石化作用 的英文怎麼說
中文拼音 [dànhuàzuòyòng]
石化作用
英文
lapidify-
Weathering prepares the rock for transport by decomposing and disintegrating it.
風化作用通過分解和崩解準備了要搬運的巖石。The catalytic mechanism of expansible graphite in esterification and the causes behind the lower esterification were discussed
推斷了可膨脹石墨在乙酸乙酯合成中的催化作用機理,分析了可膨脹石墨催化乙酸乙酯合成產率偏低的原因。There the soil is from weathered limestone soil or loess.
那裡的土壤是經過風化作用的石灰石土壤或黃土。( c ) the total energy of manganate - oxides materials decreases after intercalation lithium. the electrovalent bond weakens and the covalent bond strengthen between manganese and oxygen due to ion polarization effect, which makes the spinel structure more stable
( 3 )對于錳系材料嵌鋰后,體系總能量降低;鋰離子的靜電作用和極化作用,使錳氧之間的離子鍵成分減小,共價鍵成分增加,整個尖晶石骨架結構更加穩定。Quartz core zones : mineralisation occurs in enclaves of albitisation around the core of the pegmatite. tantalite crystals are large and randomly distributed
石英核心帶:礦化作用存在於被納長石礦包圍的偉晶巖核心。鉭鐵礦呈現巨大而不規則分佈。The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures
原生巖石為亮晶鮞粒石灰巖和泥晶鮞粒石灰巖,白雲石化作用使其巖石結構大多遭受破壞。Weathering of rock is essentially a static process.
巖石的風化作用基本上是一種靜力作用。The author finded out that the rice in the mediums with phosphorus and phosphate rocks can grow well, the quantity of the algea and the phosphorus in the mediums increase. on the contrary, in other mediums the rice appear to be short of phosphate
其中,全磷培養基和含磷礦石粉的無磷培養基中雜交水稻正常生長,沙角衣藻生物量較實驗前有所增長;由於實驗梯隊磷礦石的轉化作用,使培養基有效磷濃度均較實驗前也有所增長;而其他實驗組水稻均出現不同程度的缺磷表徵。The diageneses which are constructive to the reservoirs are mainly dolomitization and burial dissolution
對儲層起建設性作用的成巖作用主要有白雲石化作用、埋藏溶解作用。According to the mechanism of dolomitization, it can be divided into penecontemporaneous dolostone and post - penecontemporaneous dolostone
白雲巖可據白雲石化作用的機理和時間分為準同生白雲巖和準同生后白雲巖兩大類。By the phenomenon came from critical sand - gravel granular mixtures slope experiment, the falling causation, form, scale, and preventing principal in sliding - sand slope were discussed. the causation can be drawn : the slope received sands from the slope top continuously ; non - uniform degree and granular size in strong weathering environment may be changing ; and the restrain in slope foot was weakened. these factors, cause the fal
結合乾燥沙石臨界單面坡實驗現象觀察,對溜砂坡災害的產生原因、崩塌特性及防治原則進行了討論,提出溜砂坡崩塌的三個主要成因:寒凍風化引起上部沙粒來源的持續不斷;坡面的風化作用使顆粒進一步均勻、細化,造成原來處于亞臨界而穩定的坡面達到臨界而容易失穩;坡腳對牽引式崩塌的制衡作用削弱,易受坡腳干擾而誘發。The finding of dnaase in the earthworm the tissue extract of earthworm which had been diluted 28 times could digest 4 ul pbv220 - r - inf ( 6. 66 u g / ul ) completely at 37 @ in a hour but it had no effect on rna
雙胸蚓組織中dna酶的發現28倍稀釋雙胸蚓組織粗提液37保溫1小時,可將4vlpbv220 。 y一inf質粒( 6石6119 11l )完全消化但對rna無消化作用。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沉積物地球化學與化學風化進程和機械剝蝕率化學風化指數與化學風化率屬于表徵化學風化作用意義不同的函數,前者為相對概念反映流域巖石在原巖基礎上己發生淋溶作用的深度,主要受到了氣候因子的深刻影響(中國流域沉積物化學風化指數由北到南呈有規則的遞增序列,氣候因子對風化進程的影響掩蓋了巖性的巨大差異) ,而化學風化率含義是指單位流域面積巖石風化淋溶產生的離子絕對總量。Principle : it is adoping tattered dose to blend inner place the pouing perforate against water, utilizes such water action to come into being swelling the pressu ` re, by the rock, confuses soil forms piece and so on the brittleness substance distends to crack either cuts
