diff --git a/source/en/sdr.rst b/source/en/sdr.rst
index b8e0d0f6..f5c58b53 100644
--- a/source/en/sdr.rst
+++ b/source/en/sdr.rst
@@ -234,12 +234,12 @@ These mechanics can be captured as a linear interpolation of the difference of p
 
 Now we define the amount of sediment flux that is retained on any pixel in the flowpath using :math:`dT_i` as a weighted flow of upslope flux:
 
-.. math:: T_i=dT_i\cdot\left(\sum_{j\in\{pixels\ that\ drain\ to\ i\}}F_j \cdot p(i,j)\right)
+.. math:: T_i=dT_i\cdot\left(\sum_{j\in\{pixels\ that\ drain\ to\ i\}}F_j \cdot p(j,i)\right)
     :label: ti
 
 where :math:`F_i` is the amount of sediment export that does not reach the stream "flux", defined as:
 
-.. math:: F_i=(1-dT_i)\cdot(\left(\sum_{j\in\{pixels\ that\ drain\ to\ i\}} F_j \cdot p(i,j)\right) + E'_i)
+.. math:: F_i=(1-dT_i)\cdot(\left(\sum_{j\in\{pixels\ that\ drain\ to\ i\}} F_j \cdot p(j,i)\right) + E'_i)
     :label: fi
 
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