1) shallow water over-lake
浅水漫湖
1.
The careful observations of core data,logging and 3D-seismic and petrographic analysis reveal that the 2nd member of the Shahejie Formation in the Dawangbei Sag consists of sandy beach and bar of shallow water over-lake.
通过岩心精细的观察,结合测井、三维地震以及岩石鉴定分析等资料的综合研究发现,大王北洼陷沙二段盆地断坳期为浅水漫湖砂质滩坝沉积,可分为:滩、坝主体、坝侧缘、坝间4种沉积微相,其中坝主体的成分成熟度和结构成熟度较高,且坝主体砂层最厚,滩、坝侧缘和坝间砂体次之。
2) Flooded-lake facies
洪水漫湖
3) flood-overlake
洪水-漫湖
1.
It was showed,by cores observation,grain size analysis,logging data and electron microscope observation in Jiyang Paleogene depression,that the sediment of flood-overlake was controlled by ephemeral flood because the lake was shallow and the weather was dry-half dry.
结果表明,济阳坳陷在孔一段到沙四段沉积早期处于湖盆裂陷初期,沉积作用明显受季节性洪水注入影响,在东营、惠民两凹陷形成洪水-漫湖沉积体系。
4) Human reservoir
湖漫水库
1.
Statistics Analysis on Maximun Annual Water Level of Human Reservoir by PPCC Testing;
湖漫水库PPCC检验法的坝前年最高水位统计特性分析
2.
Human reservoir is a key medium reservoir,which prevents floods and supplies water primarily.
湖漫水库是一座以防洪、供水为主的综合利用的重点中型水库,地理位置十分重要。
5) flood-lake facies
洪水-漫湖相
6) 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。
补充资料：河道洪水演进(见河道洪水演算法)
河道洪水演进(见河道洪水演算法)
neaao non郎hUi河道洪水演进yanJ县n 见河道洪水演算法。
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