水空間 的英文怎麼說
中文拼音 [shuǐkōngjiān]
水空間
英文
hydrospace-
So these karst series problems are lowness ability of making soils, distributing odds of surface water and groundwater, leakiness of fountain, alkalescence of circumstance, lowness of bio - diversity, rapidness converse succession of vegetation and fragility of soil character and entironment. and karst region produces many problems, e. g. rock desert, soil erosion and degeneration because of artificial influence and destruction
巖溶空間介質具有地上地下雙層結構，可溶巖造壤能力低，巖溶水空間分佈不均、地表地下水關系密切、水源易漏失，偏堿性環境、生物資源集聚程度低，植被逆向演替快、順向演替難，巖溶地質與生態環境十分脆弱，受到人為因素的影響和破壞，極易產生石漠化、土壤侵蝕與退化等一系列問題。Precipitation and height above sea level is good in spatial. the model reflect characteristic of the theory of mountanious climatology effectively
建立的降水空間分佈模型，可很好地反映山地氣候的特點。Proceeding with the analysis of water resource peculiarity of jilin province, the authors bring forward that effective gathering and using of rainwater can supplement the gross amount of rainwater in valley, probe into rainwater resources use in jilin province : first is to make rainwater resources use plan in valley program, secondly is to construct gully dam system according to water and soil conservation project, to strengthen sloping field collection rain ' s project and forest - grass construction, to increase storage space, thirdly is to fully utilize field project and water conservancy project to gather rain water, intercept rainfall on the spot so as to restore water environment
摘要從吉林省水資源特點分析入手，提出了雨水資源的有效集蓄利用是補充流域水資源總量不足的重要因素，探討了在吉林省雨水資源主要利用途徑是首先在小流域規劃中作好雨水資源利用規劃；其次是建設以水土保持治溝骨幹工程為主的溝道壩系，強化坡面集雨工程和林草植被建設，增大貯水空間；第三是充分利用田間工程和水利工程集雨蓄水，使降雨就地就近被攔蓄，最終使水環境得以修復。With the change of industry structure, the city is experienceing the process of deindustrialization. the docks which were necessary for the city are not important any more
曾經繁榮的運河港埠逐漸被廢棄，其所處的城市濱水空間也呈現一派衰敗景象，人們不願接近它。Research on user - behavior oriented urban design of water - front areas
以使用者行為為導向的濱水空間城市設計E. design principle and exploration of appropriate scenery modality at waterfront space in inland town in irrigated area of yellow river
黃灌區城鎮濱水空間景觀設計原則與適宜景觀形態探索B. space exploiture and ecological environment research of waterfront in towns at irrigated area of yellow river.
黃灌區城鎮濱水空間開發與生態環境保護研究c黃灌區城鎮濱水空間開發水景觀與水文化研究dThe paper mainly discussed five aspects as follows : a. the introduction of waterfront in inland town at irrigated area of yellow river
全文著中討論了以下五方面內容： a黃河流域內陸城鎮濱水空間環境概況介紹bThe success and the failure of city waterfront design affects not only cityscape but also the sustainable development of urban area
城市濱水空間設計的成敗，絕不僅僅只是影響到城市的面貌，而且還影響到城市區域的發展或整個城市的可持續發展。Human activities have destroyed a large number of wetlands, that made hydrological space effects of wetlands obviously drop and greatly weakened water regulating function of wetlands greatly
人類活動大量破壞濕地，使濕地水空間效應明顯下降，極大地削弱了濕地水調節功能。Analysing and elaborating the constitute of green area ecological space of waterfront in city from four aspects, i. e. natural space, hydrophilic space, traffic space and plot space
從自然空間、親水空間、交通空間、情節空間四個方面分析論述了城市濱水區綠地生態空間的構成。The thesis is included five parts. the first part deals with the meaning of the writing, and introduces the condition of the city waterfront design & development in the world
