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232.
Geochemical Information Indicating the Water Recharge to Lakes and Immovable Megadunes in the Badain Jaran Desert 总被引:1,自引:0,他引:1
CHEN Jiansheng ZHAO Xi SHENG Xuefeng Wang Jiyang GU Weizu and CHEN Liang State Key Laboratory of Hydrology-Water Resources Hydraulic Engineering Hohai University Nanjing Jiangsu E-mail: jschen@hhu.edu.cn Institute of Isotope Hydrology Research Hohai University Nanjing Jiangsu Institute of Geology Geophysics Chinese Academy of Sciences Beijing 《《地质学报》英文版》2005,79(4):540-546
1 Introduction The Badain Jaran Desert, located in western Inner Mongolia, China, has a unique landscape containing 144 lakes (72 of which are still watery) with a total water area of about 23 km2, and the world’s highest stationary sand dunes with a height between 200 m and 500 m. Much attention has been paid to the water recharge of the desert in the past decade. Investigations on the resources of water system there have been performed continuously since the early 1990s, which lead to th… 相似文献
233.
福州市土地利用景观格局分析 总被引:5,自引:0,他引:5
以福州市土地利用现状图为基本图件,在GIS支持下编制了福州市土地利用景现图,进而选取几种主要指数,通过Excel软件计算,定量分析了福州市土地利用的景观格局及破碎化特征。结果表明:林地为基质景观,优势度指数最高,分离度指数最低;耕地、园地、城镇村及工矿用地和水域的均匀度较高,多样性指数较大,但破碎化程度较深;未利用地破碎度最低。从总体上看,土地利用的景观比较单调、多样性指数较小、破碎化程度也较低,景观异质性不高。 相似文献
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广西南丹地区尾矿分布于大厂、车河、芒场等矿区。尾砂来自以锡石为主的多金属矿床,尾砂中除Sn,Pb,Zn,Ag,Sb的质量分数达到工业指标外,Au亦达到综合利用指标。通过试验证明,对尾矿中的细微粒锡石可采用风力分级选矿、磁选和化学选矿等方法回收;尾砂中的非金属资源可作为填充材料、水泥原料利用,使尾砂型人工矿床充分的资源化。 相似文献
236.
生态城市的内涵及建设策略 总被引:7,自引:4,他引:7
程伟 《云南地理环境研究》2005,17(4):43-45
生态城市是通过倡导生态理念,采用生态技术,建立生态化产业体系,从而达到社会、经济、环境的可持续发展,实现自然生态平衡、人文生态和谐的城乡统一体。从可持续发展的角度出发,利用生态学和社会学的观点,论述生态城市的内涵,提出科学的城市规划、合理的城市评价指标体系、完善的城市管理制度是实现生态城市的前提,强调只有自然生态、人文生态两手抓才能真正实现经济、社会、环境全面发展。 相似文献
237.
Development of a soil moisture‐based distributed hydrologic model for determining hydrologically based critical source areas
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A simple grid cell‐based distributed hydrologic model was developed to provide spatial information on hydrologic components for determining hydrologically based critical source areas. The model represents the critical process (soil moisture variation) to run‐off generation accounting for both local and global water balance. In this way, it simulates both infiltration excess run‐off and saturation excess run‐off. The model was tested by multisite and multivariable evaluation on the 50‐km2 Little River Experimental Watershed I in Georgia, U.S. and 2 smaller nested subwatersheds. Water balance, hydrograph, and soil moisture were simulated and compared to observed data. For streamflow calibration, the daily Nash‐Sutcliffe coefficient was 0.78 at the watershed outlet and 0.56 and 0.75 at the 2 nested subwatersheds. For the validation period, the Nash‐Sutcliffe coefficients were 0.79 at the watershed outlet and 0.85 and 0.83 at the 2 subwatersheds. The per cent bias was less than 15% for all sites. For soil moisture, the model also predicted the rising and declining trends at 4 of the 5 measurement sites. The spatial distribution of surface run‐off simulated by the model was mainly controlled by local characteristics (precipitation, soil properties, and land cover) on dry days and by global watershed characteristics (relative position within the watershed and hydrologic connectivity) on wet days when saturation excess run‐off was simulated. The spatial details of run‐off generation and travel time along flow paths provided by the model are helpful for watershed managers to further identify critical source areas of non‐point source pollution and develop best management practices. 相似文献
238.
GPS Solutions - The GPS satellite transmitter antenna phase center offsets (PCOs) can be estimated in a global adjustment by constraining the ground station coordinates to the current International... 相似文献
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240.
Hai‐Ping Hu Jin‐Liang Feng Feng Chen 《Boreas: An International Journal of Quaternary Research》2017,46(3):412-427
A series of confirmed and suspected dammed palaeo‐lake sedimentary successions is scattered within the middle Yarlung Tsangpo valley in Tibet. However, the chronology, the genesis of the dam and its location, the water level of the dammed lake, the process of dam failure and the spatiotemporal relationships between the sedimentary successions remain controversial. Here, we focus on one sedimentary succession of the suspected dammed palaeo‐lake at Xigazê. We measured the grain‐size distribution, magnetic susceptibility, organic and inorganic carbon content, and δ13Corg and δ15Ntotal ratios of the sediments. In addition, we measured the δ18Oshell and δ13Cshell values of modern and fossil Radix sp. shells, and the δ18Owater and δ13CDIC values of the ambient water with different hydrological regimes. The results indicate that the δ18Oshell values of modern Radix sp. and the δ18Owater of the ambient water body significantly depend on its hydrological status. In addition, a strong positive relationship was observed between δ18Oshell values of modern Radix sp. shells and the δ18Owater of the ambient water on the Tibetan Plateau. According to this correlation, the δ18Owater values of the palaeo‐water body are reconstructed using the δ18Oshell values of Radix sp. fossil shells in the Xigazê section. Further, based on the δ18Oshell values of fossil Radix sp., the reconstructed δ18Owater of the palaeo‐water body and the specific habitats of Radix sp., we infer that the sedimentary succession in the Xigazê broad valley was mainly formed within the backwater terminal zone of a dammed palaeo‐lake and that the elevation of the water level of the lake was approximately 3811 m a.s.l. AMS 14C dating indicates that the deposits of the dammed palaeo‐lake were formed at about 33–22 cal. ka BP. Finally, the presence of Radix sp. fossil shells within the Xigazê section suggests that Radix sp. survived the late Last Glacial Period on the Tibetan Plateau. 相似文献