含粘土的砂 的英文怎麼說

中文拼音 [hánniándeshā]
含粘土的砂 英文
argillaceous sand
  • : 動詞1 (東西放在嘴裏 不咽下也不吐出) keep in the mouth 2 (藏在裏面; 包含) contain 3 (帶有某種...
  • : 粘動詞(粘附) glue; stick; paste; adhere to; bond
  • : 4次方是 The fourth power of 2 is direction
  • : 名詞(沙子) sand; grit
  1. The results indicate that : 1. the main physical and chemical characteristics vary regularly : with rising of the altitude, there is a transition from silt > sand > clay to sand > silt > clay in the mechanical composition ; the argic horizon emerges below the altitude of 1600 meters ; the content of organic matter is enrichment, the content of organic carbon of epipedon is higher than 20 g / kg, while the content of organic carbon increases with increasing of altitude, and in the altitude of 3500 - 3700meters, the soils under the meadow have the maximum content organic carbon ; the soils appear acid - slightly acid reaction, the ph decreases appreciably and acid strengthen with increasing of altitude ; the soils higher than the altitude of 2500 meters are base unsaturated, indicating the soil leaching is strong, the ph and bs are distinct plus correlated ; the contents of sio2, al2o3, and fe2o3 of the soil body and clay are all relatively stabilization ; in the soil body, the content of sio2 is much high and cao is very little, the total contents of sio2, a12o3 and fe2o3 occupy 92 % of the mineral parts, the sequence of mineral elements is : sio2 > al2o3 > fe2o3 > k2o > mgo > cao > tio2 > mno

    研究結果表明: 1太白山南坡主要理化性質隨海拔高度上升呈有規律變化:隨海拔高度上升,機械組成由粉粒粒逐漸過渡到粒粉粒粒,海拔1600m以下出現化層;壤有機質豐富,表層有機碳量一般在20g kg以上,有機碳量隨海拔高度升高而相應增加,海拔3500 3700m灌叢草甸植被下有機碳量最高;壤呈酸性或微酸性,並隨海拔上升, ph值略微降低,酸性增強,海拔2700m以上壤多呈鹽基不飽和狀態,表明壤淋溶作用較強, ph值和鹽基飽和度呈極顯著正相關;體與粒中sio _ 2 、 al _ 2o _ 3 、 fe _ 2o _ 3量相對比較穩定,體中sio _ 2量較高, cao量較少, sio _ 2 、 al _ 2o _ 3和fe _ 2o _ 3量之和約占壤礦質部分92 ,礦質元素順序依次為: sio _ 2 al _ 2o _ 3 fe _ 2o _ 3 k _ 2o mgo cao tio _ 2 mno 。
  2. The time corresponding to the four parts along the section are as follows : the top lake - swamp sediments : holocene ; the uppart fine sand : later late pleistocene ; the middlepart sandy clay : middle - early late pleistocene ; the lowpart clayer silt : later - middle - pleistocene. the fossils and stone artifacts found in salawusu site should be formed during the last but one glacier, its age range is about 0. 13 - 0. 19 ma, and belongs to later middle - pleistocene

    分析q曲線與氧同位素曲線一致性以及以上研究結果,包薩拉烏蘇地層這套沉積物沉積時代為:頂部湖沼相沉積物:全新世;上部具交錯層理:晚更新世晚期;中部粉:晚更新世中期至早期;下部質粉:中更新世晚期。
  3. Testing on logs in laminated shaly sands it demonstrates that the model can be applied in laminated shaly sands. testing on effects of rdc. and vdc representing clay resistivity and fraction or dry clay resistivity and fraction on water saturation calculated by the model it proves that it is very reasonable for rdc to be clay resistivity and vdc to be dry clay fraction, so the mode l derived from the paper can be used to evaluate shaly sands

    通過一組層狀泥質巖測井資料解釋,表明該模型適用於層狀泥質巖地層解釋;通過考察rdc 、 vdc代表或干電阻率及量對該模型計算水飽和度影響,說明rdc代表電阻率,而vdc代表干量是合適,因此,使用文中給出電阻率模型能更好地解決泥質巖問題。
  4. The organic matter, total n, hydrolytic n were increased, then reduced with the increase of abandoned time. the loss of organic c got up to 59. 4 % in abandoned land. in 0 - 20cm, the sand content of 0. 25 - 0. 05mm was increased gradually, the average content of sand in the abandoned land was up to 76. 84 %, the sand contents of silt and sand was gradually reduced, the soil mechanic compose became coarse

