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Spatial-temporal Characteristics of Land Subsidence Corresponding to Dynamic Groundwater Funnel in Beijing Municipality,China 被引量:14
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作者 CHEN Beibei GONG Huili +5 位作者 LI Xiaojuan LEI Kunchao ZHANG Youquan LI Jiwei GU Zhaoqin DANG Yanan 《Chinese Geographical Science》 SCIE CSCD 2011年第6期753-764,共12页
Due to long-term over-exploitation of groundwater in Beijing Municipality, regional groundwater funnels have formed and land subsidence has been induced. By combining a groundwater monitoring network, GPS monitor- ing... Due to long-term over-exploitation of groundwater in Beijing Municipality, regional groundwater funnels have formed and land subsidence has been induced. By combining a groundwater monitoring network, GPS monitor- ing network data, radar satellite SAR data, GIS and other new technologies, a coupled process model based on the dy- namic variation of groundwater and the deformation response of land subsidence has been established. The dynamic variation of groundwater fimnels and the land subsidence response process were analyzed systematically in Beijing. Study results indicate that current groundwater funnel areas are distributed mainly in the southwest of Shunyi District, the northeast of Chaoyang District and the northwest of Tongzhou District, with an average decline rate of groundwa- ter level of 2.66 rn/yr and a maximum of 3.82 m/yr in the center of the funnels. Seasonal and interannual differences exist in the response model of land subsidence to groundwater funnels with uneven spatial and temporal distribution, where the maximum land subsidence rate was about --41.08 mm/yr and the area with a subsidence rate greater than 30 mm/yr was about 1637.29 km2. Although a consistency was revealed to exist between a groundwater funnel and the spatial distribution characteristics of the corresponding land subsidence funnel, this consistency was not perfect. The results showed that the response model of land subsidence to the dynamic variation of groundwater was more revealing when combining conventional technologies with InSAR, GIS, GPS, providing a new strategy for environmental and hydrogeological research and a scientific basis for regional land subsidence control. 展开更多
关键词 land subsidence groundwater funnel over-exploitation of groundwater INSAR deformation response
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清代各地“仓斗”形成的机制考释 被引量:7
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作者 胡铁球 《清华大学学报(哲学社会科学版)》 CSSCI 北大核心 2021年第2期27-51,207-208,共27页
清政府除了制定部颁标准仓斛外,还制定了"京仓洪斛""通仓洪斛"("洪斛"又称"红斛")等数种官方量器。部颁标准仓斛的容重,籼糙米1石=120斤,粳糙米1石=130斤,白粮1石=138.25斤,小麦1石=125斤,粟米... 清政府除了制定部颁标准仓斛外,还制定了"京仓洪斛""通仓洪斛"("洪斛"又称"红斛")等数种官方量器。部颁标准仓斛的容重,籼糙米1石=120斤,粳糙米1石=130斤,白粮1石=138.25斤,小麦1石=125斤,粟米1石=137.2斤,黑豆1石=123.2斤,因斛量方法和新陈粮质不同,每石上下浮动2斤至3斤为正常。与部颁标准量器的容重对比,便会发现各地的仓斗大小相差悬殊,其形成机制主要有四,其一是沿明代旧例用"通用市斗"来收发税粮,使得"仓斗"与"通用市斗"概念相同,这主要分布在西北等地;其二是沿着中央洪斛制造的原理,将标准量器扩容到可容纳其法定加耗数目,如某地每石加耗1.5斗,则该地"仓斗"将在标准仓斗基础上每石扩容1.5斗;其三是用当地"标准市斗"作"仓斗",由于各地"标准市斗"大小不一,致使各地仓斗大小不一;其四是用本地"通用市斗"代替"仓斗"征粮。 展开更多
关键词 京斗 仓斗 市斗 容重 机制
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