自由水含量 的英文怎麼說

中文拼音 [yóushuǐhánliáng]
自由水含量 英文
free-water content
  • : Ⅰ代詞(自己) self; oneself; one s own Ⅱ副詞(自然;當然) certainly; of course; naturally; willin...
  • : causereason
  • : 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...
  • : 動詞1 (東西放在嘴裏 不咽下也不吐出) keep in the mouth 2 (藏在裏面; 包含) contain 3 (帶有某種...
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • 自由 : freedomliberty
  1. 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分的背景值、土壤分背景的區域分異、坡面分異、鑲嵌結構及其季節分異等: ( 1 )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分背景在概念上是特指該區天然草被群落下的土壤分狀況; ( 2 )黃土高原的土壤分背景值,根據植被地帶的不同表現出南向北逐漸降低的規律:森林地帶3米以下土層分背景值普遍穩定地高於12 ,森林草原地帶4米以下土層分背景值穩定大於6 ,且均隨土層的加深逐漸增加,而草原帶的土壤分背景值土表至底土層一直在4 6之間徘徊。
  2. Depending on how the ground surface is denuded, the feature of the current crustal stress field and rock stress environment can be calculated analyzing the result in this paper : by analyzing the recovering feature of the elastic deformation of the rockmass in unload - stage under various pressures, it has been found there is close relationship between the recovering degree of the elastic deformation of the rockmass and the unloading degree of the pressure the direction of the major principal stress in the crustal stress field is not consistent with the direction of the crushing stress regional tectonics borne during the last tectonic movement. the evolving degree of the regional geomorphology evidently affects the current crustal stress field, which changes from the self - weight stress field to the horizontal stress field, with the changing of the eroding degree of the regional geomorphology ranging from valley area to hilly country to flat country. in valley area, where there is two stress belts, the bankslope s tress belt and the self - weight stress belt within the mountain. the direction of the major principal stress is nearly parallel to the ground surface and inclines towards the valley in the bankslope stress belt. it is nearly vertical in the self - weight stress belt

    通過本文的研究成果,根據區域性地貌的演化特徵,我們可以大致地對現今地應力場進行判斷:在分級卸荷條件下,巖體中彈性變形的恢復具有明顯的規律性,這種規律對于研究地應力場的演變是有幫助的;地應力場中最大主應力方向與區域構造形跡在最近的構造運動中所受區域性擠壓應力的方向無明顯的對應性;區域性地貌形態的演化程度對現今地應力場的特徵具明顯的影響,隨著區域性地貌侵蝕程度峽谷區、丘陵區、平原區的變化,現今地應力場特徵重應力場、平應力場為主重應力場特徵向平應力場的規律變化;在峽谷區,山體中具有兩個應力帶:重應力帶和卸荷應力帶,最大主應力方向在卸荷應力帶中近平行於坡面並傾向于河谷、在重應力帶中近於直立;根據原始地面遭剝蝕的程度,可以大致地估算最大主應力和中間主應力的值和方向;在丘陵區和平原區,最大主應力的方向近於平,並與附近區域性侵蝕盆地和河流的展布方向基本平行,根據原始地面遭剝蝕的程度,可以大致估算其最大主應力的值;根據區域性地貌形態的特徵來分析工程區的現今地應力場特徵,並進而大致了解巖石的應力環境,這種分析方法得出的結論與許多實際的地應力測試成果基本一致,對于大型電工程地下廠房和壓力隧洞的設計是有所幫助的。
  3. In this paper, the so preparing self - compacting concrete with low and middle strength using super fine mountain sand artifical sand and phosphorus slag is studied systemically. through the study the influence of the shape, the proportion of the dust and the grade of sand to the workability and the mechanical property of self - compacting concrete, it is found that super fine mountain sand artifical sand are not suit to prepare low and middle strength self - compacting concrete, but when they are combined and the additive and assistant band material are used, c20 - c40 high performance self - compacting concrete is prepared ; the corresponding additive is developed to solve the delamination caused by the low proportion of banding material ; the evaluating system for the workability of low and middle strength self - compacting concrete is built ; the controlling method for production, construction and curing was set up. and the result of the research is applied into several projects

    通過分析特細山砂和機制砂的顆粒形態、粉末、顆粒級配等特性對密實混凝土的工作性能和力學性能的影響,發現特細山砂、機制砂不宜單獨用於配製中低強度等級密實混凝土,宜將特細山砂和機制砂進行合理復配,並選擇合適的外加劑和礦物摻合料,優化配合比設計,可生產c20 c40中低強度等級密實高性能混凝土;研製開發出了具有高效減、保塑、抗離析功能的外加劑,有效解決了中低強度等級密實混凝土於膠凝材料用少而出現的離析、泌問題;應用正交設計方法,對因素和平進行合理選擇,確定了生產中低等級密實混凝土的最優配合比;建立了中低強度等級密實混凝土的工作性評價體系;提出了生產、施工及養護的質控制技術方法。
  4. Add preservatives and deoxidants to the mixture solution, and go throuth the process of separating by sinking in the container ; owing to the density difference between oil and water, the mixture solution inside the conatainer will be separated of itself, and the result is that crude oil floats on the surface, while water sink to the bottom, but the separated crude oil still has water content which will be removed through electric dehydration

    「在混合液中加入防腐劑和脫氧劑,然後進入容器進行沉降分離,於油密度不一樣,混合液在容器中然地分離,原油浮在上面,沉在容器下面,分離后的原油仍有少,再進行電脫分離。 」
  5. We should put them in the cool and ventilate place to make them dry naturally because there is a lot of moisture in the first samples, and they are enough dry when the sediments can freeze together

    於初樣中還有大分,將初樣置於陰涼通風處讓其然乾燥,其最終乾燥程度為沉積物尚能固結在一起。
  6. The prediction model of silicon content in hot metal tapped from blast furnace based on self - organized experience evolution is composed of following components : feature extraction and vector quantification of temporal process data, memory, storage, accumulation and evolution of the prediction experience

    高爐鐵組織經驗進化預測系統主要動態數據特徵提取、動態模式組織分類化以及預測經驗的記憶、存儲、積累和進化三部分組成。
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