水化變異 的英文怎麼說
中文拼音 [shuǐhuàbiànyì]
水化變異
英文
hydration variation-
The coefficient of variation of saturated water content decreased with the depth of profile. the coefficient of variation of bulk density and field capacity fluctuate with depth of soil
飽和含水量的變異系數都隨深度的增加逐漸降低,含水量、容重和田悶持水量的變異系數隨深度的呈波動變化。In the mouth of the bohai bay, there was a clockwise gyre in summertime of 1958 associated with the low - salinity and low - density center, and the gyre is replaced by an anticlockwise gyre associated with the high - salinity and high - density
與渤海溫鹽場和環流場變異相應,渤海和黃海的水交換量也發生了變化,現在的渤海和1958年時相比與黃海的水交換量呈減少趨勢。In fact, it is the special system of our country that increase the incoherence and unconditionally of all the stockholders and the lack of the true investors. these two elements increase the stockholders " dissimilated behavior. in dividend policy, the difference of payment level resulted from the variance of the controlling degree embodies not the difference of stockholders " decision making to increase the company " value but the particular preference of the nonnegotiable shareholders and the management
而最根本的原因是由於我國特定製度安排導致了股東群體的非一致性和非制約性的強化以及真正投資主體的缺位,兩個因素的共同作用加劇了股東行為的異化,表現在股利政策上,由股權控制度變化產生的支付水平差異主要體現為非流通股股東及管理層的特殊偏好,而從質的角度,以公司價值為目標的真正股東化主體的決策差異分析無效。I find that the difference between male and female teacher is significant on their conception of sustainable development, and the male teachers holds prior opinions. because of different sense on student development and student cognition, primary school teachers are differentiated from other group of teachers ; teachers with secondary school education background are differentiated from teachers with higher education background ; although there is no obvious difference on sustainable development resulted from age difference, there are teaching motives and emotional and physical quality differences in various age groups ; the aspect influenced mostly by age factor is the conception of teaching effectiveness ; school type is not related with the sustainable development of teacher. based on my research, i make the following suggestions to the practical scheme ( the life - long continuous education ) aimed at improving of sustainable development of teacher ' s quality
第三,通過對來自14所學校的272位教師問卷調查,統計分析發現:因學生發展觀和身心素質不同導致男女教師可持續發展系統水平產生差異,男教師優于女教師;因學生發展觀和學生觀不同導致小學教師與其他學段教師可持續發展系統水平產生差異,小學教師低於其他學段的教師;因學生發展觀和學生觀不同導致中專畢業的教師與其他學歷的教師可持續發展系統水平產生差異,中專畢業的教師與他學歷的教師有差距;雖然不同教齡段的教師可持續發展系統水平差異不顯著,但進一步比較發現,在教學動機和身心素質方面還是有差異的,並且與教齡變化最緊密的是教師的教學效能感;教師可持續發展系統水平與學校類別無關。The first geologic reason for degeneration of the eco - environment in the headwater area of the yellow river is that the increase of the recent geologic function caused desertification and grasslands resource decreased and underside changed, destroied the balance of water - air - heat in the area ; the second is that the water environment changes by the degradation and atrophy of frozen earth cause multilayer and synthesis cause of formation degeneration of the eco - environment ; the third is that the man and rats function accelerated degeneration of the eco - environment in the headwater area of the yellow river
摘要黃河源區生態環境惡化的地質原因之一是現代地質作用增強,形成以荒漠化為主的草地資源退化與下墊面改變,地區水氣熱平衡破壞;二是因凍土退化、萎縮,引起水環境變異,導致多層面與綜合成因的生態環境惡化;三是人為及鼠類活動對源區生態環境惡化起著推波助瀾的作用。According to the results of the compaction test and hearing ration test, it is discovered that the filled soil also has the swelling property after being compressed, which may result in the crack of the subgrade with the change of the water contents
通過對路基填土的擊實試驗和承載比試驗表明,填土壓實之後具有一定的膨脹性,在含水量變化差異性影響下的脹縮變形可能導致路基開裂。E. mollis had higher genetic diversity among populations, and the reason may be as follows : ( 1 ) those populations are generally large and are not subject to significant loss of variation through small - population effects such as random genetic drift and inbreeding coupled with selection
