流化作用 的英文怎麼說

中文拼音 [liúhuàzuòyòng]
流化作用 英文
fluidization
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  1. Cataclastic texture which came from brittle deformation made the jadeite quality bed, but the mylonitic texture which resulted from ductile deformation made the jadeite quality good

    在強大剪切應力和鈉質體的共同下,鉻鐵礦的淡是形成綠色的主要原因。
  2. The mechanism of the downburst formation was also investigated based on the cloud microphysics of the simulated storm and it was found that this downburst was primarily produced by hail loading, and enhanced by hail melting and rain evaporation. and the loading and the melting of hail played a very important role in producing the downburst. the gale at the surface was caused by the severe downburst

    從雲微物理學角度分析了此次局地性大風的形成原因,認為由高空冰雹粒子的拖曳產生的負浮力是促發強下沉氣產生的主要原因,其次是冰雹的融和雨水蒸發冷卻對下沉氣起加速,冰雹的拖曳和融對下沉氣具有決定性的
  3. Elementary geochemical study on the roles of fluids during metamorphism

    變質的元素地球學研究
  4. The main results are following : ( 1 ) the variation of clay / silt ratio can indicate the secondary clay action of dust depositions ; the variations of magnetic susceptibility and total fe content are inferred to be records of the changeable intensity of bio - pedogenesis ; the variations of sr content and rb / sr ratio can indicate bio - pedogenesis, dissolving and leaching action ; the content of total organic carbon ( toc ) can reflect variation of climate and vegetation during soil formation, it indicates the intensity of weathering and bio - pedogenesis ; the content variation of caco3 can show the intensity of dissolving - leaching action and secondary deposit, which was noted as pseudomycilia in pores and fissures in the sediment, so it can indicate the intensity bio - pedogenesis quite well. these proxy indexes also reflect obvious regional difference of pedogenic environment and the intensity bio - pedogenesis ; namely, secondary clay action, dissolving - leaching action and bio - pedogenesis are all much stronger in south than that in north

    實驗結果表明:粘粒粉沙比值能很好地指示粉塵堆積物的次生粘;磁率和全鐵很好地指示生物風成壤; sr和rb sr比值能很好的指示生物風成壤和淋溶;總有機碳( toc )含量的高低,在一定程度上反應了土壤發育過程中氣候和植被狀況的變,指示著成壤過程中腐殖質的程度; caco3含量的變,可以反映了黃土古土壤形成時的風成壤的強弱程度,指示成壤過程中的淋溶和次生碳酸鹽;並且各指標所指示的成壤環境和成壤強度存在明顯的區域差異,即渭河域土壤的生物風成壤、次生粘和淋溶均表現出南部強于北部。
  5. Purification of surface water nitrogen and phosphorus pollutants by zhalong riparian wetland

    扎龍河濱濕地對地表徑氮磷污染物的凈
  6. The holes themselves have a restricting or stabilizing effect because flow may become sonic.

    因為這時動可成為音速動,所以這些小孔本身有一種節製或穩定
  7. ? he pretreatment of ne together with yohimbine, an a, adrenergic receptor antagonist, had no effect on the facilitatory action of capsaicin on neurotransmitter release from primary afferent terminals. this result suggests that the a2 adrenergic receptor on primary afferent terminals might be involved in ne depression on capsaicin - induced neurotransmitter release

    將飛型腎上腺素受體阻滯劑育亨賓( yohimbine )與ne同時預灌后, caps對初級傳入終末遞質釋放的易不受影響,提示初級傳入纖維終末上的a 。
  8. The low solubility of calcium zincate produced from the chemical reaction of zinc oxide and calcium hydroxide in alkaline solution can improve the cycling life the zinc electrode, and the discharge capacity will tend to be stable. furthermore, the effects of la2o3 additives on the electrochemical performances of zinc electrodes were investigated. the results shows that the addition of la2o3, in zinc electrode can improve the area of reduction peak and the hydrogen evolution potential which means the cathodic hydrogen evolution reaction can be hindered

    鋅與氫氧鈣在堿性溶液中學反應生成的難溶於堿的鋅酸鈣可以使鋅電極的循環壽命得到提高,放電容量也趨于平穩,此外還考察了氧鑭對鋅酸鈣電極電學性能的影響,結果表明:添加適量氧鑭能明顯改善鋅電極的電學性能,使鋅電極的還原峰電位正移,電極反應可逆性得到改善,同時也可抑制鋅電極析氫反應的發生,提高了鋅電極的陽極電,對陽極反應有一定的活;同時還可以改善鋅電極的放電特性,增加電極的放電容量。
  9. Through field investigation, microscopic study, x - ray phase analysis and mineral infrared spectrum analysis, the authors determine the laumontitization had occurred widely in the axi gold field. according to the development of laumontitization and its relationship to mineralization, authors reveal that the laumontitization appeared mainly at the top and periphery to ore - bodies. it befallen at the edge of the geothermal fluid system or happened in the late stage of geothermal fluid system evolution, hence can be assigned as an indicator to prospect for epithermal gold deposit. the fluid causing laumontitization in the axi gold deposit is similar to those causing hot spring type gold deposit or in modern geothermal field. the fluidization of the axi gold deposit happened in carboniferous, showing the west tianshan is a good district for epithermal gold mineralization and preservation. so west tianshan is prospecting for exploring epithermal gold deposit

