海岸線要素 的英文怎麼說

中文拼音 [hǎiànxiànyāo]
海岸線要素 英文
coastline features
  • : Ⅰ名詞(水邊的陸地) bank; shore; coast Ⅱ形容詞[書面語] (態度嚴峻或高傲) lofty
  • : 名詞1 (用絲、棉、金屬等製成的細長的東西) thread; string; wire 2 [數學] (一個點任意移動所構成的...
  • : 要動詞1. (求) demand; ask2. (強迫; 威脅) force; coerceⅡ名詞(姓氏) a surname
  • : Ⅰ形容詞1 (本色; 白色) white 2 (顏色單純) plain; simple; quiet 3 (本來的; 原有的) native Ⅱ名...
  • 海岸線 : beachline; sea line; shoreline; strandline; coastline海岸線測量 coastlining; 海岸線效應 coast-line effect
  • 海岸 : seaboard; seabeach; seashore; seacoast; coast; shore
  • 要素 : essential factor; key element; part; element; factor
  1. 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 )黃河河口口門逕流潮汐區域並非持續保持淤積狀態,在特定的來水來沙、邊界條件和洋動力條件下,該區域可以處于沖刷狀態; ( 2 )從河口泥沙沉積分配的過程來看:三角洲與濱區泥沙的沉積變化趨勢是基本一致的,各部位的泥沙沉積比例變化基本呈波動狀態,且三角洲與濱區泥沙的沉積比例與來沙量密切相關,基本成正比關系; ( 3 )在口門處,影響泥沙沉淤的因集中在潮汐頂托、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積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流路泥沙沉積分配的回歸計算式,據此可以預估計算河口不同區域泥沙的沉淤量; 、 5 )本項研究首次論證了河口三角洲動態平衡的概念,並建立了黃河河口來沙量與造陸面積的相關關系,得出了當河口多年平均來沙量維持在3 . 45億t時其河口三角洲則可能處于動態平衡狀態的重結論; 『 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。
  2. In this section the evolution process of the coastline in the bayou area and diaokou bayou area was analysed through overlay analysis of gis. furthermore, the evolution rules and the enfluence factors were also analysed briefly

    在比較兩種基於遙感數據的提取方法可行性的基礎上,運用一般高潮法提取,通過gis疊加分析深入剖析了黃河口地區、釣口河口地區的演變過程,並簡分析了的演變規律及其影響因
  3. It may be useful to deepen the related study. in this thesis, some contents are studied as follows : ( 1 ) fractal characters of china coastline, mountain ridges, faults are studies roundly, including the fractal demarcating of the length of continental coastline of china, the spatial change of fractal dimensions of coastline from north to south of china, spatial relations of fractal dimensions of china coastline, mountain ridges, faults, etc. ( 2 ) fractal characters of china earthquakes, landslides and mud flow are studies roundly too, including the spatial relations of fractal dimensions of them, etc. ( 3 ) the fractal mechanism of china coastlines are discussed in different scales, including the pattern of the controlling effect of faults, crannies, etc. in a word, fractal characters of china main geomorphologic phenomena and geological disasters are studied in this paper, it is useful to deepen the related studies, and explore possible ways of geographical innovation of china

    概而言之,本項研究對可以稱得上是一個典型研究區域的中國主地貌與主地質災害中可能存在的分形現象進行了系統探討,並以分維為中介參數對中國主地貌與主地質災害以及二者之間的空間關系進行了探討,從而在廣度上在一定程度上豐富了中國地學分形研究的基本材,在一定程度上也填補了對中國中觀地學現象分形研究的空白;同時,本項研究還選擇了分形研究領域里最傳統、博士學位論文摘最具代表性的為突破口和創新點,探討了中國分形性質的存在機制問題,研究了不同尺度下構造與物質組成對中國分形性質的影響,從而在深度上在一定程度上深化了傳統的分形研究,在實現地學分形研究從現象揭示到機制探討的轉變方面進行了率先的探索。
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