This shows you the differences between two versions of the page.
Both sides previous revision Previous revision | Next revision Both sides next revision | ||
start:hype_model_description:hype_orgc [2018/08/15 14:18] cpers [Riparian zone] |
start:hype_model_description:hype_orgc [2018/09/03 15:25] cpers [Turnover of humusC] |
||
---|---|---|---|
Line 49: | Line 49: | ||
==== Turnover of humusC ==== | ==== Turnover of humusC ==== | ||
- | Turnover of humusC is a sink for humusC and a source of OC in all soil layers (k = 1.3). The loss of humusC does not all go to the TOC, ut a proportion (parameter //minc//) is mineralized. Turnover (//transhC//, //mg/m2/d//) depends on a general parameter (//kho//), temperature function (//tempfcn//), humidity function (//smfcn//) and the pool of humusC (//humusC//). | + | Turnover of humusC is a sink for humusC and a source of OC in all soil layers (k = 1.3). The loss of humusC does not all go to the DOC, but a proportion (parameter //minc//) is mineralized. Turnover (//transhC//, //mg/m2/d//) depends on a general parameter (//kho//), temperature function (//tempfcn//), humidity function (//smfcn//) and the pool of humusC (//humusC//). |
<m> transhC(k) = kho * tempfcn(k) * smfcn(k) * humusC(k) </m> | <m> transhC(k) = kho * tempfcn(k) * smfcn(k) * humusC(k) </m> |