整體逐漸穩定 的英文怎麼說
中文拼音 [zhěngtǐzhújiānwěndìng]
整體逐漸穩定
英文
global asymptotic stability- 整 : Ⅰ形容詞1 （全部在內; 完整） whole; all; complete 2 （整齊） neat; tidy; orderly Ⅱ動詞1 （整理; 整...
- 體 : 體構詞成分。
- 逐 : 動詞1. （追趕） pursue; chase; run after 2. （驅逐） drive out; expel; banish 3. （挨著次序） one by one
- 漸 : 漸副詞（逐步; 漸漸） gradually; by degrees
- 穩 : 形容詞1 （穩定; 穩當） steady; stable; firm 2 （穩重） steady; staid; sedate 3 （穩妥） sure; rel...
- 定 : Ⅰ形容詞1 （平靜; 穩定） calm; stable 2 （已經確定的; 不改變的） fixed; settled; established Ⅱ動詞...
- 整體 : ensemble; whole; entirety
- 逐漸 : gradually; by degrees; little by little
- 穩定 : 1 （使穩定） stabilize; steady 2 （穩固安定） stable; steady 3 （物質的性能不易改變的作用） stabi...
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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「土壤水分背景」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水分的背景值、土壤水分背景的區域分異、坡面分異、鑲嵌結構及其季節分異等： （ 1 ）由於植被生長發展、演替的基礎階段是天然草被群落，故認為黃土高原的土壤水分背景在概念上是特指該區天然草被群落下的土壤水分狀況； （ 2 ）黃土高原的土壤水分背景值，根據植被地帶的不同表現出自南向北逐漸降低的規律：森林地帶3米以下土層水分背景值普遍穩定地高於12 ，森林草原地帶4米以下土層水分背景值穩定大於6 ，且均隨土層的加深水分含量逐漸增加，而草原帶的土壤水分背景值自土表至底土層一直在4 6之間徘徊。Iii ) the result from simulating rainfall on watershed model indicats that changes of projective area, surface area and volume represented development of watershed physiognomy. volume of model body decreased and projective area and surface area increased with developing process of watershed model. when development of gully trending to stablization, projective area become stable and surface area changed fluctuantly
（ 3 ）流域模型的模擬降雨實驗觀測結果分析表明：流域模型地貌的發育演化主要體現在其投影面積、表面積和相對體積的變化上；流域模型投影面積和表面積在整個試驗過程中一致增大，當溝道發育逐漸趨于穩定時，投影面積變化也趨于穩定，表面積則呈現出波動性變化。Memories of the asian financial crisis in 1997 - 8 inevitably fade as the region in general continues to enjoy financial stability and economic growth
隨區內整體繼續保持金融穩定及錄得經濟增長， 1997至98年期間亞洲金融危機已逐漸被淡忘。After the cold war, the relationship among great powers enters a stage of in - depth adjustment. international forces have experienced the process of division and reorganization and the world pattern has undergone and will undergo profound changes
冷戰結束后，東北亞地區格局進抵深入調整時期，逐漸形成了以美、中、俄「大三角」為主體，內含中、俄、日、韓「小四邊」的新型相對穩定的格局。It is on the base of the specific historical tradition and the background of society and culture, according to the needs of society and its own condition and directed by the specific idea of run a university, independently and creatively, could win over, integrate and optimize higher education resources and then gradually has an unique and steady integrative trait with comprehensive competitive. the trait is called the individuality of university. higher education resources are the sum total of the essential factors invested by the government, society, the people who receive education and the university itself, which can improve the function of higher education
探討大學個性與高教資源配置關系的前提是釐清個性、大學個性、高教資源以及高教資源配置的內涵，得出的結論如下：個性在不同學科具有不同的含義，教育學所說的個性可理解為個體的主體性表現；大學個性是指大學在一定歷史傳統與社會文化背景基礎上，依據社會需求及自身條件，在一定辦學理念指導下，自主地、創造性地爭取、整合、優化高等教育資源，逐漸形成綜合競爭力的獨特而穩定的整體性特徵；高教資源是指政府、社會、受教育者、高校自身共同投入高等教育領域的一切能增進高等教育功能的要素的總和；高教資源配置則是對高教資源在不同使用方向上的分配。分享友人