高原土 的英文怎麼說
中文拼音 [gāoyuántǔ]
高原土
英文
upland soil-
In loess plateau, flat shovels were popular, and my shovel liked a flat pan, the paste of barnyard grass flour laid open around the shovel, at the edge the paste was emitting flashy air bladder, not for one minute, a battercake was finished
黃土高原用的是平板鐵鍬，宛如一隻平底鍋，稗子麵糊均勻地向四周攤開，邊緣冒著一瞬即逝的氣泡，不到一分鐘就煎成了一張煎餅。It was on this very soil that the greco - bactrian civilization had its best flowering and left the indelible marks of finest greek art in the potwar plateau around
是在這土壤， greco - bactrian文明有它最佳開花和左最美好的希臘藝術不可磨滅的標記在potwar高原在拉瓦爾品第和克什米爾附近。She also wanted to cross china from east to west, to start from beijing, through hua bei campagna, to get loess plateau, and though silk road to arrive at pamirs plateau
她還想自東向西橫穿中國，從北京出發，走華北平原，到黃土高原，走絲綢古道，最終到達帕米爾高原。The people is living in a cave digged out from the hill slope and this is the famous cave dwelling village for shaanxi and shanxi - a special kind of housing specially at the loess plateau
?洞是中國山西及陜西一帶居民因應黃土高原的自然環境而發展出來的居住設施-挖洞而居。This article aimed to study how to improve the utilization of the water resources by applying the technology of filtration irrigation to the plowland croppers in the hills area of loess tableland
本題目研究的目的是在黃土高原丘陵區研究大田農作物應用節水滲灌技術來提高其對水資源的利用效率。Dust aerosols in qingdao come from three area : the desert in west of inner mongolia and the dene in east of inner mongolia together with loess altiplano
沙塵粒子的來源主要有三個地方：一是內蒙西部沙漠地區；二是內蒙東部沙地；三是黃土高原。Soil caco3 eluviation and deposition process is the most important development and evolution process of soil, from parent material to mature soil in the loess plateau, arid and semiarid area
土壤碳酸鈣（ caco _ 3 ）的淋溶淀積過程是黃土高原以及乾旱和半乾旱地區土壤形成發育的主要過程之一，也是地球化學過程的主要內容。At the same time, the quality of different - state water was studied. the results show : the soil bulk density of the fir wildwood heightens with the increase of soil depth, specifically 0. 74 > 0. 94 andl. 34g / cm3, the saturated, canaliculus and field moisture contents decrease gradually in layer a, b and c, accordingly the soil total foveola decreases gradually, and the moisture - hold capacity of the soil lessens gradually with the increase of the soil depth ; there is small difference of the soil bulk density between layer a and b in the outer space, which are respectively 0. 92 and 0. 99g / cm3, and the other laws are the same as the in ner in the main ; reverse success often occurs in the low position of the thoroughly - fell trace and plateau marsh is formed
結果表明：冷杉原始森林土壤容重隨土層深度的增加而增大，分別為0 . 74 、 0 . 94 、 1 . 34g cm ~ 3 ，飽和持水量、毛管持水量、田間持水量a層、 b層、 c層逐漸減小，十壤總孔隙度也逐漸減小，土壤的持水能力隨深度的增加逐漸減弱；林外空地a層、 b層十壤容重相差不人，分別為0 . 92和0 . 99g cm ~ 3 ，其它規律與林內人體相同：皆伐跡地的低洼地段容易發生逆行演替，形成高原沼澤地。Study on the synthesis of corundum - mullite - gahnite multiphase materials by two - step sintering process using kaolinite as raw material showed that impurities introduced by kaolinite mainly increased the liquid amount at high temperature, which can assist sintering of specimen. the experiment results indicated that the samples with lower gahnite content had better sinterability than others. however, if the gahnite content was relative high, the promoting effect on sinterability caused by kaolinite was not significant
採用天然原料高嶺土二步煅燒合成剛玉?莫來石?鋅鋁尖晶石復相材料研究發現：天然原料中帶入的雜質主要是增加液相量，促進高溫下試樣的燒結；當尖晶石含量較低時，試樣在1300保溫2h時，在1600燒后試樣燒結性能相比之下較好；而當鋅鋁尖晶石含量較高時，天然料對試樣的促燒作用不是非常明顯。Caco3 not only affects soil physical and chemical characteristics but also causes co2 change in the air, because caco3 is main components among the total pool of inorganic carbon of soil. this paper systematically summarized and analyzed general development characteristics of soil profile caco3 in loess hill gully area including source, content, forming - condition, distribution and illuviation - depth of caco3, which will have the most important significance for the further studies on global soil and climate change
