1) shallow-water lacustrine basin
浅水湖盆
1.
Low permeable oil field of large shallow-water lacustrine basin in China is one of the important exploration areas.
我国大型浅水湖盆中低渗透储层是十分重要的勘探领域之一,该文以松辽盆地扶杨油层为例,系统论述了低渗透储层的特点、成藏条件及勘探难点,提出了利用地质和地震相结合,有效预测主力河道发育区和含油相对富集区的方法体系,形成了一套在低渗透储层中“贫中找富”的勘探思路及技术对策。
2) compressed shallow-lake basin
压性浅水湖盆
1.
Study on the sedimentary systems of compressed shallow-lake basin:taking middle—lower Jurassic in Turpan Depression as an example
压性浅水湖盆沉积体系——以吐鲁番坳陷中下侏罗统为例
3) closed depression shallow lacustrine basin
闭塞浅水坳陷湖盆
1.
The sedimentary tectonic sets belong to closed depression shallow lacustrine basin,and the stratigraphic sequence is similar to that of a craton basin and a gentle slope divergent continental margin.
松辽盆地泉四段扶余油层发育浅水湖泊三角洲相和浅水湖泊相,沉积构造环境属于闭塞浅水坳陷湖盆,其层序特征类似于稳定克拉通盆地层序,也类似于缓坡被动大陆边缘型盆地层序,气候是控制陆相坳陷盆地层序形成的主要因素,三级层序内总体应表现为水进体系域-高位体系域构成1个完整的层序,而低位体系域不发育。
4) shallow lake
浅水湖
1.
Total phosphorus (TP), inorganic-phosphorus (IP), organic-phosphorus (OP), Fe/Al-bound phosphorus (Fe/Al-P) and Ca-bound phosphorus (Ca-P) in surface sediment of the seven shallow lakes along the middle-lower reaches of the Yangtze River were measured, using the standard measurement and test(SMT)procedure of phosphorus forms in the freshwater sediments.
对长江中下游7个浅水湖泊的表层沉积物,应用淡水沉积物中磷形态的标准测试程序(SMT)测定了其中的总磷、无机磷、有机磷、铁/铝磷和钙磷等5个部份,分析了各形态磷之间以及各形态磷与沉积物理化性质如总氮、有机质、主要氧化物组成之间的相关性。
2.
The mechanisms of shallow lakes eutrophication were also complex.
我国浅水湖泊面临严重的富营养化，而沉积物-水界面磷的行为研究是揭示湖泊富营养化机理的重要一环，为我国富营养化浅水湖泊的治理与管理提供指导和理论依据。
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：湖盆
| 湖盆 lake basin 地表上汇集水体的相对封闭的洼地。形似盆状。湖盆成因有地壳运动形成的，如断陷湖盆、坳陷湖盆；还有外力作用形成的，如冰蚀湖盆、堆积湖盆等，此外也有人类经济活动形成的，如水库库区等。湖盆可以由5部分组成：湖岸、沿岸带、岸边浅滩、水下斜坡、湖盆底。湖泊面积的大小，湖盆地质条件和水流动态不同，湖盆的形态也有差异。研究湖盆的形态及其变化，有助于了解湖泊的起源、发展；湖泊的容积、湖水的理化性质和水文形势的变化。 |
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