相對於26種長壽木本特有種和61種狹窄的地理分佈種來說,翅果油樹種群也具有高的遺傳變異水平。這表明翅果油樹種群不存在遺傳上的退化現象。Abstract : hydrochemical survey in four gold ore districts shows that the distribution of different forms in water exhibits regular variation in different regions and climate zones. this paper has preliminarily established distribution patterns of different forms of gold anomalies, thus providing grounds for hydrochemical prognosis of concealed ore deposits
文摘:通過對4個金礦區的水化學測量,發現水中不同狀態金分佈在不同地域氣候帶下呈規律性變化,初步建立水中不同狀態金異常分佈模式,為水化學預測隱伏金礦提供依據。It is the geographical data pretreatment to unite the map projection and to workout map of catchment basin for analyst and explaining anomaly of sand and geochemistry
地理數據處理主要是統一地圖投影變換和為分析解釋重砂和化探異常進行的匯水盆地圖的編制。As one ascends the etheric, the biology begins to transmute itself gradually over time to a new cellular structure that is known as “ crystalline ”, which is also a cellular structure that one ' s ancestry knew at an earlier time in human history upon earth
當他提升時,則以太層、生物層開始逐漸變異到新的分子結構中,也就是所稱的「水晶化」 , (注:看到其它譯法如晶體化,舍利子化)這也是他的祖先在地球人類歷史早期就了解的細胞結構。This research investigated the variability and the quantitative relationships among soil nutrients ( soil ph, total n, organic matter, available p ), growth status ( spad, lai and spad lai ) and yield of rice. all data were analyzed by both classical statistics and geostatistics based on gis. by further integrating gis, gps and crop management knowledge model, a decision support system for precision farming ( dsspf ) was developed, which laid a technical foundation for the practical application of precision farming system
本研究基於gis技術,以經典統計和地統計學為分析手段,確立了田區土壤養分(土壤ph 、全氮、有機質、速效磷、速效鉀) 、水稻作物長勢( spad 、 lai 、 spad * lai )和產量的空間變異特徵及定量關系;進一步以作物管理知識模型為智能決策支撐,提出了gis與模型及gis與gps的組件化集成技術,構建和實現了基於田區作物產量、土壤養分和苗情監測差異的精確農作決策支持系統( dsspf ) ,為精確農作系統的應用奠定了技術基礎。The paper main contents including : ( 1 ) the paper analyzed spatial variability of hydrology geological parameters ; and studied on the tendency and regulation of annual water table resource in shandianhe river in inner mongolia ; and analyzed the general changing tendency of water table with time ; analyzed and illustrated the conditions of supply, penetration and drainage of ground water. ( 2 ) the paper analyzed the data of rainfall, evaporation, transpiration and runoff, assessed the surface water resources. ( 3 ) the paper used drainage method of ground water and finite element method assessed groundwater resources and forecasted the water table in the future six years
內容包括: ( 1 )分析了水文地質參數的空間變異性並分析研究了地下水的歷年動態變化趨勢和規律及其補給、徑流和排泄條件; ( 2 )整理和分析了研究區的降水、蒸發和徑流資料,評價了地表水資源量; ( 3 )採用總排泄法和有限元法對研究區地下水資源量進行了評價,並對未來6年地下水水位進行了預測。It is indicated that the hydration process of cement - based materials with slag, fly ash and silica fume is different in some degree from that of neat cement because of the difference in mineral structure and hydration mechanism. the periods of accelerating, decelerating and terminating are prolonged and hydration reaction decelerates. the second peak of rate curve of the heat evolution could be divided into two small peaks, which are contributed to the hydration of clinkers and mineral mixtures at the temperature of 30 but when temperature comes to 50, the two small peaks combine into one and the reaction accelerates
結果表明,與硅酸鹽水泥相比,由於礦物摻合料與水泥熟料在活性和水化機理上的差異,水化歷程有較大的改變:多組分體系誘導期、加速期和衰減期延長,水化反應速率明顯降低;低溫時,水化放熱速率曲線上的第二放熱峰細化成分別對應于熟料和礦物摻合料水化的兩個小峰;高溫時,反應速率加快,雙峰合併;進一步研究發現,摻合料的種類與摻量對水化歷程也有較大的影響;建立了適用於多組分水泥基材料不同水化階段的水化動力學方程。The numerical simulation of moisture varying processes have not shown a good fit to the measured, showing a moisture varying model of simple reduction, and not revealed the distinct courses at various slope locations. however, after simulating by the selected parameters shown the difference between various slope locations, the the coefficient of efficacy ( ce ) was increased obviusly and reached over 0. 6, that is to say, the simualted results is reliable in a certain
