風化層表土 的英文怎麼說

中文拼音 [fēnghuàcéngbiǎotǔ]
風化層表土 英文
regolith
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  • 表 : Ⅰ名詞1 （外面;外表） outside; surface; external 2 （中表親戚） the relationship between the child...
  • 風化 : 1 （風俗教化） morals and manners; decency 2 [化學]（化合物失去結晶水） efflorescence3 [地] （地...
  1. The earth surface of the region across it is mostly thicker humus soil or leaf falling covering layer, and has good heat reserving property, it is mostly weathering shingle, soil - aggregate mixture, and clay - gravel 0. 5m - 4. 0m under it, and weathering rock

    所經地區的地表多為較厚的腐殖土或落葉覆蓋層，其保溫性良好，下層0 . 5 ? 4 . 0米多為風化沙礫、碎石土和礫石土， ， 4 . 0米以下為風化巖石。
  2. The surface soil and the unconsolidated mantle rock beneath it form only a thin venner.

    地表土壤和它下面的未固結的風化層只是形成一個很薄的蓋層。
  3. 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壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；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冰期。
  4. 3 analyzing particle size of the wind - blown sediment and surface soil indicate that the former in 0. 02mm - 0. 2mm occupy about 40 % and 55 % of sloping field and shoaly land of bashang, which shows that bashang is the erosion and desertification region or the latency. 4 the search of decreasing effect of wood strap indicates that in lower wind speed the effect is distinct

    3風蝕物及表層土壤顆粒粒徑分析表明，地表200cm高度內風蝕物粒徑在0 . 02mm 0 . 2mm之間；壩上地區坡梁地與灘地該粒徑范圍顆粒分別佔40和55左右，說明壩上地區是風蝕沙化或潛在風蝕沙化地區。
  5. Contrasting stone coal to the soil developed from it and water to water leached from stone coal shows that slight fluorine pollution of surface water and plant resulted from weathering of stone coal and leaching

    摘要通過對比典型剖面上的石煤及其風化發育的土壤的氟含量、流經石煤層的水與不經過石煤層的水的氟含量，研究石煤風化、淋溶時氟對土壤、地表水和農作物的影響。
  6. ( 4 ) we defined ssee factor ( surficial soil element enrichment factor ) and wpem factor ( weathering profile element mobility factor ), and applied them to evaluate the degree of effects of black shales weathering on soil, water bodies and their sediments composition

    （ 4 ）提出了表土層元素富集因子和風化剖面元素遷出因子，用於估算巖石風化對水體及其沉積物、土壤的化學組成影響的程度。
  7. After the study and research on the village housing conditions in jiangsu and western zhejiang province, this article analyses and discusses on what the villages has gained in this kind of change and what has been lost, and believes due to the influence of the negative metropolis elements, the village is sacrificing the nature, the ecology, the local construction, and the traditional folk culture, which are the main sources of sustainable development of the chinese villages

    認為鄉村受負都市元素的影響正在失去包括自然、生態、鄉土建築、傳統風俗文化在內的中國鄉村可持續發展的資源，論述了鄉村現代化過程中的避免都市化的重要性，緊迫性。透過鄉村居住狀態都市化傾向的表象，去挖掘其背後的深層原因，從社會、經濟、文化、建築等角度分析現代鄉村居住狀態都市化的起因和後果。
  8. From the aspects of planning the green land space, protecting ancient banyans, strengthening view forest land vegetation tending, expanding the vegetable species application, building the compounded layers of plant community, building the different type of garden view, considering the folk - custom culture plant development, paying attention to the surface soil protection and application of controlling the damage plants, it discussed the greening countermeasures of building fuzhou urban plant diversity, so as to provide the references for the further compilation of protecting and rebuilding urban biodiversity

    摘要從規劃綠地空間、保護古榕樹、加強風景林地植被撫育、擴大植物種群應用、構建復層植物群落、營造多樣的園林景觀、考慮民俗文化植物開發、重視表層土保護和控制危害性植物應用等方面，探討了構建福州城市植物多樣性綠化對策，從而為進一步實施保護和重建城市生物多樣性提供參考。
  9. The geologic condition of side slope is complex. it is composed of soil and intense weathering rock on the surface and slightly weathering rock under the surface. further more, it has many faults, fissuring and weak intercalations

    其水電站尾水渠高邊坡所處區域地質條件復雜，邊坡表面由幾米至十幾米厚的坡積土和強風化破碎巖石組成，下部是弱風化和微風化巖石組成，且斷層、節理和軟弱夾層分佈廣泛。
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