用,又会在什么样的条件下对湖泊产生二次污染等一系列问题。

It was revealed that for the period from 1952 to 1998, the effect on the rise of water level was 2 to 10 times higher as by the cause of silts than by cultivation.

结果显示,1952~1998年的47年间,洞庭湖湖泊湿地围垦对江湖洪水位升高影响的相对量是湖泊淤积对江湖洪水位升高影响值的2~10倍。

The result shows that the level of the water quality in Wuliangsuhai Lake has been close to the fifth level from 2003 to 2005. Based on the grass type lakes character and economic loss rate of water due to pollution, the damage extent of utilizing functions of water in Wuliangsuhai Lake is assessed though investigation, monitoring and analysis from 2003 to 2005. Results show that water in Wuliangsuhai Lake has not been suitable for serving as a water source for drinking and swimming.

选用L.D詹姆斯的污染损失—浓度模型,根据2003年~2005年乌梁素海实测水质资料,对乌梁素海湖泊使用功能损害程度进行评价表明:乌梁素海水已不适宜作为饮用水源和游泳用水,作为人体非直接接触的旅游娱乐用水及渔业养殖用水也受到严重威胁(中损害,2003年为重损害),乌梁素海湖水作为一般居住环境用水呈现逐年改善的趋势(重损害→中损害→轻损害),湖泊功能整体损害程度相当严重。

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