濕潤度 的英文怎麼說

中文拼音 [shīrùn]
濕潤度 英文
wettability
  • : Ⅰ形容詞(沾了水的或顯出含水分多的) wet; damp; humid Ⅱ名詞(姓氏) a surname
  • : Ⅰ形容詞(細膩光滑; 滋潤) moist; smooth; sleek Ⅱ動詞1 (加油或水 使不幹枯) moisten; lubricate 2 ...
  • : 度動詞[書面語] (推測; 估計) surmise; estimate
  • 濕潤 : moist; humectation; humidification
  1. Adds silvery brightness to gray hair and neutralizes brassy tones in all shades. formulated with blue malva and coneflower to help impart wanted moisture and brightness

    中和所有顏色秀發的黃銅色,增加灰發的光澤。藍曼娃和矢車菊配方,增加秀發的濕潤度和亮澤。
  2. Based on the field investigations and laboratory examinations, a study of the population of the epiphytic dolichomitriopsis diversformis ( mitt. ) nog. in fanjing mountain reveals that its habitats are different among different host trees, but that there lies the common habitat characteristics of not more than 2m height from the bottoms of host trees trunks, less light, high relative humidity, slow wind speed, slow evaporation speed and long time of remaining humid in middle - lower tree bark ; that it is one dioecious moss species, the morphology is remarkably different between its perichaetium and perigonium, the number of its perichaetia is much more than that of its perigonia, its perigonium is difficult to find out, its sporophyte is upright, its seta is long and thin, its capsule is regular long oval and its calyptra is cucullate

    摘要通過野外調查和室內觀測對貴州省梵凈山樹附生尖葉擬船葉蘚種群的研究表明,其生境因其所附生的樹種不同而有所不同,但具有共同特點:附生在樹干下部距地面2m高的范圍之內,光照弱、大、風速小、蒸發量小、中下部樹皮保持的持續時間長;其為雌雄異株蘚種,雌、雄器苞形態差異明顯,雌器苞數量多,雄器苞數量少並且難于發現,孢子體直立,蒴柄細長,孢蒴規則長卵形,蒴帽兜形。
  3. Mainly used as a raw material for the manufacture of guanamine, gibuanide, various resins, trimeric cyanamide, fire retardant etc

    具有去污發泡乳化分散等性能,生物降解90 。
  4. Suitable for very sensitive skin types due to the healing properties attributed to the remarkable helichrysum essential oil immortelle in this moisturizer

    可有效地令肌膚重生,適用於一些問題皮膚,如疹,極敏感等,可保持皮膚及促進問題皮膚的修復。
  5. The soils ( paleudults ) consist predominantly of light brown fine loamy sand to fine sandy loam changing with depth into a brown sandy clay loam and sandy clay with red mottles

    土壤(強發育老成土)主要為淡棕色細壤質砂土到細砂質壤土,隨著深增加,土壤變為棕色砂質粘壤土和帶有紅色斑點的砂質粘土。
  6. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面分析來看,本區在全新世早期氣候回返,相對較寒冷乾燥,東亞冬季風影響較明顯,此時為沙層堆積向砂質土壤過渡,自北至南堆積的沙粒漸細;全新世中期氣候溫暖,東亞夏季風影響顯著,此時為明顯的成壤期,表現在自北至南普遍可見發育較好的黑壚土層,且南部的成壤作用比北部好,土壤的厚也要大;全新世晚期至今,氣候向乾冷方向轉化,但變化幅遠小於末次冰期。
  7. On the influence of global change of cenozoic climate and uplift of himalayas, the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in pliocene

    受新生代全球氣候變冷和喜馬拉雅運動的影響,該盆地一方面受印洋季風的影響增強,干季節交替明顯;另一方面受地形地貌影響,沿襲了溫暖的氣候條件。
  8. The modified zndx in comparison with others is well indicative of the severity and extent of flood / drought event and of more objective classification of them, which is therefore quite applicable to a extended area. ( 3 ) the main anomaly structures of grades of drought / food in summer over northwest china present pluvial pattern and dry pattern in all the areas, and spatial changes are opposite pattern from the noth to the south and the west to the east. the first four rotated loading vector fields represent four principal precipitation anomaly areas : the weishui river basin, east of the qinghai - xizang plateau

    但修訂過的zndx指數根據氣溫、土壤及前期氣候濕潤度等因子能夠客觀的反映出西北地區的旱澇特徵。 ( 3 )西北地區季與年區域旱澇等級表明:西北地區的乾旱雨澇有顯著的階段性和年際變化特徵。 1980 』 s到1990 』 s中期,氣候較,土壤增墑較明顯; 1990 』 s中期以後是40年乾旱最異常的時段; 1960 』 s旱澇交替發生,旱澇趨勢接近常年; 1970 』 s氣候雖乾旱,但沒有1990 』 s中後期顯著。
  9. The existence of south great wall need no more testification. the " border wall of miao area " had nothing different in time. framework and function from the north great wall except the area it passed with humid climate and dense population, so the peculiarly cultural background of the great wall as functional borderline between different ethnic cultures in history was embodied clearly in a little county. it is advantageous for us to rootle cultural content of the great wall and produce popular brand of tourism on the great wall culture

    中國南方長城的存在已是不爭的事實,苗疆邊墻不論從修築的時間、結構和功能上都與北方長城沒有什麼兩樣,不同的是它經過我國溫暖的地區,那裡民族眾多,人口密較大,從而使長城作為歷史上中國特定地區不同民族文化之間的功能界線,這一特有的文化背景,在更小的區域內得到了清晰地體現。
  10. Trees in leaf and in soggy ground are blown over easily by high winds and are damaged much more than trees after leaf falls.

