DOC: FindSlipTransmissionMetrics and FindBoundaryStrengths updated wi…

…th citations

Signed-off-by: Michael Jackson <[email protected]>

Source/Plugins/OrientationAnalysis/Documentation/OrientationAnalysisFilters/FindBoundaryStrengths.md

@@ -1,12 +1,13 @@
 # Find Feature Boundary Strength Metrics  #
 
-
 ## Group (Subgroup) ##
 
 Statistics (Crystallographic)
 
 ## Description ##
 
+**THIS FILTER ONLY WORKS ON Cubic m-3m LAUE CLASSES**
+
 This **Filter** calculates the same metrics as in the [Find Neighbor Slip Transmission Metrics](FindSlipTransmissionMetrics.html "") **Filter**.  However, this **Filter** stores the values in the **Face Attribute Matrix** of a **Triangle Geometry**.  The algorithm the **Filter** uses is as follows:
 
 1. Find the two **Features** that are separated by a **Face** in the **Triangle Geometry**
@@ -15,7 +16,28 @@ This **Filter** calculates the same metrics as in the [Find Neighbor Slip Transm
 4. Store the metrics in the **Face** map
 5. Repeat for all **Faces**
 
-*Note:* Each metric is calculated twice for the two different directions slip could approach the boundary.  The values are stored on each **Face** in the **Face** map in a way that notes the direction (i.e., when **Feature** 1 has neighbor **Feature** 2 and when **Feature** 2 has neighbor **Feature** 1) because the direction across the boundary between the **Features** affects the value of the metric. 
+*Note:* Each metric is calculated twice for the two different directions slip could approach the boundary.  The values are stored on each **Face** in the **Face** map in a way that notes the direction (i.e., when **Feature** 1 has neighbor **Feature** 2 and when **Feature** 2 has neighbor **Feature** 1) because the direction across the boundary between the **Features** affects the value of the metric.
+
+## Luster-Morris Parameter (M' Values)
+
+The values are calculated as presented in [1].
+
+## Fracture Initiation Parameter (fip)
+
+Three (3) *fip* values are computed as outputs to this filter. These are best explained in [2], see page 021012-4
+
+![Fracture Initiation Parameter F1](Images/ComputeNeighborSlipTransmission_F1.png)
+
+![Fracture Initiation Parameter F1spt](Images/ComputeNeighborSlipTransmission_F1spt.png)
+
+![Fracture Initiation Parameter F7.png](Images/ComputeNeighborSlipTransmission_F7.png)
+
+
+## Citations
+
+[1] [Luster, J., Morris, M.A., 1995. *Compatibility Of Deformation In Two-Phase Ti-Al Alloys: Dependence On Microstructure And Orientation Relationships*. **Metallurgical and Materials Transactions A 26, 1745**](https://link.springer.com/article/10.1007/BF02670762)
+
+[2] [D. Kumar, T. R. Bieler, P. Eisenlohr, D. E. Mason, M. A. Crimp, F. Roters, and D. Raabe. On Predicting Nucleation of Microcracks Due to Slip Twin Interactions at Grain Boundaries in Duplex Near γ-TiAl. Journal of Engineering Materials and Technology, 130(2):021012–12, 2008. doi:10.1115/1.2841620.](https://doi.org/10.1115/1.2841620)
 
 ## Parameters ##
 

Source/Plugins/OrientationAnalysis/Documentation/OrientationAnalysisFilters/FindSlipTransmissionMetrics.md

@@ -1,13 +1,14 @@
 # Find Neighbor Slip Transmission Metrics  #
 
-
-## Group (Subgroup) ##
+## Group (Subgroup)
 
 Statistics (Crystallographic)
 
-## Description ##
+## Description
+
+**THIS FILTER ONLY WORKS ON Cubic m-3m LAUE CLASSES**
 
-This **Filter** calculates a suite of *slip transmission metrics* that are related to the alignment of slip directions and planes across **Feature** boundaries.  The algorithm for calculation of these metrics is as follows:
+This **Filter** calculates a suite of *slip transmission metrics* that are related to the alignment of slip directions and planes across **Feature** boundaries. The algorithm for calculation of these metrics is as follows:
 
 1. Get the average orientation of the **Feature**
 2. Get the **Feature**'s list of neighboring **Features**
@@ -16,8 +17,28 @@ This **Filter** calculates a suite of *slip transmission metrics* that are relat
 5. Store metrics in lists for the **Feature**
 6. Repeat for all **Features**
 
-*Note:* The transmission metrics are calculated using the average orientations for neighboring **Features** and not the local orientation near the boundary. Also, the metrics are calculated twice (i.e., when **Feature** 1 has neighbor **Feature** 2 and when **Feature** 2 has neighbor **Feature** 1) because the direction across the boundary between the **Features** affects the value of the metric. 
-
+*Note:* The transmission metrics are calculated using the average orientations for neighboring **Features** and not the local orientation near the boundary. Also, the metrics are calculated twice (i.e., when **Feature** 1 has neighbor **Feature** 2 and when **Feature** 2 has neighbor **Feature** 1) because the direction across the boundary between the **Features** affects the value of the metric.
+
+## Luster-Morris Parameter (M' Values)
+
+The values are calculated as presented in [1].
+
+## Fracture Initiation Parameter (fip)
+
+Three (3) *fip* values are computed as outputs to this filter. These are best explained in [2], see page 021012-4
+
+![Fracture Initiation Parameter F1](Images/ComputeNeighborSlipTransmission_F1.png)
+
+![Fracture Initiation Parameter F1spt](Images/ComputeNeighborSlipTransmission_F1spt.png)
+
+![Fracture Initiation Parameter F7.png](Images/ComputeNeighborSlipTransmission_F7.png)
+
+
+## Citations
+
+[1] [Luster, J., Morris, M.A., 1995. *Compatibility Of Deformation In Two-Phase Ti-Al Alloys: Dependence On Microstructure And Orientation Relationships*. **Metallurgical and Materials Transactions A 26, 1745**](https://link.springer.com/article/10.1007/BF02670762)
+
+[2] [D. Kumar, T. R. Bieler, P. Eisenlohr, D. E. Mason, M. A. Crimp, F. Roters, and D. Raabe. On Predicting Nucleation of Microcracks Due to Slip Twin Interactions at Grain Boundaries in Duplex Near γ-TiAl. Journal of Engineering Materials and Technology, 130(2):021012–12, 2008. doi:10.1115/1.2841620.](https://doi.org/10.1115/1.2841620)
 ## Parameters ##
 
 None