黃土性土 的英文怎麼說

中文拼音 [huángxìng]
黃土性土 英文
loessal soil
  • : Ⅰ形容詞(像絲瓜花或向日葵花的顏色) yellow Ⅱ名詞1 (指黃河)short for the huanghe river:黃泛區the...
  • : Ⅰ名詞1 (性格) nature; character; disposition 2 (性能; 性質) property; quality 3 (性別) sex ...
  • 黃土 : [地質學] loess黃土保持 loess conservation; 黃土地 loessland; 黃土地基 loess foundation; 黃土地貌 ...
  1. In order to elaborate the app licability of osl to loess, especially single aliquot regenerative protocol ( sar ), involving stimulation of the same disc with an infra - red laser diode followed by blue leds to polymineralic fine - grains of loess, such explanations as light bleaching, preheat, anomalous fading, prior - ir exposure were investigated in this paper. for drawing adequate coarse grains from loess, quartz and feldspars, as well as loess, were etched by hydrofluoric acid and fluorosilicic acid. the sequence of ages of holocene loess in weihe rivier basin has been established by single - aliquot ( sar ) and multiple - aliquot using fine - grains and sar using coarse - grains

    本文通過渭河流域全新世的光曬退實驗,地表樣品的d _ e值測定,細顆粒單片的預熱、反常衰退、紅外暴露實驗,說明釋光測年在全新世中應用的可行及單片再生劑量法( sar )在細顆粒中的適用;為了從中分離出足夠的粗顆粒,進行了純石英和長石的氫氟酸( hf )和氟硅酸( h _ 2sif _ 6 )溶蝕實驗,粗顆粒石英溶蝕分離實驗;通過細顆粒單片、多片的blsl 、 irsl和post - irosl ,熱釋光,及粗顆粒石英的blsl的年代測定,選擇適于全新世的釋光測年方法,並建立了渭河流域全新世的年代序列。
  2. We have not some certain appropriable method to solve this problem. more less job has been done on the loess nonlinear model

    本論文用正演和優化相結合的方式對的非線本構模型中的參數進行反演。
  3. Adsorption of benzoic acid on loess soils affected by surfactant

    表面活劑對吸附苯甲酸的影響
  4. Younger leaves faded green and lusterless ; older leaves marginal scorch, interveinal blotchy chlorosis, necrotic patches bleaching and withering ; characteristic of some soil acidity conditions

    甜菜錳和鋁合併中毒:幼葉褪綠失去光澤,老葉邊緣枯,脈間有壞死褐色斑點,接著白化,枯萎。這是酸壤特有的。
  5. Furtherly, according to their state in suffering force and their modes of initial motion, the casualty loess landfalls on the house side - slope are classified into two types of tension - sliding loess landfall and collapsed earth cave dwelling

    根據體受力狀態和起始運動方式,將宅基邊坡傷亡崩塌劃分為張裂?滑移式崩塌和坍窯兩種類型,總結了其前兆、時空分佈特徵,著重分析了其形成原因。
  6. Code for building construction in collapsible loess zone

    濕陷地區建築規范
  7. Code for building construction in collapsible loess regions

    濕陷地區建築規范
  8. Empirical formula of reinforcement depth of dynamic consolidation in collapsible loess foundation treatment

    強夯法處理濕陷地基加固深度公式探討
  9. 4. the prevention - cure measure for the landfall is put forward

    4 .提出了陜北宅基邊坡傷亡崩塌的防治措施。
  10. The study of rammer method in treating slumping loessal loam

    強夯法在處理濕陷中的研究
  11. Collapsibility of loess and its discrimination criteria

    的濕陷及其評價準則
  12. Malan loess was a special water sensitive geological deposit, whose physical, mechanical and hydraulic properties changed obviously under the softening action of water

    摘要馬蘭在水軟化作用下,體的物理、力學與水理質呈現出明顯的規律,屬典型的水敏感地質體。
  13. Experiment results show : ? he theory and method of information content could play an important role in the case study on the accuracy and application of dem. ( 2 ) in the loess plateau area, there are much difference between 5m resolution dems of 1 : 10000 map scale and 25m resolution dems of 1 : 50000 map scale while gathering terrain characteristic information, and yet the spatial structure of dem error have discipline and measurability on statistics. ( ? the results could offer fundamentals and methods to people on their work to research the terrain information content of dems with different scale level

