溪水侵蝕 的英文怎麼說

中文拼音 [shuǐqīnshí]
溪水侵蝕 英文
brook erosion
  • : 名詞(小河溝) small stream; brook; rivulet; streamlet
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : Ⅰ動詞(侵入) invade; intrude into; infringe upon Ⅱ形容詞(接近) approaching Ⅲ名詞(姓氏) a surname
  • : Ⅰ動詞1. (損失; 虧耗) lose 2. (腐蝕) erode; corrode Ⅱ名詞(天體現象) eclipse
  • 溪水 : stream; brook; lymph
  1. The research results mainly show : ( 1 ) the ecological degradation characteristics of wuxi county include : some soil is thin and barren and its water and fertility conservation abilities are poor, gradual degradation of soil results in decrease of vegetation diversity and the vegetation community structure gradually inclines tc simplicity from complexity. the types of soil and water loss in wuxi county mainly involve surface erosion and gully erosion. according to investigation, surface erosion area occupies 80 % or so or erosion area, in which the slope farmlands surface erosion area accounts for about 70 % of farmland erosion area

    研究結果主要包括: ( 1 )巫縣生態退化特徵表現:作為生物生長基質的部分土壤薄而貧瘠,保保肥能力差,部分地區基巖裸露,土壤的不斷退化導致植物種多樣性減少,植物種群結構逐步由復雜趨向簡單化;縣內土流失的類型主要包括面和溝兩大類,據調查,面面積占總面積的80左右,其中坡耕地面佔耕地面積的70左右。
  2. ( 5 ) by analyzing the terrace in the lacustrine sediment of the ancient barrier lake, diexi, minjiang river, forming of the terrace is not only because of the intermittent arising of the tectonic movement, but also because of descend of the eroding normal covering resulting from destroying of the barrier lake

    ( 5 )通過對岷江疊古堰塞湖湖相沉積中的河流階地分析可知,階地的形成不僅僅是由於新構造運動的間歇性抬升作用,由於堰塞湖的潰決引起洪下泄,導致河流基準面的下降也可以形成階地。
  3. Soil erosion and nutrient losses in jiangjiatang watershed in lanxi city in zhejiang province during exploitation was studied from 1993 - 2000 using adoptive research methods such as runoff plot, catchment area, and rare earth element tracer ( eu ), and the soil fertility index appraisal. the major conclusions are as follow : 1. the principle of water and soil losses together with nutrients and the forms in which they were lost were studied under different fanning systems in runoff plot

    本研究選擇浙江省中部金衢盆地邊緣蘭土保持監督站蔣家塘小流域為研究試驗點,以協作單位蘭土保持監督站小流域開發試驗區為基礎,採用坡面徑流小區法、單源匯試驗區出口實測法、穩定性核素- eu土芯示蹤法研究了2000年坡耕地不同農作措施土流失規律及養分流失規律和小流域綜合開發過程中土流失規律及養分流失規律,並對小流域土壤的肥力現狀進行評價。
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