    隨撂荒年限增加,壤有機質、全氮、堿解氮等主要養分均表現出先降低后增加趨勢;撂荒地有機碳損失平均達到59 . 4 ;在撂荒地表面0 - 20cm范圍內, 0 . 25 - 0 . 05mm粒徑量逐漸增加,各撂荒地粒平均量達76 . 84 ,粉粒和量逐漸降低,壤機械組成出現粗化現象。
  5. With increase of artificial forest age, the content of soil organic matter decreased sharply. and soil physical, chemical and biological properties of forest became worsen. from soil physical properties analysis, soil silt, clay, physical clay, aggregate degree and structure coefficient in topsoil increased with increase of artificial forest age and soil sand deceased

    壤物理性質方面,隨著人工雲杉林齡增加,壤表層粉粒、粒、物理性粒、團聚度和結構系數降低,量增高,壤飽和持水量、毛管持水量及總孔隙和毛管孔隙在人工雲杉演替過程中表現出「 u 」型變化。
  6. In order to direct the water to the forebav of the pump station from the original canal, a channel long 135 m is designed. it crosses through the terrain top with a depth of more than 50 m. soil of the channel slopes is a strongly - weathered silty and sandy mudstone with many well - developed reticular cracks and takes the structural surfaces almost same as the channel slopes

    東深供水工程金湖泵站位於塘廈鎮東面,屬低山、殘丘地貌,地面高程22 60m ;泵站前池進水渠橫切山脊,連接原東深供水河,設計開挖1條長135m進水渠,坡高50多米,邊坡質為強風化質泥巖,網狀裂隙發育,結構面基本與坡面重合;坡體質中有較多礦物,具有遇水軟化特性。
  7. Abstract : the cause of underwater concrete reinforcing cage up - floating accident is improper operation, such as loose - placement of reinforcing cage, fast - drawing of conduct pipe, improper embedded depth of conduct pipe ; and the poor quality of concrete, for example, the slump, sand percentage, adhesiveness and initial setting time don " t meet requirement

    文摘:水下混凝澆注鋼筋籠上浮事故原因是操作不當,如鋼筋籠固定不牢、提升導管過猛、導管埋深不當等,以及混凝品質差,如坍落度、率、聚性、初凝時間等不合要求。
  8. An important issue is that the dry bulk and shear modulus of sandstone are tightly correlated in a simple relationship with distribution of porosity, mineral composition, clay content, cementation, and differential pressure

    乾燥體變模量和剪切模量與孔隙度分佈、礦物成分、量、膠結度和差壓關系是嚴格相關,這一點非常重要。
  9. Grain - size accumulation percentage of the aeolian sands in the past 150 ka in milanggouwan section is mainly characterized by the aeolian palaeo - mobile dune sands, which are composed of majority fine sands and minority very fine sands. there is n ' t almost any silt and clay. those of the fluvial facies, especially the lacustrine facies and palaeosols, are mainly composed of very fine sands and also contain some quantities of silt and clay

    米浪溝灣剖面150kabp以來風成粒度累積百分量以古流動物質為主,其中以細量最高,極細為次,幾乎不;河流相、特別是湖沼相與古壤以極細量占優勢,且具一定
  10. The cause of underwater concrete reinforcing cage up - floating accident is improper operation, such as loose - placement of reinforcing cage, fast - drawing of conduct pipe, improper embedded depth of conduct pipe ; and the poor quality of concrete, for example, the slump, sand percentage, adhesiveness and initial setting time don " t meet requirement

    水下混凝澆注鋼筋籠上浮事故原因是操作不當,如鋼筋籠固定不牢、提升導管過猛、導管埋深不當等,以及混凝品質差,如坍落度、率、聚性、初凝時間等不合要求。
  11. ( 2 ) in the thesis, some other important factors on the stability of subway foundation during earthquake are studied, for example, the intension of earthquake, the unit weight of the subway tunnel, the depth of the subway tunnel, the content of clay in sandy soil, and inputing different earthquake waves

    ( 2 )研究了對地鐵隧道地基抗震穩定性有著重要影響一些其它因素,例如,地震動強度、地鐵隧道平均容重、地鐵隧道埋深、量以及不同實測地震波等。
  12. Because these factors make change more often, soil time space variability is more bigger. the relationship of single factor between soil water infiltration capacities and certain influencing factor could be established quantitatively by means of soil water infiltration tests in indoor, there is negative correlation relation between soil water infiltration capacities and soil structure. there is negative correlation relation in high grit content and low physical clay content soil, and second - degree polynomial relation in high physical clay content junk structural soil between soil water infiltration capacities and soil moisture

