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)Colorado State University, Department of Soil and Crop Sciences, Fort Collins, United States
