Carbon dioxide development in aerobic parts of lignite mining dumps: The influence of rising groundwater in the Cospuden-Zwenkau dump: II--Quantitative models

摘要

The variation of carbon dioxide in the Cospuden–Zwenkau dump, in the southwest of Leipzig in Saxony, Germany, is caused by a variety of reasons, some having to do with the different types of residual mining spoils used as lower and upper dump materials, and some having to do with the dynamical evolution of conditions both within the dump and externally as time progresses.