原理:它是採用破碎劑與水混合灌入鉆孔中內,利用其水化作用產生膨脹壓力,將巖石、混泥土構件等脆性物體脹裂或切割。( s ) weathering and unloading action which are the two main exogenous process is active in epigenetic - surface. so, although one is different with the other, they are associated with each other closely and are cntrolled by geostress and seepage fields. in fact, weak weathered zone corresponds to weak load - off one, strong weathered zone corresponds to strong load - off one in virtue of result of this dissertation. ( 6 ) rock mass is a geologic body which is composed of rock and structural plane. and under the condition of geostress. temperature and seepage fields, correspondingly. studying weathering should pay attation to the aspects of rock, structural plane and fields. according to this. the author subdivises rockmass weathering into rock weathering and structural weathering, ulteriorly, the dissertation studies rockmass weathering from three aspects as follows : ? ock weathering : aberrance degree of mineral and physical mechanical performance of weathered rock ; ? e have already knew that weathering action damage the integrity of rock mass, but few applies it to engineering practice. the dissertation is based on trend o
本文研究結果為弱卸荷與弱風化大致對應、強卸荷與強風化大致對應; ( 6 )巖體是由組成它的巖石與缺陷賦存於一定環境場中的地質體,據此本文將巖體風化細劃為巖石風化與結構面風化,並進而將表徵巖體風化的指標相應地歸結為三個方面來加以研究並應用於工程實踐,這就是:對于巖石風化,主要為礦物的變異程度與風化巖石的物理力學性能研究:雖已認識到風化作用破壞了巖體完整性,但將該理論應用於巖體風化分帶卻不多見,本文即從淺表部位硬性結構面間距、條數、跡長、塊度等隨遠離臨空面的變化規律來研究巖體風化分帶:不同風化、卸荷程度的巖體實際處于不同環境場中,彈性波速變化與特定環境場相對應,因而是反映巖體風化、卸荷的綜合因素。The tiny, delicate skeletons are usually scattered by scavengers or destroyed by weathering before they can be fossilized
微小纖細的骨骼通常在石化前就被食腐肉的動物拆散了,或者被風化作用破壞掉了。Because of long - time water erosion and weathering, the furface of the stone becomes uneven, looking like a rough sea
由於長年被水流沖蝕溶蝕及風化作用,使巖石表面凸凹不平,如同風吹過水面,捲起千層浪。We will also explore topics like sediment transport and deposition in modern sedimentary environments, burial and lithification, survey of major sedimentary rock types, stratigraphic relationships of sedimentary basins, and evolution of sedimentary processes through geologic time
我們也將會探討以下題目,例如沉積物搬運和現代沉積環境中的沉積作用,埋藏和石化作用,觀測主要的沉積巖類型,沉積盆地中地層的關系,和地質時期沉積過程的演變。The dolomitization is the base of forming high quality reservoirs
白雲石化作用是形成優質儲層的基礎。The dolostones have experienced several types of post - depositional diagenetic modifications, of which dolomitization, dissolution, recrystallization and tectonic stress processes have exerted an important effect on porosity and permeability
認為該白雲巖在沉積期后變化中經歷了多種成巖作用改造,其中影響白雲巖儲集性的作用主要有白雲石化作用、溶蝕作用、重結晶作用和構造應力作用,對白雲巖孔滲改善起了積極作用。分享友人