Test of carbonate rock sample ' s dissolution reveals that lithology ' s effects on dissolution mainly lie on their different start - up dissolution velocities 摘要對(duì)碳酸鹽巖類巖石樣品的溶蝕試驗(yàn)表明,巖性對(duì)溶蝕的影響主要表現(xiàn)為各類巖石在啟動(dòng)溶蝕速率上的差異。
In the same conditions of temperature , pressure and specific surface area , the start - up dissolution velocity of limestone sample is more than the dolostone ' s one 在相同溫壓、相同比表面積的條件下,灰?guī)r類巖石樣品的啟動(dòng)溶蝕速率大于白云巖類巖石樣品的啟動(dòng)溶蝕速率。
Waste - silicate glass - test for determination of the initial dissolution velocity on contact with a regularly renewed aqueous solution , regenerated within a closed circuit by evaporation and condensation 廢品.硅酸鹽玻璃.通過蒸發(fā)和濃縮在一封閉環(huán)管內(nèi)重新產(chǎn)生的,不斷更新的含水溶液的接觸中初始溶解速度的測定試驗(yàn)
However , when the samples have different effective contact areas , the degrees of dissolution may depend on the swing of the pendulum between the dissolution velocity and their effective contact area 但當(dāng)樣品在水巖反應(yīng)過程中有不同的比表面積時(shí),溶蝕作用的強(qiáng)弱或快慢就取決于巖石溶蝕速率與水巖反應(yīng)有效接觸面積的消長關(guān)系。