soils 中文意思是什麼

soils 解釋
土壤
  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太白山南坡土壤的主要理化性質隨海拔高度的上升呈有規律的變化:隨海拔高度上升,機械組成由粉粒砂粒粘粒逐漸過渡到砂粒粉粒粘粒,海拔1600m以下出現粘化層;土壤有機質豐富,表層有機碳含量一般在20g kg以上,有機碳含量隨海拔高度升高而相應增加,海拔3500 3700m的灌叢草甸植被下有機碳含量最高;土壤呈酸性或微酸性,並隨海拔上升, ph值略微降低,酸性增強,海拔2700m以上的土壤多呈鹽基不飽和狀態,表明土壤淋溶作用較強, ph值和鹽基飽和度呈極顯著正相關;土體與粘粒中的sio _ 2 、 al _ 2o _ 3 、 fe _ 2o _ 3含量相對比較穩定,土體中sio _ 2含量較高, cao含量較少, sio _ 2 、 al _ 2o _ 3和fe _ 2o _ 3含量之和約占土壤礦質部分的92 ,礦質元素含量的順序依次為: sio _ 2 al _ 2o _ 3 fe _ 2o _ 3 k _ 2o mgo cao tio _ 2 mno 。
  2. Soils that are acidified enhance the cadmium uptake by plants

    酸性的土地使植物更容易吸收土壤中的鎘。
  3. Effects of simulated acid rain on exchangeable cation transplant and acidifying potential in litchi orchard soils

    模擬酸雨對果園土壤交換性陽離子遷移及其對土壤酸化的影響
  4. Cadmium strongly adsorbs to organic matter in soils

    突然中的有機物非常容易吸收鎘。
  5. Organic acids are normal constituents of most agricultural soils.

    有機酸是大多數農業土壤中通常的組分。
  6. Such complexes might have affinity for detrimental inorganic oxyanions such as arsenate, a common toxic contaminant in soils. the purpose of this study is to investigate the influence of environmental conditions on the adsorption of arsenate on fe - oxyhydroxide - monlmorillonte complexes, which is significant to agrology, geochemistry and environmental science

    本研究即以南方的土壤環境條件為參考,模擬在ph = 5時的酸性氧化條件下,土壤中低聚合羥基鐵?蒙脫石復合體的形成、物化性特徵及其吸附砷酸根陰離子的行為。
  7. Alfalfa will fail to grow well on soils which lack sufficient amounts of available calcium.

    苜蓿在有效鈣含量不足的土壤上生長不良。
  8. So these karst series problems are lowness ability of making soils, distributing odds of surface water and groundwater, leakiness of fountain, alkalescence of circumstance, lowness of bio - diversity, rapidness converse succession of vegetation and fragility of soil character and entironment. and karst region produces many problems, e. g. rock desert, soil erosion and degeneration because of artificial influence and destruction

    巖溶空間介質具有地上地下雙層結構,可溶巖造壤能力低,巖溶水空間分佈不均、地表地下水關系密切、水源易漏失,偏堿性環境、生物資源集聚程度低,植被逆向演替快、順向演替難,巖溶地質與生態環境十分脆弱,受到人為因素的影響和破壞,極易產生石漠化、土壤侵蝕與退化等一系列問題。
  9. Effect of different applying methods on improving alkaline soils with gypsum

    石膏不同施用方法改良堿化土壤效果淺析
  10. Alluvial soil was found to be more likely to show a greater deficiency of magnesium than glacial till soils.

    沖積土比冰川土更容易呈現較嚴重的缺鎂。
  11. Particulate matter in soils and aquatic systems reacts with and influences the biological activity of pesticides.

    土壤和水系統中的顆粒物質都與農藥的生物活動起反應,並影響後者。
  12. Earthworm populations in arable soils in the united states may be destroyed by frost.

    在美國可耕地中蚯蚓的種群會被冰凍所毀壞。
  13. Many believe artificial soils do not simulate natural soils.

    許多人相信人造土並不像天然土。
  14. Seven plots selected from wanglang reserve were distributed in different types of forest and at different altitude, and different plot has different microclimate. soil property, microbial population, soil nutrient content of forest soil were determined in wanglang natural reserve, from may to october 2002 to july 2003, the ecological distribution of three main groups, bacteria, actinomycete and fungi were determined in the forest soils by the cell enumeration methods. six kinds of physiological groups, including ammoniation bacteria, nitrification bacteria, nitrosification bacteria, aerobic autogenesis azotobacter, aerobic cellulose - decomposing bacteria and anaerobic cellulose - decomposing bacteria were enumerated by the most - probable number ( mpn )

    2001年10月在王朗自然保護區內設立了3個定位研究樣地和4個臨時樣地,通過多次現場采樣與室內實驗分析,測定了白樺林、岷江冷杉林、紫果雲杉林、繡線菊-羊茅群落、羊茅群落及高山柳灌木叢等6種不同植物群落內土壤微生物三大類群數量、功能微生物數量、土壤養分,並在固定樣地內使用埋袋法進行了三個埋藏深度的凋落物分解袋試驗,初步研究了枝條、闊葉、針葉等凋落物組分在不同分解階段所含養分的動態變化。
  15. During the 1950s, 1960s, 1970s and up to the early 80s, the key planting objectives were to restore vegetation to the badlands and to cover the eroded scars with trees as soon as possible - to prevent further erosion and to assist in the development of better soils

    由1950年代至1980年代初,植林的重點目標是盡快使劣地重長植被,以樹木覆蓋侵蝕痕跡,從而防止水土繼續流失,幫助建立更佳的土壤。
  16. Influence on different overburden soils due to bedrock fracture

    地下斷裂對不同土質上覆土層的工程影響
  17. Adsorption of benzoic acid on loess soils affected by surfactant

    表面活性劑對黃土吸附苯甲酸的影響
  18. Bio - remediation techniques of crude oil contaminated soils

    生物修復石油污染土壤
  19. Gley soils are typical of tundra, meadows, and boggy areas

    該種土壤是苔原、草地以及沼地所特有的。
  20. Field soils often have bulk densities ranging from 1. 0 to 1. 4gcc; with commensurate porosities and infiltration characteristics.

    田間土壤的容重常在1.0到1.4克立方厘米范圍內,且具有均勻的孔隙度和滲透性。
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