    土地上,帶葉樹容易被強風吹倒的危害程比落葉以後大得多。
  11. To the influence of the plateau terrain, the impact of the elevation and the roughness of terrain to every energy component out and incoming are study, and basing the soil spectrum model proposed above, a new radiative transfer model of terrain area was put forwarded in which the soil water content, lai, terrain roughness and elevation were considered synchronously, and incoming scatter light was integral with the solid angle of semi - globe space defined by the slope of the pixel, so scattering lights of terrain and the sky are properly considered, but the operation is still within the acceptable range

    地形與反射率的關系是本文研究的一個重點。本文對崎嶇山地象元的各入射光和反(散)射光分量進行了深入分析,在所提出的土壤光譜模型和植被冠層模型的基礎之上進一步提出了新的適合青藏高原的山地輻射傳輸模型。該模型同時考慮了土壤含水量、植被覆蓋( lai ) 、地形起伏和海拔高的影響,並以象元坡面定義的半球空間立體角對環境入射光進行積分,使周圍地形和天空散射光均得到適當考慮,計算量又在可接受范圍內。
  12. Testing method of wettability of glass substrate

    玻璃襯底材料濕潤度的試驗方法
  13. For accumulating heat from piping and making as even the temperatures in various spaces betwiin pipes an possible, gravel foundation is first laid, mortar is mixed fully by mixing ratio of 1 : 2, the floor is finished level and then perfect curig in damp condition is carried out

    為保證管路間蓄熱和溫均勻應鋪下砂礫層后進行配比為1 : 2的灰漿完成處理,不僅要保證地板水平,還要在狀態下自然乾燥,使得到徹底的養護,人為的養護會導致地板雛裂,應予以注意。
  14. Results showed : ( 1 ) if the proportion of water in the soil is lower than wilting coefficient, and if irrigating water is very little, ( irrigating water is spreading horizontally and vertically ) the relationship between the horizontal width ( x ) and the ? rtical depth ( y ) is remarkable. the equation is y - 0. 02 12x2 + l. 8546x - 17. 88. the related coefficient is r = 0. 9350

    結果表明: ( 1 )在土壤含水量低於萎蔫系數的乾燥條件下,進行微量穴滴灌,滴灌點土壤面直徑x與最大垂直面滲透深y呈顯著相關,數學模型為: y = - 0 . 0212x ~ 2 + 1 . 8546x - 17 . 88 ,相關系數r = 0 . 9350 ( 2 )在微量補水灌溉情況下,只有灌水量大於4000ml /穴,才能使滴灌水滲透到20cm以下土層,達到作物根系集中層,否則水分很難被作物吸收,造成滴灌水的浪費。
  15. The moisture degree indicated that all the four forests were humid annually, but different monthly

    年平均濕潤度計算結果表明各林型均為,但月濕潤度差異明顯。
  16. The skin wettedness is appropriate to the first environment.

    皮膚濕潤度處于與前一個環境相適應的狀態。
  17. Adhesives - wettability - determination by measurement of contact angle and critical surface tension of solid surface

    膠粘劑.濕潤度.通過固體表面接觸角和臨界表面張力的測量確定濕潤度
  18. Standard test method for surface wettability and absorbency of sheeted materials using an automated contact angle tester

    使用自動接觸角測試儀測定覆蓋材料表面濕潤度和吸收性的標準試驗方法
  19. By thoroughly analyzing the concept of " potential evaporation " and " wet environment area evapotranspiration ", using index of comparatively potential evaporation and comparatively actual one, the complementary relationship between actual and potential evapotranspiration was testified entirely with data integration technique. 2

    選擇適合的「潛在蒸散」和「環境蒸散」的估算式,利用相對潛在蒸散量指標,相對實際蒸散量指標及流域濕潤度,通過數據集群技術,完整模擬並展現了蒸散互補相關關系。
  20. The correlativity between theoretical value and the actual value of soil moisture content in 93. 3 percent of observational stations is distinct. all this shows that calculational methods of zndx is more reason for studing the flood or drought of northwest chine. ( 2 ) index _ z and index _ k ca n ' t objectively remark extent of drought and flood event. both ca n ' t distinguish the difference of some years which have the same precipitation and have different temperature, awc

    西北地區10個代表站三種指數值的對比表明, z指數與k指數僅反映西北地區同期的降水,而zndx指數不僅反映了同期降水狀況,且與同期氣溫及前期氣候濕潤度有關。 ( 2 )通過z 、 k與zndx指數對西北地區旱澇等級的對比研究表明, z指數與k指數對西北地區旱澇等級的確定不具有客觀性。
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