土壤水分變化的數值模擬結果? ?坡耕地的上、中、下各部位的模擬土壤水分變化過程基本一致,這與實際觀測結果差異較大,因此,還不能準確反映坡耕地不同部位的水分變化特徵,但通過對模擬參數的調整,可獲得一定可靠性的模擬結果,盡管未達到很理想的程度。The hydrology system have some characters of complicated open macro system to a certain extent, the complexity and indeterminacy of the hydrology system becomes more and more standing out with the hydrology scale changing from the microscopical to the midscopical, even to the macroscopical, which present spatial variability, differ between the unit and the system, the model re - parameterization and the different scale model coupling
水文系統在某種程度上具有開放的復雜巨系統的特徵,隨著水文尺度由微觀到中觀、宏觀,水文系統的復雜性和不確定性就愈突出,表現有空間變異性、單元與系統的不一致性、模型的再參數化及不同尺度模型耦合等問題。Our pulp tableware always be in the priority of being using by the national mid & large instant food companies, such as kangshifu, unite enterprise, nissin, huafeng, longfeng, rongdi in shenyang, gigantic star in guizhou and so on
5 、變異后,自然降解泥化成為有機肥料,還原為二氧化碳與水,回歸大自然6 、產品經噴塗、覆膜后可提高其阻隔透氣性,助其不粘飯,冷藏時產品不易變軟Results show that the corresponding relations are significant between the feature of drought and flood years in significant abnormal regions of precipitation and changes of the same period three wind fields
指出降水顯著異常區域的旱澇變化與同期三層風場變化有較好的對應關系。全球陸地3 - 5月旱澇的變化和海溫變化之間存在一定聯系。It sets up a evaluated system by analyzing groundwater chemical components, through studying pertinence in water chemical component and soil strength, it also puts forward that water chemical change can map soil strength variation under water - soil interaction. from the theory of the water - soil interaction on, the interrelation of city construction, the variation of groundwater condition and the soil structure strength is analyzed and that the measure of soil structure and the significance which is by the water - soil interaction is studied in this paper. at the same time, in the paper : the recourse of the soil structure strength is summarized ; the physical meaning of soil mini - scale structure is defined ; the measure of soil structure is classified ; the four basis forms of the water - soil interaction is induced ; the chemistry mechanism of the water - soil interaction is discussed
通過水化學組份與土強度間的相關性分析,提出水化學組份的變異可以映射水土作用下土強度的變異;從水土作用的理論出發,分析了域市建設、地下水環境變異與土結構強度間的相互關系,研究了土的結構尺度及其在水土作用中的意義:總結了土的結構強度的來源、定義了土細觀結構的物理涵義井劃分了土的結構尺度及層次、歸納了水土作用的四個基本形式、討論了水土作用的化學作用機理。Though groundwater - soil interaction is long and slow, it is marked and transient the water ' s chemistry change comparing to the interaction between the water and soil during whole geological history process. the results of quantity accumulated in a short time will reduce to the soil ' s nature change
盡管地下水與地基土體之間的相互作用是長期的、緩慢的,但與土體形成和經歷的整個地質歷史進程的水土作用相比,水化學環境變異是顯著且短暫的,水土作用將會在短時期內進行量的積累,從而使土的性質達到質的變化。Because these factors make change more often, soil time space variability is more bigger. the relationship of single factor between soil water infiltration capacities and certain influencing factor could be established quantitatively by means of soil water infiltration tests in indoor, there is negative correlation relation between soil water infiltration capacities and soil structure. there is negative correlation relation in high grit content and low physical clay content soil, and second - degree polynomial relation in high physical clay content junk structural soil between soil water infiltration capacities and soil moisture
由於這些因素在時刻發生變化,使得土壤的時空變異性較大,只能用室內土壤水分入滲試驗來定量確定土壤水分入滲能力與某些影響因素之間的單因子相關關系,土壤水分入滲能力與土壤結構之間呈負相關關系,土壤水分入滲能力與土壤含水量之間在土壤砂粒含量高,物理性粘粒含量低的無結構土壤中呈負相關關系,在物理性粘粒含量高的團粒結構土壤中呈二次多項式關系。分享友人