The geochemistry of CO2 and its sources and reactions in low-temperature geothermal water was approached in three ways; by carbonate mineral saturation, a component mixing model and by reaction path isotope modelling.
Jarðefnafræði CO2, uppruni og efnahvörf í lághita jarðhitakerfum var rannsakaður á þrjá vegu, með mettun kolefnis steinda, blöndunar líkani og með jarðefnafræðilegum samsætulíkanreikningum.