The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学数据（DPDC）球变化研究提供了有关硅藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境主的富含有机质的湖沼相积环境、特定的地质、地形条件地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要漫滩相、湖沼相或冲湖相新近积软弱土,结构松散,积零乱,杂,饱水可液化粉细砂层及粉土层较发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学数据库（DPDC）为全球变化研究提供了有关硅藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境为主的富含有机质的湖沼相积环境、特定的质、形条件为下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南区场土主要为漫滩相、湖沼相或冲湖相新近积软弱土,结构松散,积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发,震或动力荷载的作用下有可能发生软土震陷或砂土液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学数据库（DPDC）为全球变化研提供了有关硅藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研，看出还环境为主富含有机质湖沼相积环境、特定地质、地形条件为地下水砷异常。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要为漫滩相、湖沼相或冲湖相新近积软弱土,结构松散,积零乱,成分复杂,饱水液化粉细砂层及粉土层较为发育,在地震或动力荷载作用下有能发生软土震陷或砂土液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学数据库（DPDC）为全球变提供了有关硅藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过，可以看出以还原环境为主的富含有机质的湖沼相环境、特定的地质、地形条件为地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要为漫滩相、湖沼相或冲湖相新近软弱土,结构松,零乱,成分复杂,饱水可液粉细砂层及粉土层较为发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学数据库（DPDC）变化研究提供了有关硅藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境主的富含有机质的湖沼相积环境、特定的地质、地形条件地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要漫滩相、湖沼相或冲湖相新近积软弱土,结构松散,积零,复杂,饱水可液化粉细砂层及粉土层较发育,在地震或动力荷载的作用下有可能发生软土震陷或砂土液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古湖沼学库（DPDC）为全球变化研究提供了有关硅藻植物、古湖沼学其它生态学记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境为的富含有机质的湖沼相积环境、特定的地质、地形条件为地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地为漫滩相、湖沼相或冲湖相新近积软弱,结构松散,积零乱,成分复杂,饱水可液化粉细砂层及粉层较为发育,在地震或动力荷载的作用下有可能发生软震陷或砂液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻学数据库（DPDC）为全球变研究提供了有关硅藻植物数据、学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，以看出以还原环境为主的富含有机质的相积环境、特定的地质、地形条件为地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要为漫滩相、相或冲相新近积软弱土,结构松散,积零乱,成分复杂,饱水粉细砂层及粉土层较为发育,在地震或动力荷载的作用下有能发生软土震陷或砂土。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

藻古湖沼学数据库（DPDC）为全球变化研究提供了有藻植物数据、古湖沼学和其它生态学数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境为主的富含有机质的湖沼相积环境、特定的地质、地形条件为地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地主要为漫滩相、湖沼相或冲湖相新近积软,结构松散,积零乱,成分复杂,饱水可液化粉细砂层及粉层较为发育,在地震或动力荷载的作用下有可能发生软震陷或砂液化。

The Diatom Paleolimnology Data Cooperative (DPDC) is a database of diatom and associated ecological and paleolimnological data useful in studying global change.

硅藻古数据库（DPDC）为全球变化研究提供了有关硅藻植物数据、古和其它生态数据和记录等。

We propose that As anomalism in groundwater possibly resulted from the combined effects of organic matter-enriched lacustrine sediments, geological setting and topographical characteristics.

通过研究，可以看出以还原环境为主的富含有机质的积环境、特定的地质、地形条件为地下水砷异常的原因。

Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.

苏南地区场地土主要为漫滩、新近积软弱土,结构松散,积零乱,成分复杂,饱水可液化粉细砂层及粉土层较为发育,在地震动力荷载的作用下有可能发生软土震陷砂土液化。