碳酸鈣在土壤剖面中淀積的深度和類型是黃土高原土壤發育的重要標志，鈣積層是黃土高原土壤發育環境的歷史信息庫，同時土壤碳酸鈣作為土壤無機碳庫重要組成，它通過溶蝕后再結晶與大氣co _ 2之間進行物質交流來影響全球氣候變化。Landscape pattern analysis for loess plateau
黃土高原土壤中微量元素的中子活化分析Meanwhile, most aspects about this perspective are concerned, which include quantification of the soil water background of the plateau area, the regional spatial variation of soil water background and variation along the slope, mosaic structure and seasonal changes etc. the results show that : ( 1 ) for the fundamental circumstance for vegetation development is the original debilitated slope, so the perspective of soil water background specially for the loess plateau refers to the soil water conditions on the original slope. ( 2 ) the value of soil water background appears to be a descending trend from south to north based on the difference of vegetation zones. in the forest zone, soil moisture contents beneath 3m depth from the soil surface are more than 12 % usually ; in the forest - pasture zone, the values of soil moisture content beneath 4m depth underground are more than 6 % and stable, and tend to be ascending while the depth increases ; but the values in the dry pasture zone is lingering between 4 % to 6 % from the surface layer to sub - layers
發展了「土壤水分背景」的概念，並以之為基礎對其各個方面進行了研究，使之形成一個相對獨立和完整的體系，主要包括黃土高原土壤水分的背景值、土壤水分背景的區域分異、坡面分異、鑲嵌結構及其季節分異等： （ 1 ）由於植被生長發展、演替的基礎階段是天然草被群落，故認為黃土高原的土壤水分背景在概念上是特指該區天然草被群落下的土壤水分狀況； （ 2 ）黃土高原的土壤水分背景值，根據植被地帶的不同表現出自南向北逐漸降低的規律：森林地帶3米以下土層水分背景值普遍穩定地高於12 ，森林草原地帶4米以下土層水分背景值穩定大於6 ，且均隨土層的加深水分含量逐漸增加，而草原帶的土壤水分背景值自土表至底土層一直在4 6之間徘徊。Based on the serious shortage of soil moisture, soil aridity and vegetation recession in this region, the following issues are studied in this dissertation : ( 1 ) the meaning of soil water and its role in the water circulation ; ( 2 ) soil water deficit and its influence to vegetation growth ; ( 3 ) the definition of soil dried layer and the causes of its formation ; ( 4 ) soil dried layer distribution and characteristics in north of shaanxi loess plateau ; ( 5 ) the primary study of measurable index of soil dried layer
本論文主要針對黃土高原土壤水分嚴重虧缺現狀以及因之而形成的土壤干化和林草植被衰退現象，主要對以下幾方面的問題進行了研究： （ 1 ）土壤水分的意義及其在生態系統水分循環過程中的作用； （ 2 ）林草植被土壤水分虧缺狀況及其對植被生長的影響； （ 3 ）土壤干層的涵義及成因分析； （ 4 ）陜北黃土高原土壤干層的分佈及特徵； （ 5 ）土壤干層的量化指標初步研究。The loess plateau, a dense warren of eroding canyons where some villages are unreachable by roads, is separated from much of the change stirring up china
黃土高原，土質疏鬆、溝壑縱橫的人口稠密之地，這里的許多村莊都沒有通路，與世隔絕。Impact of climatice change on soil water content in loess plateau, gansu
氣候變化對甘肅黃土高原土壤貯水量的影響Evolution feature on the moisture of soil for loess highland in gansu
甘肅黃土高原土壤水分氣候特徵By precipitation data of 42 gansu stations of loess plateau in march to july from 1961 to 2000 year and the soil weight information of moisture content at 11 agricultural meteorology stations from build station to 2000 year in march to november
摘要利用甘肅黃土高原42個氣象站1961 - 2000年3 ~ 7月降水量和11個農業氣象觀測站逐年3 ~ 11月上旬的土壤重量含水率資料，分析了甘肅黃土高原土壤水分的地域和時間分佈特徵。Interaction of soil and water conservation measures with soil water in the loess plateau in china
黃土高原土壤水分與水土保持措施相互作用( 3 ) over the past 15 years, land, loess plateau of north of shanxi province, utilize degree rate of change r from one year < 0, prove that this district land is utilized and is in adjusting one or decline phase
（ 3 ）從1986 2001年15年來，陜北黃土高原土地利用程度變化率r 0 ，說明該區土地利用處于調整期或衰退期。土地利用程度變化處于發展期的只有榆陽區、神木縣和吳堡縣三個地區。Soil erosion and village svstainabilit in loess plateau region
黃土高原土壤侵蝕與聚落生存對策研究分享友人