壤中冰 的英文怎麼說

中文拼音 [rǎngzhōngbīng]
壤中冰 英文
soil ice
  • : 名詞1. (土壤) soil 2. (地) earth 3. (地區) area 4. (姓氏) a surname
  1. This work carries out a temporal - spatial analysis and comparison in facial pattern, grain - size, and susceptibility of the sediments of the hunshandake sandy land ( hsl ) on the basis of studies of more than fifty geological sections, a number of samples collected from surface sands as well as results derived from previous studies. the preliminary results of this work provide new environmental information of the working area, which makes it possible to have a brief discussion about the evolution of the hsl since the late glacial epoch. this work can be summarized as the followings

    期,渾善達克沙地全面擴張,達到了沙漠化最大規模,剖面的古風成砂是最直接的證據,此時氣候乾冷;全新世早期,渾善達克沙地成比較好,是一個大面積成期,相當于全新世適宜期,此時氣候暖濕;全新世晚期,渾善達克沙地沙漠化正過程加強,在沙地各剖面上普遍發育風沙沉積,氣溫較乾冷;目前:渾善達克沙地為另一成期,成作用相對于適宜期較差,氣候乾暖。
  2. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面分析來看,本區在全新世早期氣候回返,相對較寒冷乾燥,東亞冬季風影響較明顯,此時為沙層堆積向砂質土過渡,自北至南堆積的沙粒漸細;全新世期氣候溫暖濕潤,東亞夏季風影響顯著,此時為明顯的成期,表現在自北至南普遍可見發育較好的黑壚土層,且南部的成作用比北部好,土的厚度也要大;全新世晚期至今,氣候向乾冷方向轉化,但變化幅度遠小於末次期。
  3. Born all in the dark wormy earth, cold specks of fire, evil lights shining in the darkness

    這些統統產于黑暗而蠕動著蚯蚓的土。火焰的冷顆粒,不祥之物,在黑暗發光。
  4. We sampled the palaeosol or buried soil of this section formed during the middle stage of last glacial at the interval of 10cm and totally we got 40 samples for spore - pollen analysis. we adopted the analytic procedure that is developed by mingjian wei ( personal communication ) to treat the spore - pollen samples

    以10厘米為間距,在末次期發育的古土採集孢粉樣品40個,用魏明建等改進的孢粉分析方法進行樣品的實驗室分析,通過外加標志花粉的方法計算花粉濃度。
  5. The best we can say is that the hypothesis is consistent with several indirect pieces of evidence ? most notably, the low atmospheric co2 levels inferred from ancient soils and the timing of the first planet - encompassing ice age

    我們頂多能說這個假說是由若干殘缺的間接證據構築而成,其最值得注意的是從古代土成份推知大氣的低二氧化碳含量,以及第一次全球性期發生的時機。
  6. In the recent years numerous scientists have found that there appeared many abrupt climatic changes during the last glacial by studying the high - resolution achieves of environmental change such as polar ice - core, deep ocean sediment and loess - palaeosol sequence et al

    近十幾年來,隨著研究技術和方法手段的進步,許多科學家通過對極地芯、深海沉積物、黃土-古土等環境演化信息載體的研究,在末次發現了許多氣候突變事件。
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