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黄土高原水土保持专业数据库No description found
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黄土高原水土保持专业数据库 | loess.csdb.cn Reviews
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黄土高原生态环境数据库
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电子邮件 loess@ms.iswc.ac.cn.
黄土高原水土保持专业数据库
http://www.loess.csdb.cn/pdmp/foreground/viewMetadata.action?id=233
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黄土高原水土保持专业数据库
http://www.loess.csdb.cn/pdmp/foreground/viewMetadata.action?id=232
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黄土高原水土保持专业数据库
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关键字 黄土高原,土壤,地球化学. 摘要 本数据集是根据中国科学院水利部水土保持研究所田均良、彭祥林等所著的 黄土高原土壤地球化学 一书 科学出版社,1994年 整编而成的。 本数据集主要包括 黄土高原土壤的类型和基本形状、黄土中元素 如造岩元素、铁族元素、亲铜元素、稀土元素等 的地球化学特征,黄土高原土壤元素的含量、剖面分布、地域分异,天然放射性元素的土壤地球化学,此外还有土壤地球化学与人类健康、土壤微量养分与微肥使用等方面的数据。 关键字 黄土高原,水文站,泥沙. 数据的时间范围为50年代初-80年代末 数据的空间范围覆盖黄河流域的主要水文观测站 数据项目包括 逐日流量 133个站的资料 、逐日泥沙含量 128个站的资料 、逐日降雨量 177个站的资料 、逐日蒸发量 70个站的资料 、逐月河流悬移质颗粒级配 70个站的资料。 摘要 黄土高原地区西起日月山,东至太行山,南靠秦岭,北抵阴山,涉及青海、甘肃、宁夏、内蒙古、陕西、山西、河南七省 区 50个地 盟、州、市 ,317个县 旗、市、区 ,全区总面积64万km2,其中多沙粗沙区面积7.86万km2。
黄土高原水土保持专业数据库
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Loes Ruland and Erik de Lange. Dorpsstraat 14 Mheer, 043-4574517. Loes Ruland en Erik de Lange. Site ontwikkeld door: Spider productions.
LOESS LEXICON.net - Dedicated to the study and research into loess
Dedicated to the study and research into loess. This website is still under construction, please visit us later! Loess particle size distributions. This website is devoted to the worldwide Study of Loess. Loess tends to develop into highly rich soils. Therefore under appropriate climatic conditions these areas are among the most agriculturally productive in the world. Loess grains are angular, with little polishing or rounding, composed of crystals of quartz, feldspar, mica and other minerals. Becaus...
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LÖSS der Heurige von Leithner, Öhlzelt und Schwillinsky in Langenlois
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loess.com - This website is for sale! - passport,travel Resources and Information.
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黄土高原水土保持专业数据库
loess (Will) - DeviantArt
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:: LOESS :: Vinos Ribera del Duero y Rueda
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loess in a sentence | simple examples
In A Sentence .org. The best little site that helps you understand word usage with examples. Loess in a sentence. A certain deposit called loess or hwang-tu (yellow earth) covers a great part of. Together with previously reported U-series dating of speleothem calcite and palaeomagnetic stratigraphy, as well as sedimentological considerations, these layers may be further correlated to S6-S7 in Chinese loess stratigraphy or marine isotope stages (MIS) 17-19, in the range of 0.68 to 0.78. Together with prev...