論文由五個部分組成：第一部分：首先簡介了世界城市濱水空間設計及開發的現狀，然後論述了論文寫作的意義及相關概念。The thesis tries to study the theory of city waterfront creation from the aspects of " general system theory " and " the relationship between the man and environment. my major research target is funanhe which lies in chengdu
本論文嘗試在「一般系統論」和「人與環境關系」的理論體系下，以成都府南河為主要研究對象，進行城市濱水空間創造的理論研討。Effect of spatial precipitation heterogeneity on runoff process
降水空間不均勻性對徑流過程模擬的影響The result shows that not only spatial precipitation heterogeneity and spatial land use / cover variability but also spatial soil evaporation heterogeneity influences flood simulation. as remarked above, spatial variability is very crucial to hydrological modeling
計算結果表明不僅降水空間分佈、模型參數對水文過程模擬的精度有很大的影響，而且土壤蒸發空間不均勻性對模擬洪水也有一定的影響。Most of the spatial patterns do n ' t exsit outstanding periods, specially the spatial pattern of year precipitation, the first six spatial patterns do n ' t exsit outstanding periods, if exsit, the periods are also relative short, the most master period is about 3 years, secondly about 5 years
大多惰況下各空間型不存在顯著的周期，特粥是年降水空間型，前六個空間型都不存在顯著周期，即使存在也是一些相對較短的周期，其中以準3年的周期為主，其次是5年左右的周期。Accordingly, four precipitation subdivisions are put forward : i ( south area including rizhao, linyi, zaozhuang and jining ), ii ( east area including yantai, weihai, qirgdao and the east of weifang ), iii ( north area including heze and liaocheng ) and iv ( north area including dezhou, binzhou, dongying, jinan, taian, laiwu, zibo and the west of weifang )
另外，山東春季降水空間分區可分為4個區：區（南部區） ，包括日照、臨沂、棗莊、濟寧；區（半島區） ，包括煙臺、威海、青島和濰坊東部；區（西部區） ，包括荷澤、聊城；區（北部區）包括德州、濱州、東營、濟南、泰安、萊蕪、淄博、濰坊西部。The distribution of lrgr summer mean rainfall was determined by the obstructing effect and two stronger ascending airflow that come from bengal bay and south sea and converge around corresponding windward slopes ; the general circulation distribution in meridional section is equal, which showed the passing - effect of lrgr
縱向嶺谷區多年平均夏季降水空間分佈主要由縱向嶺谷的「阻隔」效應，以及夏季從孟加拉灣來的氣流和從南海來的氣流在相應迎風坡面輻合，形成兩支較強的上升氣流所致；而縱向剖面大氣環流的變化則較為均勻，顯示了縱向嶺谷的「通道」效應。Based on the 34 stations monthly precipitation and 100m 100m dem of chongqing, the paper study spatial distribution of precipitation of chongqing based on gis. accounting to the theory of mountanious climatology, the paper analyse the factors affecting spatial distribution of precipitation, establish the model of spatial distribution of precipitation
本文用重慶地區34個氣象觀測站1971 - 2000年30年氣候整編資料的月平均降水總量資料，以及重慶地區100m 100mdem數據，對重慶地區降水空間分佈進行研究。根據山地氣候學原理，利用gis技術，分析降水空間分佈的影響因子，建立重慶地區月平均降水空間分佈模型，計算重慶地區月平均降水量的空間分佈。This paper deals with the water - bearing media and water - bearing quality of the rocks in the damsite, at first, then it concludes two water - bearing space structures, namely, t - shaped and y - shaped structures, after the classification of the different rocks ' water permeability. furthermore. on the basis of the dynamic state of the ground - water and the hydrogeological conditions of this area, the groun - water system of the area has been prelimilarily divided accordingly
本文首先研究了壩址區出露巖體的含水介質和含水性，並對巖體透水性進行了分類，總結出了兩種巖體的含水空間結構，即「 t 」字型與「 y 」字型結構。在此基礎上通過研究地下水的動態，以及水文地質條件對本區的地下水系初步進行了劃分。分享友人