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151.
1 Introduction Land degradation is a major threat to environmental and agricultural quality of land[1] and is directly related to food security issues. An instrument for decision-makers to plan or stimulate allocation of land to users that can be sustained and are economically viable and socially acceptable. Different kinds of land are unequally suited to various uses. Land evaluation is the assessment of the suitability of a tract of land for a specified kind of use and it provides objective…  相似文献   
152.
We have found some mistakes in the article by Jianwei Song et al. (2007). The revisions arc given below: 1. "NEHRP 2003" in Figs.8 and 9 should be changed to "BSSC 2003". 2. "Tsopelas" or "Tsopelas method"  相似文献   
153.
First Occurrence of M andarinoite in China   总被引:6,自引:0,他引:6  
This report describes the first occurrence of the rare mineral mandarinoite (Fe3+2 Se3Og · 6H2O) in China. It occurs in the Lower Permian Maokou Formation carbonaceous shale in Yutangba Village east of Enshi City in southwestern Hubei Province. The shale is selenium-rich and contains native selenium, V-Mo-Cr-bearing iron oxide, clay and quartz. Weathering of the selenium in the bedrock under moderate to high redox conditions in the presence of ferric iron has formed mandarinoite.  相似文献   
154.
1IntroductionClimatic warming, flood hazards and their impacts on human society receive increasing attention from governments and public (IPCC, 2001). During recent years, agriculture, industry and even the development of the whole national economy suffered tremendous loss resulted from flood and waterlogging hazards.The Yangtze Delta is densely populated and economically developed. Monsoonal climate, geomorphologic characteristics and human activities inflict floods and water-logging hazar…  相似文献   
155.
Zircon SHRIMP ages of the Aolaoshan granite on the south margin of the Qilian Mts. range from 445±15.3 to 496±7.6 Ma (averaging 473 Ma), belonging to the Early Ordovician. Geochemically, the granite is similar to I-type granite and, tectonically, was formed in an island-arc environment based on relevant diagrams for structural discriminations. Considering also the regional geology, the authors suggest that the granite is part of an ultrahigh-pressure belt on the south margin of the Qilian Mts. and that its formation bears a close relationship to this belt.  相似文献   
156.
1 .FeoreKToH“呵eeK“e oeojeHHoeT“6aeee汤Ha从a认及aMa Baeee益H以a兹仄aMo‘py、eH ropH以Mo xpe6TaMo KyoHb一。yHb,以H二,HoaH卜j乏。AP山HH仄aK.3TH eK几a及qaT以e roPH反e eHeToM曰o5Pa3o3a几Heb B no3八HeKa几e风oHeKoMH PaHeBaPH城HHCKoM瓜aH米eHH只x.CaM 6aeee益H nPe仄cTaa几只eT:eo6诚,MaeeHB e oeHoBaHHeM八oKeM6PH直qeeK“x MeTaMoP中HqeeKHx noPo八. OT及e几bH曰e qaeTH以a盆八aMeKoro MaeeHaa B eBo旧oqePe皿b,Pe3Ko oT几Hqa心Te只Me水及yCo6o盆no TeKToHHqeeKoMy xaPaKT…  相似文献   
157.
INTRODUCTIONThelargestlakeinMexicoandthirdlargestinLatinAmerica,ChapalaLake(approximately2 0°N) ,is 1 50 0mabovesealevel,measures 75× 2 5km ,hasaveragedepthof6m (maximumdepthcloseto 1 1m)andamountainchainalongitsnorthernandsouthernshores (Fig .1a) .TheLermaRiverflowsintoit;theSantiagoRiverflowsoutofit.Thebeautifullandscape,andwarmclimateconducivetobreezecirculationalongitsshore ;absenceofabrupttemperaturevariations,andthemoderateairhumidityat tractmanytouriststothelake .Manyretirees…  相似文献   
158.
Characteristics of shallow gas hydrate in Okhotsk Sea   总被引:1,自引:0,他引:1  
Multidisciplinary field investigations were carried out in Okhotsk Sea by R/V Akademik M.A. Lavrentyev (LV) of the Russian Academy of Sciences (RAS) in May 2006, supported by funding agencies from Ko- rea, Russia, Japan and China. Geophysical data including echo-sounder, bottom profile, side-scan- sonar, and gravity core sample were obtained aimed to understand the characteristics and formation mechanism of shallow gas hydrates. Based on the geophysical data, we found that the methane flare detected by echo-sounder was the evidence of free gas in the sediment, while the dome structure de- tected by side-scan sonar and bottom profile was the root of gas venting. Gas hydrate retrieved from core on top of the dome structure which was interbedded as thin lamination or lenses with thickness varying from a few millimeters to 3 cm. Gas hydrate content in hydrate-bearing intervals visually amounted to 5%―30% of the sediment volume. This paper argued that gases in the sediment core were not all from gas hydrate decomposition during the gravity core lifting process, free gases must existed in the gas hydrate stability zone, and tectonic structure like dome structure in this paper was free gas central, gas hydrate formed only when gases over-saturated in this gas central, away from these struc- tures, gas hydrate could not form due to low gas concentration.  相似文献   
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