Index: doc/wflow_sbm.rst
===================================================================
diff -u -r811ccc8ee1bc08f6169c5fc5f1ef03fd8a5d236f -rea444fd8367f2c40011fde0b4fee26b081fa738b
--- doc/wflow_sbm.rst	(.../wflow_sbm.rst)	(revision 811ccc8ee1bc08f6169c5fc5f1ef03fd8a5d236f)
+++ doc/wflow_sbm.rst	(.../wflow_sbm.rst)	(revision ea444fd8367f2c40011fde0b4fee26b081fa738b)
@@ -6,12 +6,12 @@
 ------------
 
 The soil part of wflow\_sbm model has its roots in the
-topog\_sbm model but has had considerable chnages over time. topog\_sbm is specifically designed to similate fast
+topog\_sbm model but has had considerable chnages over time. topog\_sbm is specifically designed to simulate fast
 runoff processes in small catchments while wflow\_sbm can be applied more
 widely. The main differences are:
 
 
-+ The unsaturated zone can be split-up in defferent layers
++ The unsaturated zone can be split-up in different layers
 
 + The addition of evapotranspiration losses