白雲石模 的英文怎麼說
中文拼音 [báiyúndànmó]
白雲石模
英文
dolocast- 白 : Ⅰ形容詞1 (似雪的顏色) white 2 (清楚; 明白; 弄明白) clear 3 (空的; 沒加他物的) pure; clear; ...
- 雲 : Ⅰ動詞[書面語] (說) say Ⅱ名詞1. (雲彩) cloud 2. (雲南) short for yunnan province3. (姓氏) a surname
- 石 : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
- 模 : 模名詞1. (模子) mould; pattern; matrix 2. (姓氏) a surname
- 白雲 : bai yun
-
Burial dissolution mainly developed inside the primary micropores, the partly filled intergranular porosities and the intercrystal porosities, which furthermore formed lots of enlarged pores, intergranular pores, oolimolds
埋藏溶解作用主要在粒間半充填剩餘縫隙、交代白雲石的晶間孔內進行,這進一步溶蝕造就了大量超大孔隙、粒間溶孔、粒內孔、鑄模孔等。The results demonstrate that the pingba red residua is a typical in situ chemical weathering crust, and the material sources of the profile are derived from underlying triassic dolomites, the chemical weathering of dolomite can be divided into two stages : " leaching - accumulating trend " and weathering trend ", the stable teconic and whole weathering of dolomite should be the main reason for the development of thick and consecutive red weathering crust overlying dolomite rock in central guizhou
結果顯示該剖面是下伏基巖白雲巖風化成土並累積的結果,無其他外來物源,是原位風化殼;成土過程具有兩階段模式特徵,即白雲石、方解石的溶蝕酸不溶物累積和酸不溶物進一步風化兩個階段;長時期的構造穩定和白雲巖整體溶蝕作用是黔中地區白雲巖風化殼土層厚度大、分佈連續的主要制約因素。This paper ( 1 ) overviews the development of geochemical reaction modeling, ( 2 ) explains the theory and equations employed by geomodel 1. 0, ( 3 ) briefly presents the flow of the program, ( 4 ) displays the interface and functions of geomodel 1. 0, ( 5 ) shows two reaction examples and does some analysis, and ( 4 ) summarizes the features and shortcomings of geomodel 1. 0
本文將: ( 1 )系統的總結地球化學反應模擬的理論及其發展歷史和現狀; ( 2 )闡述geomodel1 . 0中引用地球化學反應模型原理和方程; ( 3 )介紹geomodel1 . 0中編碼和流程; ( 4 )介紹geomodel1 . 0的界面及功能; ( 5 )展示白雲母和鉀長石溶解實例,並對鉀長石的溶解模擬結果進行分析; ( 5 )總結軟體的特點及存在的不足。
分享友人