diff --git a/user_guide/doc/source/namelists/jules_soil_biogeochem.nml.rst b/user_guide/doc/source/namelists/jules_soil_biogeochem.nml.rst
index a138b99..443aed4 100644
--- a/user_guide/doc/source/namelists/jules_soil_biogeochem.nml.rst
+++ b/user_guide/doc/source/namelists/jules_soil_biogeochem.nml.rst
@@ -115,6 +115,34 @@ If using the ECOSSE soil model, most soil parameters are read from a separate fi
 
           .. note:: If layered soil C is used (:nml:mem:`l_layeredc` = TRUE) the temperature and moisture of each soil layer is used to calculation respiration from that layer.
 
+   .. nml:member:: l_lessdecomp_sat
+
+      :type: logical
+      :default: F
+
+      Switch affecting the moisture function used for soil respiration calculation.
+
+      TRUE
+          The response of the soil carbon decomposition to soil moisture is modified using an approach similar to Equation 3 and Figure 1 in Chadburn et al. (2022). Microbial activity drops to zero in completely dry conditions. In anaerobic conditions, respiration is significantly reduced compared to the maximum rate in aerobic conditions. In Chandburn et al. (2022) the value of the respiration in anaerobic conditions is set to 20 % of the maximum rate. This is set by :nml:mem:`fsth_lessdecomp_sat`. This approach was developed for JULES-peat.
+
+      FALSE
+         The response of the soil carbon decomposition to soil moisture is calculated using Equation 67 in Clark et al. (2011).
+
+      .. seealso::
+         References:
+
+         * Chadburn, Sarah E., et al. "A new approach to simulate peat accumulation, degradation and stability in a global land surface scheme (JULES vn5. 8_accumulate_soil) for northern and temperate peatlands." Geoscientific Model Development 15.4 (2022): 1633-1657 (https://gmd.copernicus.org/articles/15/1633/2022/).
+
+         * Clark, D. B., Mercado, L. M., Sitch, S., Jones, C. D., Gedney, N., Best, M. J., Pryor, M., Rooney, G. G., Essery, R. L. H., Blyth, E., Boucher, O., Harding, R. J., Huntingford, C., and Cox, P. M.: The Joint UK Land Environment Simulator (JULES), model description – Part 2: Carbon fluxes and vegetation dynamics, Geosci. Model Dev., 4, 701–722, (https://doi.org/10.5194/gmd-4-701-2011), 2011.
+
+   .. nml:member:: fsth_lessdecomp_sat
+
+      :type: real
+      :default: 0.2
+
+      The value of the soil respiration in anaerobic conditions as a fraction of the maximum rate. Values should be between 0 and 1. Only used if :nml:mem:`l_lessdecomp_sat` = TRUE.
+
+       .. note:: In Chadburn et al. (2022) the value of this parameter is set to 0.2 but in Elise Dehaen's PhD thesis (Exeter University, 2026) a value of 0.1 was proposed for peatlands.
 
 
 .. nml:group:: Parameters for the 4-pool model (only used if :nml:mem:`soil_bgc_model` = 2)