流域面積比 的英文怎麼說

中文拼音 [liúmiàn]
流域面積比 英文
basinarea ratio
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • : 名詞(在一定疆界內的地方; 疆域) land within certain boundaries; territory; region
  • : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : Ⅰ動詞1 (比較; 較量高下、 長短、距離、好壞等) compare; compete; contrast; match; emulate 2 (比...
  • 流域 : [水文] watershed; basin; drainage area; catchpit; catchment area; drainage basin; feeding ground;...
  • 面積 : [數學] area
  1. The area of sienna in 1997 decreased 103271. 9 hectares than that in 1987, decreased 82. 15 % than before

    變化最小的類型為河,變化最大的為黃土區, 1997年的黃土區1987年減少103271 . 9公頃,原來減少82 . 15 。
  2. Study achievement appears as following aspects : ( 1 ) yellow river estuary gate river flow and tide flow mixed area is not keep standing deposition status, on special income water and sediment conditions, boundary conditions and oceanic power conditions, this area may on the scour status ; ( 2 ) observed from estuary sediment deposition distributing process : delta and sea offing area sediment deposition vary trend is similar, each part sediment deposition scale varies as wave shape ; ( 3 ) on estuary gate, affect the sediment deposition factors, primary factors are tide prop, the gate widens gradually, estuary gate have branches, brine induced flocculation. this paper study the estuary gate widen, estuary gate have branches to affect the river channel deposition in quantity ; ( 4 ) based on field measured data, for the first time, deduce the estuary sediment deposition and distributing regress formula which can estimate estuary different areas sediment deposition volume ; ( 5 ) this subject demonstrate the estuary delta coastline dynamic balance conception, build the relationship between the estuary income sediment with deposition land area, draw the following important conclusion : when estuary years - averaged income sediment keeps at 345 million tons, the delta coastline may on the dynamic balance status. ( 6 ) this subject firstly brings up estuary sediment optimized control conception, and has the primary study on the macroscopically optimized control conception method

    研究認為: ( 1 )黃河河口口門逕潮汐區並非持續保持淤狀態,在特定的來水來沙、邊界條件和海洋動力條件下,該區可以處于沖刷狀態; ( 2 )從河口泥沙沉分配的過程來看:三角洲與濱海區泥沙的沉變化趨勢是基本一致的,各部位的泥沙沉例變化基本呈波動狀態,且三角洲與濱海區泥沙的沉例與來沙量密切相關,基本成正關系; ( 3 )在口門處,影響泥沙沉淤的因素主要集中在潮汐頂托、口門逐漸加寬、河口門分汊、鹽水造成絮凝等,本報告主要對口門加寬,口門西妥理工大學工程碩士專業學位論文分漢對河道淤的影響進行了定量分析: (一扣根據實測資料首次建立了河贖路泥沙沉分配的回歸計算式,據此可以預估計算河口不同區泥沙的沉淤量; 、 5 )本項研究首次論證了河口三角洲岸線動態平衡的概念,並建立了黃河河口來沙量與造陸的相關關系,得出了當河口多年平均來沙量維持在3 . 45億t時其河口三角洲岸線則可能處于動態平衡狀態的重要結論; 『 6 )本項研究首次提出了河口泥沙優化調控的概念,並對其宏觀優化調控模式進行了初步探討。
  3. The proportion that the sediment yield of the main gully accounts for the total sediment yield of the experimental watershed model is from48. 7 % to 66. 6 %, and the proportion that deposition sediment yield of main gully accounts for the total deposition sediment yield of the experimental watershed model is from64. 9 % to 99. 4 %. the developing process of topographic feature of the experimental watershed model. expanding the gully width and cutting down the gully bottom are the two chief forms of the topographic feature development