    通過野外考察顯微鏡下薄片鑒定x射線物相分析和礦物紅外光譜等研究,確定了阿希金礦濁沸石的普遍存在根據濁沸石發生的規律及其與礦床形成的關系,確定濁沸石主要見于礦體的上部和外圍,發育在地熱體系統的邊緣和演晚期,可為尋找淺成低溫熱液型金礦的標志之一。導致阿希金礦濁沸石體性質與熱泉型金礦成礦體和現代地熱田類似,發生在石炭紀,證明西天山地區具有良好的淺成低溫熱液型金礦的形成和保存環境,因此找礦前景較好。
  10. The hydrothermal breccia and karst in the beiya area are divided into 4 types and zones, including : sedimentary tuff and breccia induced by hydrothermal explosion and sedimentation on land surface ; hydrothermal sedimentary conglomerate and gas - explosive ejecting breccia related to sedimentation in and collapsing of some shallow karst caves ; netted hydotherma1 limcstone breccia and hydrothermal explosive breccia pipe related to hydrofracturing, corrosion and explosion in the hydrothermal channels ; and yellow granular limestone formed by simmering and alteration in the deep heated water reservoir

    北衙地區熱水角礫巖和熱水巖溶可分為4種類型和層次,即地表相爆發沉積形成的沉積凝灰角礫巖、熱水沉積鮞狀灰巖與鈣華膠結角礫巖;與近地表洞穴沉積和垮塌有關的熱水沉積礫巖和汽爆射角礫巖;與熱水通道相蝕裂和爆破角礫有關的網路狀灰巖角礫巖筒和熱水隱爆角礫巖筒;深部相熱水浸煮蝕變灰巖。
  11. Severe fires can often cause changes in successional rates and soil hydrologic functions, degradation of soil physical properties, alter c : n ratios, and result in subsequent nutrient loss through accelerated erosion, leaching or denitrification, and alterations in microbial populations and associated process can occur

    高強度火燒往往能引起演替頻率的改變,土壤物理性質退,水文功能發生改變,改變c n比,加劇侵蝕、淋溶和反硝,導致養分火,微生物數量及其相關過程發生變
  12. Many studies had attempted to characterize chemical weathering process by focusing on geochemisty of river particulate and sediment. the sediment geochemistry may reflect and compare with the carbonates and silicates weathering degree by introducing the chemical index of alteration ( cia ) and new sediment index of variation ( siv ) and elemental molar abundance ratio of the sediment. the one main objective of this study would provide and compare the relative weathering intensities of silicates and carbonates with the different basins

    2沉積物地球學與學風進程和機械剝蝕率學風指數與學風率屬于表徵學風意義不同的函數,前者為相對概念反映域巖石在原巖基礎上己發生淋溶的深度,主要受到了氣候因子的深刻影響(中國域沉積物學風指數由北到南呈有規則的遞增序列,氣候因子對風進程的影響掩蓋了巖性的巨大差異) ,而學風率含義是指單位域面積巖石風淋溶產生的離子絕對總量。
  13. Correlations between strontium isotope of river water and chemical weathering in karst areas, guizhou province

    貴州河河水的鍶同位素與喀斯特地區學風
  14. The furnace in the picture is a blast, literally. a blast furnace increases combustion with a blast of air

    照片中的爐子是一陣貨真價實的鼓風爐。鼓風爐利來增進氧
  15. All these systems present good assembly capability. cds / cupc and cds / ppv optoelectronic cells have been assembled and cupc presents best sensitization to cds

    制備了cds cupc 、 cds ppv光電池,均發現有陰極電產生,其中cupc對cds的敏較好。
  16. Cu et al minerogenetic elements were liberated from stratum by the affection of the mixed fluid, overprinted and alternated the original mineralization, and form xikuangshan type copper deposit

    在這種混合下,地層中cu等成礦物質析出,疊加改造了初始銅礦,最終形成稀礦山式銅礦。
  17. Abstract : enhancing function of pulsating draught for sintering process is studied with simulative burden in the laboratory. the experiment results indicate that sintering velocity is the fastest along with appropriate pulse draught frequency when negative pressure is lower

    文摘:採模擬原料,在試驗室內的脈動燒結裝置上,進行脈動氣燒結試驗,探討了脈動氣的頻率變和抽風負壓等因素對燒結過程的強
  18. Basin tectonic evolution - fluid system - mineralization is a new research task in ore - deposit

    盆地構造演體系統、礦是當代礦床學研究的新課題。
  19. Because of long - time water erosion and weathering, the furface of the stone becomes uneven, looking like a rough sea

    由於長年被水沖蝕溶蝕及風,使巖石表面凸凹不平,如同風吹過水面,捲起千層浪。
  20. ( 7 ) the main mechanics mechanism to happen large deformation is that the rock intenerated by the water, and producing flowing deformation along with the time

    ( 7 )鷓鴣山隧道發生圍巖大變形的主要力學機制是在地下水的軟下,以擠出、變為主,膨脹為輔。
分享友人