Explicit representation of microbes, enzymes, mineral surfaces, and isotopic tracers helps explain soil organic carbon decomposition and priming

Xudong Zhu1,2, Jinyun Tang3, William J Riley2, Matthew D Wallenstein4 and M Francesca Cotrufo5, (1)Colorado State University, Fort Collins, CO, United States, (2)Lawrence Berkeley National Laboratory, Berkeley, CA, United States, (3)Lawrence Berkeley National Laboratory, Climate & Ecosystem Sciences Division, Berkeley, United States, (4)Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO, United States, (5)Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, United States