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解释水流对岩石进行溶解和侵蚀
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英语corrosion
岩石经化学作用而溶解慢慢变小、变细成土壤的过程，称之为溶蚀。这种化学作用主要有以下四类：
1. 岁月的溶蚀，让这座古老的城墙显得更加沧桑。
2. 雨水的溶蚀，使得石头表面形成了独特的纹理。
3. 海水的溶蚀，塑造了美丽的珊瑚礁。
4. 风沙的溶蚀，使得沙漠中的地貌千变万化。
5. 酸雨的溶蚀，对建筑物造成了严重的损害。
corrosion-腐蚀，侵蚀;
1.The minerals may have variously experienced reaction , resorption, and perhaps even growth, as they settled.
当矿物沉降之后, 它们可能经历了多种反应作用, 溶蚀作用甚至可能还有生长作用.
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2.This produces solution channels that develop mainly in the direction of the flow.
这样就造成了主要沿水流方向发育的溶蚀通道.
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3.The ores have crystalline granular and metasomatic textures and disseminated structure.
矿石主要是结晶粒状与交代溶蚀结构,浸染状构造.
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4.The reservoir physical property were primarily dominated by sedimentary facies 、 corrosion and dolomization.
储集物性主要受沈积相带及溶蚀和白云岩化作用的控制.
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5.Secondary porosity formed formed by unsteady mineral is beneficial to formation's development. "
不稳定矿物溶蚀形成的次生孔隙有利于储层的发育.
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6.The main reservoir types in Ordovician carbonate formation in Tahe Oilfield are dissolution fractures and caves.
塔河油田奥陶系碳酸盐岩地层的主要储集空间为溶蚀缝、洞.
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7.Prediction of solutionfissure and productivity of carbonate weathering crust reservoirs is a worldwide difficult problem.
碳酸盐岩风化壳储层溶蚀缝洞和产能的预测是世界性难题.
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8.The reservior space are mainly intergranular apricot kernel inner pore and dissolved pore.
储集空间类型主要有粒间孔、杏仁体内孔和溶蚀孔.
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9.Carbonate buried - hill of rifted basin has 3 basic types of reservoir: fracture, corrosion and pore space.
断陷盆地碳酸盐岩潜山发育了裂缝型 、 溶蚀型和孔洞型3种基本储层类型.
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10.The insoluble capsule body, fast - release theophylline tablet and erodible plug were prepared , respectively.
分别制备了不溶性囊身 、 茶碱速释片和溶蚀性盖塞片.
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11.Pickling of rock is an important problem in acidizing oil and water wells.
岩石矿物颗粒的酸溶蚀是油气井酸化增产技术中的重要问题.
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