“…Karst has received more and more attention from international scholars, and s research results have been achieved on carbonate rock dissolution experiments, which mainly focused on indoor simulation experiments. For example, Li, N.Y. et al [13], L et al [14], and Hyunsang et al [15] simulated the dissolution reaction indoors by usi rock disk rotating and moving relative to the solution; Erik B. Larson et al [16], in indoor study of carbonate dissolution rates, found that the petrography and minera of carbonate rocks affect their dissolution rates in a laboratory setting; Plummer et al found large differences in calcite dissolution rates and their mechanisms of change un different pCO2 conditions by studying the kinetic mechanisms of calcite dissolution doors; Yu, S. et al [18] showed that the dissolution rate of carbonate rocks was affecte rainwater acidity and rainfall via an experimental indoor dissolution study of carbo Karst has received more and more attention from international scholars, and some research results have been achieved on carbonate rock dissolution experiments, which are mainly focused on indoor simulation experiments. For example, Li, N.Y. et al [13], Li, Q. et al [14], and Hyunsang et al [15] simulated the dissolution reaction indoors by using a rock disk rotating and moving relative to the solution; Erik B. Larson et al [16], in an indoor study of carbonate dissolution rates, found that the petrography and mineralogy of carbonate rocks affect their dissolution rates in a laboratory setting; Plummer et al [17] found large differences in calcite dissolution rates and their mechanisms of change under different pCO 2 conditions by studying the kinetic mechanisms of calcite dissolution indoors; Yu, S. et al [18] showed that the dissolution rate of carbonate rocks was affected by rainwater acidity and rainfall via an experimental indoor dissolution study of carbonate rocks by acid rain in Guilin, China.…”