    由於這些因素在時刻發生變化,使得時空變異性較大,只能用室內壤水分入滲試驗來定量確定壤水分入滲能力與某些影響因素之間單因子相關關系,壤水分入滲能力與壤結構之間呈負相關關系,壤水分入滲能力與水量之間在量高,物理性量低無結構壤中呈負相關關系,在物理性量高團粒結構壤中呈二次多項式關系。
  13. So far as the mixing material for building the earth - rock fill dam with clay core for shiquanhe hydropower station is concerned, the effect from the variation of the sand content for the filter material on the maximum dry density and the relevant parameters are to be determined within the variation area of the mixing mass ratio of ( 46 ~ 54 ) : ( 54 ~ 46 ) through this experiment, due to the max, dry density is largely influenced by the mixing ratio of both the lifter material and the clay and the sand content of the filter material, so as to determine the actual filling compactness of the mixing material of the core

    摘要由於獅泉河水電站心墻石壩摻合料最大幹密度受反濾料與摻合比例、反濾料影響較大,因此擬通過本試驗確定摻合質量比在( 46 ~ 54 ) : ( 54 ~ 46 )范圍變化時,反濾料量變化對最大幹密度影響程度及相關參數,從而確定心墻摻合料填築實際壓實度。
  14. By analyzing parameters of the model, we find out that shale distribution largely affects water saturation calculated by the model, the less the resistivities of sand grains or clay grains, the more largely the resistivities of grains affect the relation between ct and swt, the effect of m on the relation between ct and swt is increased with swt

    通過對該模型影響因素分析,發現泥質分佈形式對模型計算水飽和度有很大影響;巖顆粒或顆粒電阻率越小,顆粒電阻率對c _ t與sw關系影響越大; m ( m = n )對c _ t與s _ ( wt )關系曲線影響隨s _ ( wt )增大而增大。
  15. It was shown that salt expansion value of low liquid - limit clay was accumulated before the sixth freezing and thawing cycles, but the increment of salt expansion was reduced gradually with increasing cycles ; the salt expansion accumulation of low liquid - limit clay could be separated into three phases ; the deformation of clayey sand was mostly frost heave and subsidence under cycles, and collapsibility value of clayey sand was accumulated with increasing cycles ; the variation of salt expansion ratio and collapsibility ratio was a parabolic function of freezing and thawing cycles

    試驗結果表明:低液限前五次凍融循環過程中鹽脹具有較好累加性,隨著凍融循環次數增加,鹽脹量增長速度逐漸降低;低液限鹽脹過程可以被分為三個階段;在凍融循環過程中變形主要為凍脹和沉降變形,具有較好溶陷累加性;低液限低液限鹽脹率和溶陷率與凍融周期之間關系符合二次拋物線變化規律。
  16. Liquefaction of saturated sands is a greatly complicated phenomenon. its generation, development and dissipation are restricted by physical property, stresscondition and boundary condition of soils. in addition, there are a lot of influencing factors such as density, structure property , clay content, degree of saturation, gradation, hydraulic conductivity, initial stress condition and dynamic load character and so on

    液化是一種相當復雜現象,它產生、發展和消散主要由物理性質、受力狀態和邊界條件所制約,存在許多影響因素,例如密度、結構性、量、飽和度、級配、透水性能以及初始應力狀態和動荷載特徵等。
  17. Vegetation restoration also resulted in the changes of soil physical and chemical properties, i. e., the contents of organic matter, alkali - hydro nitrogen, rapidly - available potassium and the contents of fine sand, very fine sand and clay were increased significantly, while ph and the content of rapidly - available phosphorus were decreased

    植被恢復使壤理化性質發生了變化,與恢復前相比壤中有機質、堿解氮、速效鉀以及細、極細、粉量顯著增加, ph值和速效磷量降低。
  18. The sand in taklamakan bo has fine grains with similar diameters, and its strength characteristics are not fully are to ordinary sand as well as silty. but its strength shows some features similar to clay when with some water content

    塔克拉瑪干沙漠顆粒極細,粒徑均勻,其強度特徵既不完全等同於普通,又不同於粉,在水狀態下則又表現出與相類似特點。
  19. As we know, when meeting these soils, many breakdown and danger will occur, such as the blockings, which has attracted attention of many construction personal on site. however, at present, there exist many unknown fields in blocking. firstly, the definition of blocking is not interpretative

    但是,如果地層是量較少卵石層、地層、風化巖地層,進入壓力艙體就很難形成這種「塑性流動狀態」 ,從而嚴重阻礙施工進程甚至造成施工事故,閉塞就是常見一種施工障礙,已經引相關方面重視。
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