    研究結果顯示: 1 、地形信息容量的理論與方法對于dem精度與應用適宜的研究具有重要的作用; 2 、在丘陵溝壑區,同1 : 1萬比例尺5米解析度的dem相比, 1 : 5萬比例尺25米解析度dem在提取地形特徵方面具有較大的差異,但誤差的量值與空間分佈具有統計上的規律與可估算; 3 、以上研究結果可望為其它各級比例尺dem地形信息容量的研究提供新的理論基礎與技術方法,也可為有關規范、標準的制定提供依據。
  14. Multinomial factors should be considered in the stability analysis and hazard prediction of seismic loess slopes

    在地震斜坡穩定分析和災害預測中,必須考慮多項影響因子。
  15. In this paper, research is emphasized on the situation of slope protection in shaanxi areas, analyses the engineering and economic effect of all kinds of slope protection, compare the traditional protection with the new, puts forward the protection principle that should be followed in shaanxi areas, study the destruction mechanism and stability analysis of high slope in ocher area, and puts forward effected and economic new protection methods

    本文對陜西地區的邊坡防護狀況進行了研究,分析各種防護型式的防護效果及其經濟效益,並結合國內外的防護新技術,對傳統防護型式和新型防護型式進行了對比分析,提出陜西地區在以後的防護工程中應該遵循的原則,並研究了高邊坡的破壞機理和穩定判斷的方法,提出巖邊坡有效、經濟的新型防護措施及其施工工藝。
  16. The collapsibility on intact and reshaped loess

    原狀和重塑的濕陷
  17. It was shown that the physical property, electric resistivily and microstructure of soil in the slide area were different from those in the slope, and could be used to determine the slip zone, while the mineral ingredient and chemical composition could not be used generally to identify the slip zone

    研究結果顯示:滑坡滑帶的主要物理質指標、電阻率特、細觀結構特徵、微觀結構特徵與滑坡體及滑床有顯著差異,在實踐中可作為鑒別滑動面的標志;而滑帶的礦物、化學成分沒有明顯的差異變化。
  18. Power tamp method treatment of wet and sunk loess foundation

    濕陷地基的強夯法處理
  19. Under applying k 200mg / kg, k fixation capacity of four soils strengthened with drying and wetting cycle and temperature increasing, so, the availability weakened. in general, capacities of fixing potassium of soils in turns were : heir lu soil > lou soil > loessial soil > aeolian sandy soil

    在施鉀量為200mg kg的情況下,干濕交替對四種壤鉀的有效影響程度由大到小依次為:、黑壚綿、風沙
  20. 2. according to the weighted average, soil co2 concentration is 0. 58 - 13. 29 times of that in atmosphere and is relatively lower than similar research, meanwhile, soil co2 concentration in profile varied irregularly, which possibly is due to the chemical and physical characteristic of loess soils, season change and arid climate etc. the variation of soil co2 concentration in profile is mainly controlled by soil temperature and soil moisture, in contrast with soil temperature, the control role of soil moisture is minor. in conclusion, in order to have a good command of the distribution and change rule of soil profile co2 concentration as well as its effect factors, multi - point and successive location experiment should be made, meanwhile establish indoor soil - pillar monitoring experiment

    壤co _ 2的濃度約為大氣co _ 2濃度的0 . 58 ? 13 . 29倍與同類研究相比要低,這是與質特,觀測期又逢特別乾旱年制約了壤微生物的活動,再加上壤中有機質虧損,養分不足造成的;壤co _ 2含量的變化是隨溫度的升高而升高,在夏季達最高值,冬季最低;在壤co _ 2濃度變化的影響因子溫度和水分中,溫度的影響作用高於水分;壤剖面co _ 2濃度隨著深度增加,總的變化趨勢是遞增的,但也有反復,甚至有的順剖面而下幾乎保持一恆值,這與季節變化和自身結構的通透以及在觀測期內的乾旱氣候等條件有關。
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