    模型地貌形態發育過程溝谷擴展和下切是模型地貌形態發育的主要形式,溝谷擴展發育主要發生在發育活躍時段,主溝所佔溝谷總例在模型溝谷擴展發育過程中保持在60以上:主支溝下切發育在發育初期和發育活躍時段前期表現最為劇烈,其橫剖為v字形,在發育初期和穩定時期時段呈現淺u字形和底部較為平坦的梯形,主溝的橫剖發育明顯優先於各支溝。
  4. The factors include antecedent precipitation of low flow period and status of karst basins ( such as lithology, landform, drainage area, drainage density, length and ratio of demotion of main river and so on. ). based on the former studies, integrated the conventional statistic methods, the technique of anns is applied in this paper for researching the law of the low flow of karst basins in guizhou altiplano

    影響喀斯特枯水徑的因素異常復雜,其影響因素主要有枯季前期降水量和巖性、地貌、、河網密度、主河道長度及其降等下墊狀況。本文在前人研究的基礎上,採用人工神經網路技術,結合傳統的統計方法,研究貴州高原上喀斯特的枯水徑規律。
  5. A 2 - d hydrodynamic - numerical model was applied to typical rocky rapids called jiyutan by comparing different computational models. based on the comparison of different schemes, the change of the discharge and the flow current in a branch were analyzed, and the relationship between the flow condition and excavation area, scope as well as mode was discussed, the conclusions show : ( 1 ) in a branching rocky rapids, the velocity may be reduced and flow condition can be improved by excavating one channel partly

    本文在對各種數學模型較的基礎上,應用二維水動力數學模型研究典型石質汊灘? ?廣西潯江鯽魚灘航道整治工程方案,通過各方案計算結果較,分析了不同汊道的開挖及汊道內不同開挖、開挖范圍以及開挖方式所引起的分及工程區航道水力條件的變化規律,研究結果表明: ( 1 )對于石質汊灘來說,在某一汊道通過局部開挖河槽,擴大過水斷,可以達到降低工程段速、改善局部水條件的目的。
  6. The nature reserves cover 5. 74 % of the total area in the yangtze basin, which is 1. 9 % lower than the overall mean rate in china

    長江的自然保護區佔全的5 . 74 ,我國自然保護區占國土例低1 . 9個百分點。
  7. The statistics show that the correlation of antecedent precipitation, lithology, landform, drainage density, drainage area, length and ratio of demotion of main river and four characteristics of low flow is very complex

    統計結果表明:的枯季前期降水、巖性、地貌、、河網密度、主河道長度及其降等因子與喀斯特的枯水四特徵的相關關系異常復雜。
  8. The paper shows the research for the division of regional land - use structure in the east of gansu loess plateau according to the dates from the square and ratio of second - class land types of the detailed land - use investigation, adopting the quantified structure analysis method of landscape ecology, taking the longdong region of the upper and mid jinghe river - sheds as an example, through quantitative research of the division of regional land - use structure

    摘要根據土地利用詳查變更資料中二級分類的用地例,採用景觀生態學結構定量分析方法,以涇河中上游的隴東地區為例,對土地利用結構的地分異進行了定量研究。
  9. As compared with the conventional straight well, the horizontal well can greatly increase the contact area between well and reservoir, change the filtrational mode in the vicinity of wellbore in the reservoir and reduce filtrational resistance, thus obtaining higher oil and gas production by a relatively low producing pressure difference

    摘要同常規的垂直井相對,採用水平井開采能夠大幅度增加油氣井與油氣藏的接觸,改變油氣藏中井筒附近區的滲方式,降低滲阻力,進而可以利用較低的生產壓差來實現更高的油氣產量。
  10. The parameter in the xin ' anjiang model, imp, was extracted directly from above land use / cover data. another parameter, sm, in each subcachment and in each raster grid was obtained from the relation between sm and the ratio of forest land area to subcatchment area. thus, a semi - distributed hydrological model and a distributed hydrological model were established to analyze the effect of some parameters in xin ' anjiang on runoff process according to the spatial variability of land surface characteristics

    將遙感技術獲取的土地利用和地表覆蓋一公里柵格信息與數字高程模型數據進行空間配準,然後通過構建林地與新安江模型參數sm的關系間接確定各子及各柵格單元的的sm值,新安江模型參數imp由配準好的土地利用和地表覆蓋信息直接提取,由此建立方案與方案,來分析受下墊覆蓋的空間不均勻性影響的模型部分參數是如何對模擬水文過程產生影響的。
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