diff --git a/biblio/chapters/introduction.tex b/biblio/chapters/introduction.tex
index f01062e..a7b90f8 100644
--- a/biblio/chapters/introduction.tex
+++ b/biblio/chapters/introduction.tex
@@ -11,7 +11,7 @@ of the breakwater. The simulation will be performed using the olaFlow
 \parencite{olaFlow} model in a three-dimensionnal setting.
 
 This study presents several aspects that are crucial to consider in order to
-obtain accurate results. The seastate that lead to the studied event is known
+obtain accurate results. The seastate that led to the studied event is known
 thanks to a wave buoy located in front of the breakwater \parencite{amir}.
 However, in order to input an accurate incident wave into the numerical model,
 it will be necessary to extract the incident and reflected waves from the raw
diff --git a/biblio/chapters/literature.tex b/biblio/chapters/literature.tex
index cf9ed82..9731b98 100644
--- a/biblio/chapters/literature.tex
+++ b/biblio/chapters/literature.tex
@@ -86,7 +86,7 @@ and reflected waves. This method relies on two or more gauges, using a least
 squares method. Results are very accurate in the absence of noise, but a small
 amount of error appears when noise is added.
 
-\textcite{inch2016accurate} noticed that the presence of noise lead to
+\textcite{inch2016accurate} noticed that the presence of noise led to
 overestimation of reflection coefficient. The creation of bias lookup tables is
 proposed in order to account for noise-induced error in reflection coefficient
 estimations.
@@ -487,7 +487,7 @@ the pre-transport conditions on block displacement.
 
 \textcite{kennedy2017extreme} derived new equations following the approach from
 \textcite{nandasena2011numerical} accounting for non-parallelepipedic blocks.
-The revised equations lead to a lower velocity threshold for block movement.
+The revised equations led to a lower velocity threshold for block movement.
 This highlights the importance of boulder shape in displacement considerations.
 
 \textcite{lodhi2020role} highlighted the importance of hydrodynamic pressure in