shallow lake

With the development of urbanization, the aquatic environment of shallow lake has become worse and worse.

随着城市化进程的加快, 城市浅水湖的水环境不断恶化,湖泊水环境治理刻不容缓.

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A standard and a comprehensive health index ( I_ ( Ex)) for evaluating ecosystem health of a shallow eutrophic lake were given.

在此基础上，提出了富营养化浅水湖泊生态系统健康指标阈值和湖泊系统能量健康指数（IEx）及其健康状况分级。

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The transform and interrelationship of different form P among water, sediment and Hydrilla verticillata were studied in the imitated shallow-lake environment condition by cultivation Hydrilla verticillata in indoor and greenhouse, the transform mechanism and influence factor of different form P was also probe into.

本文在室内和温室内模拟浅水湖泊环境培养黑藻，通过研究水-沉积物-黑藻中不同形态磷的转化及其相互关系，揭示不同形态磷在水-沉积物-沉水植物体系中的转化机理和影响因子。

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Reflections on the Theory and Practice of Shallow Lake Ecosystem Restoration

浅水湖泊生态系统恢复的理论与实践思考

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Experimental Study on Phosphate Release from Sediments of an Urban Shallow Lake

城市浅水型湖泊底泥磷释放特性实验研究

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Application of MODIS_NDVI to monitoring locust pest in Baiyang Shallow Lake

MODIS NDVI在白洋淀蝗虫害监测中的应用

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A water quality systematical filter model and its algorithm in a shallow lake have been established.

本文建立了浅水湖泊水质系统滤波模型和相应算法.

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The hydrocarbon generating assemblage can be divided into two types of cannel boghead deep lake mudstone and humic coal cannel coal shallow lake mudstone in this basin.

生烃组合分为烛藻煤深湖相泥岩和腐殖煤烛煤浅湖相泥岩两种类型。

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Submerged macrophytes is key community in shallow lake ecosystem. It plays important role in water environmental quality and aquicolous ecosystem structure.

沉水植物是浅水湖泊生态系统的关键种群，对水环境质量及水生生态系统结构有重要影响。

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Delt-front acclivity and shallow lake are a major type of sedimentary sub-facies of the Suining formation of Upper Jurassic, and the provenance is uplifted area of Longmenshan.

洛带气田遂宁组主要为三角洲前缘斜坡亚相和浅湖亚相沉积，其物源区为龙门山隆起区。

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The facies includes alluvial fan, fan-delta, offshore lake, shallow lake and deep lake facies.

沉积相类型包括:冲积扇相 、 扇三角洲相 、 滨湖相 、 浅湖相、深湖相.

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Es 4 in this area belongs to shallow lake deltaic deposit, with sandstone mainly of channel sand, interbasin sand, frontal sand and far bar.

该区Es4段属于浅水湖泊三角洲沉积，骨架砂体为河道砂、河道间砂、前缘砂（席状砂）、远砂坝。

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TP was determined as the primary factor triggering the regime shift of shallow lake ecosystem.

确定总磷是浅水湖泊生态系统稳态转换的最主要驱动因子。

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Lakeshore and shallow Lake deposits are main microfacies types of lake facies.

滨、浅湖相构成了湖泊相的主要亚相类型.

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