<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Chen‐Xing Zhou</style></author><author><style face="normal" font="default" size="100%">Ran Hu</style></author><author><style face="normal" font="default" size="100%">Deng, Hang</style></author><author><style face="normal" font="default" size="100%">Bowen Ling</style></author><author><style face="normal" font="default" size="100%">Zhibing Yang</style></author><author><style face="normal" font="default" size="100%">Yi‐Feng Chen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Surface‐volume scaling controlled by dissolution regimes in a multiphase flow environment</style></title><secondary-title><style face="normal" font="default" size="100%">Geophysical Research Letters</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2023GL104067</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">50</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Fluid-rock dissolution occurs ubiquitously in geological systems. Surface-volume scaling is central to predicting overall dissolution rate&amp;nbsp;&lt;em&gt;R&lt;/em&gt;&amp;nbsp;involved in modeling dissolution processes. Previous works focused on single-phase environments but overlooked the multiphase-flow effect. Here, through limestone-based microfluidics experiments, we establish a fundamental link between dissolution regimes and scaling laws. In regime I (uniform), the scaling is consistent with classic law, and a satisfactory prediction of&amp;nbsp;&lt;em&gt;R&lt;/em&gt;&amp;nbsp;can be obtained. However, the scaling for regime II (localized) deviates significantly from classic law. The underlying mechanism is that the reaction-induced gas phase forms a layer, acting as a barrier that hinders contact between the acid and rock. Consequently, the error between measurement and prediction continuously amplifies as dissolution proceeds; the predictability is poor. We propose a theoretical model that describes the regime transition, exhibiting excellent agreement with experimental results. This work offers guidance on the usage of scaling law in multiphase flow environments.</style></abstract><issue><style face="normal" font="default" size="100%">18</style></issue></record></records></xml>