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1)  lacus subaqueous fan
湖泊水下扇
1.
It is typically developed lacus subaqueous fan of Shuangyang Formation in Moliqing fault subsidence of Yitong Basin in Eocene.
伊通盆地莫里青断陷始新统双阳组发育典型的湖泊水下扇体。
2)  shallow lakes in the middle and lower reaches of the Yangtze Rive
长江中下游浅水湖泊
1.
Phosphate release kinetics characteristics of the sediments from shallow lakes in the middle and lower reaches of the Yangtze Rive;
长江中下游浅水湖泊沉积物磷释放动力学
3)  lake water
湖泊水
1.
To understand the status of the microbiological pollution from the different water body in Jiaxing city by detecting the counts of bacterial, total coliforms, pathogen, fungi and yeasts in water samples collected from riverway water, canal water, lake water and water supply under different circumstance of temperature.
检测嘉兴市市内河道水、运河水、湖泊水、自来水中细菌总数、大肠菌群、致 病菌、霉菌和酵母菌在不同环境温度下的分布,了解嘉兴市城市不同水体微生物污染状况。
2.
Solar radiation has cooperation with biodegradation of the organic pollutants in the lake water.
论述了太阳光对湖泊水体中有机污染物降解作用的研究 ,就其降解机理、动力学特征、作用对象及降解产物等作了逐一介绍。
3.
Survey of potassium,sodium ions in lake water by atomic absorption spectrometry(AAS) was studied in this paper,negative high voltage,lamp current and other instrument settings were optimized.
采用火焰原子吸收/发射光谱法测定湖泊水中的钾、钠离子含量。
4)  salt water lake
咸水湖泊
5)  shallow lakes
浅水湖泊
1.
The attenuation of ultraviolet radiation in shallow lakes in the middle and lower reaches of Yangtze River;
长江中下游浅水湖泊紫外辐射的衰减
2.
Evaluation on temporal and spatial changes of biological integrity for shallow lakes in the middle reach of the Yangtze River;
长江中游浅水湖泊生物完整性时空变化
3.
Adsorption kinetics and isotherms of ammonium onto the 13 sediments taken from shallow lakes in the middle and lower reaches of the Yangtze River were determined, and the effect of physical and chemical properties of the sediments on its ammonium adsorption characteristics was also analyzed.
在室内模拟条件下,研究了长江中下游浅水湖泊13个表层沉积物对氨氮的吸附动力学和热力学特征,并分析了沉积物理化性质对氨氮吸附特性的影响。
6)  shallow lake
浅水湖泊
1.
Plane 2D flow-water quality-sediment pollution couple model in shallow lake;
浅水湖泊平面二维水流-水质-底泥污染模型研究
2.
Fractionation of phosphorus in sediments and its relation with soluble phosphorus contents in shallow lakes located in the middle and lower reaches of Changjiang River, China;
长江中下游浅水湖泊沉积物中磷的形态及其与水相磷的关系
3.
Geochemical characteristics of phosphorus in sediments of a large shallow lake;
浅水湖泊沉积物中磷的地球化学特征
补充资料:湖泊增减水
      因强风作用或气压骤变,表层湖水从湖泊背风岸移至迎风岸的现象。风把动量传给湖水形成漂流,表层湖水便从背风岸移到迎风岸,迎风岸水位上升,即增水现象;同时,背风岸水位下降,即减水现象。湖面气压场骤变,也能引起增减水现象。低压区湖水位升高,称为静压效应,气压下降1百帕,水位约升高1厘米。
  
  1888年J.默里发现成层湖水的水面层向迎风岸抬升,下层向背风岸抬升,提出了湖泊中的增减水现象。20世纪初J.W.桑德斯特勒姆在水槽中试验予以证实。
  
  风力引起增减水时,湖面倾斜,倾斜的湖面反过来阻滞漂流运动,并在下层湖水中形成与漂流流向相反的补偿流(图1)。在深水湖岸,补偿流波及的深度可超过漂流水层的厚度。当湖上风向风速随时间变化,漂流、补偿流的速度,水面倾斜度和增减水水位也随时间变化,称为不稳定增减水;当湖上风向和风速稳定,增减水水位、水面坡度,漂流和补偿流在时间上均是稳定的,称为稳定增减水。在有水流进出的吞吐湖泊中,漂流与补偿流流量可不相等。
  
  
  影响湖泊增减水的因素主要有:①风,包括风速和风向,风速剧烈增大时,大量湖水向增水岸转移,而补偿流来不及将等量的湖水送到减水岸,水位剧烈增加(图2)。如果研究的增减水方向不与风向平行,则须考虑风向的影响。②湖盆形态,在迎风深水湖岸,由于补偿流很大,水位上升较小;而在迎风浅水湖岸,由于浅滩的摩擦作用,补偿流不足以抵消增水的水量,因此水位上升比较大;在狭窄的湖湾和沿盛行风方向伸展的狭长湖泊中,增减水现象特别显著。③湖泊的水位,在同一地点,低水位时增减水现象较高水位时明显。对于水库,影响因素还有流量即上游来水或泄洪。
  
  
  增减水水位变化可实地测量,也可用公式计算。确定增水岸水位高度,对于设计湖岸堤防和港口码头高程等具有实际意义。
  
  

参考书目
   冯士筰编著:《风暴潮导论》,科学出版社,北京,1982。
   G.E.Hutchinson,A Treatise on Limnology,Vol.1,John Wiley & Sons,New York,1957.
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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