Paragenetic association I are composed of dissolved feldspar, quartz overgrowth and authigenetic kaolinite, This paragenetic association came into being acidic environment; Paragenetic association II include illite性爱一区二区三区、albite、dissolved authigenetic quarze and kaolinite春色校园激情综合在线影院、dolomite中文字幕字幕网在线、ankerite and ferrocalcite, the paragenetic association formed alkali environment; secondly, outcrop sandstones include paragenetic association III making up of dissolved feldspar、kaolinite直接在线观看的毛片网站、dickite and ironstone too, this paragenetic association came into being ground surface acidic environment.

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The author creates the AutomaticallyDiscriminational Model for the Classification of Sandstones System, thatis to say, people can complete the vastly sample s classification of sandstonesaccurately and swiftly, meantime, diminish the possibility of mortal mistake. Based on the study of the basic sandstone component before embedding, the typeof authigenic mineral, and the forming mechanism of porosity in Upper Paleozoicreservoirs in Ordos basin, the author selects the reasonable experiment objects forWater-Rock Interaction modeling study, designs the relatively reactant and resultantduring the diagenesis period, builds the solid-liquid thermodynamics model with theprinciple of thermodynamic phase equilibrium for kinds of primary minerals (potashfeldspar, albite, anorthite, and pyroxene, hornblende) which dissolve in acidic media,and forms the corresponding thermodynamics test database.

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It includes determination of properties of the acid protease and lipase, application of acid enzymes to processes of bating pickling pelt and wet blue of sheepskins, analysis of activities of collagenase in acid protease and trypsin. Comparison was conducted to acid bating and common bating. Orthogonal experiments were used to determine influence of some factors in acid bating on qualities of leather. Scanning electronic microscope was used to observe separating of collage fibers.

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For example, compounds containing phosphorus are converted to acidic materials which catalyze the thermal decomposition of the polymer.

例如亚州一二区，含有磷的化合物可以轉(zhuǎn)變成酸性物質(zhì)，它會催化聚合物的熱分解色色色城市。

The GFAP is a specific marker of astrocyte, its expression is more higher in the activity astrocyte, and finally the GFAP become the main composition of scar formations. The S -100 is a kind of acidity, dissolubilites, low molecular quantity and calcium hydronium conjugated protein, and it is mainly existed in neuroglial cell and schwann cell. It can promote the growth of axon, glial hyper-plasia and nerve divide and calcium's stability inside of cell, thus regulatin g the shape and metabolism of astrocyte . The quantity of S -100 protein and the degree of ischemia have direct proportion .

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The characters of geochemistry are rich alkali. And at the same time the content of calcium is high. They are rich in alkali, high in Potassium, enriched in LILE, LREE and Pb, depleted in HFSE and have a small Sr, Nd, Pb isotope range. Their source is probably a kind of even metasomatic mantle. This is consistent with the fact that there is kimberlite containing flogopite in the deep-source enclosure of Cenozoic super-K alkali lava in the southern part of this rock zone.

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According to authigenetic mineral association and nowadays stratum geochemistry character, combining the diagenesis character of sandstone in coal measure strata, it is thought to the fluid of outcrop sandstones went through ealy acidity- acidity-alkality-surficial acidity 4 fluid phases, the fluid evolution of core sandstones is ealy acidity- acidity- nowadays alkality 3 fluid phases.

由自生礦物組合以及現(xiàn)今地層水地球化學(xué)特征人人干人人操123，結(jié)合煤系地層砂巖成巖作用特征六月婷婷一区，認為露頭砂巖的流體經(jīng)歷了早期酸性－酸性－堿性－地表酸性4個流體階段，巖芯砂巖的流體演化為早期酸性－酸性－現(xiàn)今堿性3個流體階段东北老熟妇爱456视频。

The early stage of the Yanshan movement generated an Early Jurassic downfaulted basin and a Middle Jurassic compressional-downwarped coalaccumulating basin.In the middle stage,the Mid-Late Jurassic witnessed the formation of a volcanic downfaulted basin bounded by NW and NE deep faults,intermediate-basic and acid volcanic eruption and hypabyssal and near-sur...

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Mixture of BMIPF6 ionic liquid and acdic ionic liquid triethyl(propyl-3-sulfonyl ammonium methanesulfonate was prepared.

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As pH value varied in the course of diagenesis,reservoirs experienced one to three cementations or dissolution generations.Lots of secondary dissolution pores developed in the late diagenetic stage,because of the acidic mediums in the process of generation and migration of oil and gas. The anhydrites deposited in the dissolved pores resulted in the heterogeneity of secondary pores.

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acidic oxide：酸性氧化物,成酸氧化物

acidic medium 酸性培養(yǎng)基 | acidic oxide 酸性氧化物,成酸氧化物 | acidify 酸化,變酸

acidity：酸性

正常人的血液呈弱堿性(Weak alkalinity; PH7.35~7.45),當酒精 (Alcohol; C2H5OH) 進入人體,會使人體的血液呈酸性 (Acidity),酶有能力把它還原 (Reduction) 成弱堿性亦稱為堿化作用 (Alkalization),但是當酒精的酸化 (Acidify)速度,

basophilic erythroblast：早幼紅細胞(嗜酸性成紅細胞)

proerythroblast原紅細胞 | basophilic erythroblast早幼紅細胞(嗜酸性成紅細胞) | polychromatophilic erythroblast中幼紅細胞(多染性成紅細胞)

acidophilic erythroblast：嗜酸性成紅血細胞

acidophilic bacteria | 嗜酸細菌 | acidophilic erythroblast | 嗜酸性成紅血細胞 | acidophilic granulocyte | 嗜酸性粒性白細胞

acid former：成酸物質(zhì)

acid fixing bath 酸性定像浴 | acid former 成酸物質(zhì) | acid fuchsin 酸性品紅

acid hydrolysis：酸性水解

黃麴毒素B1經(jīng)由飼料進入體內(nèi),到達肝臟之微粒體(Microsome)在NADH2及O2存在下氧化為B1-2,3 oxide氧化的,此化合物具有高度之親核性(nucleophilic)會攻擊RNA與RNA中之-0-或N-group形成RNA bound B1之產(chǎn)物,再經(jīng)由酸性水解(Acid hydrolysis)過程轉(zhuǎn)變成毒性較低之2,

Nonacid forming：非成酸性

非共生性 Non symbiotic | 非成酸性 Nonacid forming | 非必要元素 Nonessential element

acid-forming：成酸的,酸性的

acid-fast || 不易被酸褪色的, 抗酸的 | acid-forming || 成酸的, 酸性的 | acid-resistant || 耐酸的

acid-forming food：成酸性食品

acceptable risk level 可接受的危險水平 | acid-forming food 成酸性食品 | Achromobacterium 無色菌屬

acid peat soil：酸性泥碳土

acid oxide ==> 酸性氧化物,成酸氧化物 | acid peat soil ==> 酸性泥碳土 | acid phosphat of lime ==> 重過磷酸鈣