mu us 中文意思是什麼

mu us 解釋
毛烏素沙漠
  • mu : n. 希臘語的第十二字母〈M, μ〉; 百萬分之一；千分之一毫米。
  • us : pron 1 〈we 的賓格〉我們。2 〈詩、古〉朕 （＝ourselves）。3 〈口語〉〈用作表語〉我們 （＝ we）。4...
  1. Study on sprouting of adventitious roots of sabina vulgaris in mu us sandy land

    毛烏素沙地臭柏不定根發生特性的研究
  2. Sample ' s analyses and tests in laboratory, this thesis makes a detailed research on holocene deposits characteristics of mu us desert, especially on characteristics of grain size composition, which break through previous description of determining the nature and gain a series of number indexes. at the same time, this thesis has also researched arenaceous source on every part of mu us. firstly mu us desert ' s forming process is deeply influenced by the east asian monsoon, the grain size gradually becomes smaller, while the magnetic susceptibility becomes larger from northwest to southeast this phenomenon not only appears on the surface of mu us, but also obviously reflects on the same layer of different places

    根據大量野外詳細考察和室內樣品分析與測試，本文對毛烏素沙地全新世地層沉積特徵做了細致的探討，尤其對區域地層的粒度組成特徵做了進一步的研究，突破了以往的定性描述，得出了一系列量化指標；結合野外的考察工作，對其不同地區的沙質來源做了詳細分析，主要得出以下結論： 1 、毛烏素沙地形成過程深受東亞季風影響，粒度自西北向東南逐漸變細、磁化率值逐漸變大。
  3. Therdly because of the influence of terrain and geological structure, arenaceous resources of different regions are different in mu us. sands are mainly from riverway in northwest ; from efflorescent cretaceous sandstone on account of higher topography in the middle part of mu us ; and sands resources are intricated in southeast, mainly including riverway sands, sands blown by the wind and embedded sands under so

    3 、毛烏素沙地因受地形和地質構造影響，不同區域的砂質來源情況不盡相同，西北部地區主要為河道沙；中部地區地勢較高，為白堊系基巖裸露而風化成沙；東南部地區沙質來源情況復雜，主要有：現代河道砂、風積沙、也有埋藏在現代壤土之下的出露古沙。
  4. Dynamics of the aboveground biomass yield of the caragana stenophylla - stipa spp. community on desert grassland in mu us sandland

    小針茅群落地上生物量對氣候因子的動態響應
  5. This paper, based on the grain - size analysis and the comparative result of the mz - o scatter gram of ancient aeolian sands in milanggouwan section with the modern dunes in mu us desert, holds that fossil eolian dunes are a proxy of the dune activation, and be regarded as " desert process ", while the overlying fluvio - lacustrine and palaeosols on the dunes are regarded as inter - desert process

    文中根據粒度分析及古今砂丘的mz ?散點圖比較結果，認為古代風成砂丘特別是古流動砂丘是砂丘活化的體現，視為「沙漠期」 ，而砂丘上覆的河湖相沉積與古土壤發育則可視為「間沙漠期」 。
  6. Genet characters of hedysarum laeve and the characters of its ramet population in different habitats in mu us sandland

    毛烏素沙地根莖灌木羊柴的基株特徵和不同生境中的分株種群特徵
  7. Situated at the southeast of the mu us desert, ordos plateau, the milanggouwan stratigraphical section in the salawusu river valley keeps a record of 38 sedimentary cycles of alternate evolution of the aeolian dune layers with the fluvio - lacustrine facies and palaeosols since 150 ka bp

    位於鄂爾多斯高原毛烏素沙漠東南邊緣的薩拉烏蘇河流域的米浪溝灣剖面，記錄了150kabp以來的38個風成的砂丘砂與河湖相和古土壤交替演化的沉積旋迴。
  8. These are the material bases for the desertization expanding that the earth ' s surface vegetation is sparsed, made - ups material is loosed, and sand source is abundant in mu us region

    毛烏素地區地表植被稀疏、組成物質鬆散、沙源豐富，為沙漠化擴展提供了物質基礎；而乾旱多風的氣候是沙漠化發展的重要因素之一。
  9. Distributing pattern of soil properties, including soil moisture and nutrients beneath the natural shrubs of sabina vulgaris and its ecological adaptability of clonal traits to sandy habitats in mu us sandland were studied using field experiments

    應用野外實驗生態學方法研究了毛烏素沙地天然臭柏灌叢地土壤資源的分佈格局及天然臭柏克隆特性對沙地環境的生態適應性。
  10. The edge dispersal clone population regulation of hippophae rhamnoides subsp. sinensis in the mu us sandland

    毛烏素沙地中國沙棘無性系種群林緣擴散規律
  11. Accordingly, the dune deposits of the section since 150 ka bp can be divided into 38 alternate evolvement processes of desert and inter - desert periods, which accord with the sedimentary cycles of the section. it is further suggested from now climate in the area that the 38 inter - succession processes of dune deposits and fluvio - lacustrine or palaeosols in past 150 ka actually result from the alternate evolvement of the ancient east asia winter and summer monsoons in the mu us desert during the long geologic times

    從這一認識出發，將米浪溝灣剖面150ka以來的砂丘堆積劃分為38個旋迴的沙漠期與間沙漠期交替演化過程，並認為，該剖面自那時以來發生的38個砂丘沉積與河湖相或古土壤的演替過程，實際上是這一長期地質時代毛烏素沙漠受東亞冬夏古代季風影響交替演化所致。
  12. Spatial heterogeneity of top soil moisture in different stand age of salix psammophila in mu us sandy land

    耕作方式及茬口對小麥播前土壤貯水量的影響
  13. And the precipitation decrease progressively and evaporation capacity greater and greater in mu us region. and the results indicate that it is more outstanding of the relationship between the moisture deficit and the current desertization situation and degree of aggravating of the main counties in this area

    研究表明，本地區主要旗縣水分虧損量與區域的沙漠化現狀及加重程度的關系密切，水分虧損量大的地區，不僅沙漠化程度重，而且加重趨勢明顯。
  14. Study on some characteristics of evaporation of sand dune and evapotranspiration of grassland in mu us desert

    毛烏素沙地水分蒸發和草地蒸散特徵的比較研究
  15. Responese of sabina vulgaris to nutrient resources in the contrasting habitats in the mu us sandland

    沙地柏對毛烏素沙地3種生境中養分資源的反應
  16. Pollination characteristics of natural population of sabina vulgaris in mu us sandland

    毛烏素沙地天然臭柏種群風媒傳粉的特徵
  17. Clonal plasticity, resources sharing and clonal labor division were adaptive strategies of s. vulgaris to sandy habitats in mu us sandland

    臭柏的克隆可塑性、資源共享和克隆分工行為是其適應毛烏素沙地環境的重要生態對策。
  18. Regulation of clonal growth of hippophae rhamnoides l. subsp sinensis population in mu us sandland

    毛烏素沙地中國沙棘無性系生長調節
  19. And mu us region, which located on the northwestern part of the loess plateau, is far from the sea and has a relatively dry climate, is one of the regions with serious desertization as well as ecological fragility. so, this study has not only important theory meaning but also obvious realistic meaning and high practical value

    毛烏素地區位於黃土高原西北邊緣，深居內陸，氣候乾旱多風，是我國沙漠化最為嚴重的地區之一，因此，對該地區沙漠化驅動機制進行研究，不僅具有重要的理論意義，而且具有明顯的現實意義和較高的實踐價值。
  20. The rise and fall of tongwan city with the environmental change of mu us sandy land

    統萬城的興廢與毛烏素沙地之變遷
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