## Examples of the withsol Operator

The *withsol* operator allows you to extract the solution from any solver sequence in the current model and use it in other studies, or during postprocessing.

### Comparing the Results Between Two Studies

Let us consider a simple thermal example. A steady-state simulation of a square with a temperature of 20ºC on the left-hand side. We run two studies in the model. One where the temperature on the right-hand side is 100ºC (*Study 1*) and one where the temperature is 200ºC (*Study 2*). To evaluate the temperature difference between the two studies, we can use the *withsol* operator.

The basic form of the *withsol* operator is: `withsol('tag',expr)`

, where `'tag'`

is the tag of the solver sequence we want to extract the solution from, and `expr`

is the expression we want to evaluate. To be able to see the tag, make sure that *tag* is selected from the *Model Tree Node Text* menu at the top of the *Model Builder* window. The tag for each node appears in curly brackets {} after the node name.

*The* Model Tree Node Text *menu, with the* Name *and* Tag *options enabled.*

To see the difference between the temperatures in *Study 2* and *Study 1*, we create a plot for the Study 2 dataset, and use the expression `T-withsol('sol1',T)`

.

*A screenshot of the model tree, with the Solution 1 and Surface 1 nodes highlighted, and the Surface Settings window with the withsol Expression highlighted.*

*The operator used in the expression for a*Surface

*plot node, which defines the temperature difference between the solution from the second study and solution from the first study.*

In this expression, the variable

*T*outside of the

*withsol*operator is taken from

*Study 2*(with the tag

`'sol2'`

), whereas the *withsol*operator picks up the temperature from

*Study 1*, which has the tag

`'sol1'`

. The resulting plot shows the temperature difference across the domain, with the difference being 0 at the end where the temperature is the same in both studies.*A screenshot of the Surface Settings window on the left and the Graphics window with a temperature plot on the right.*

*The settings for one of the*Surface

*plot nodes, wherein the operator and utilized, and the resulting plot in the*Graphics

*window.*

### Comparing the Results Between Two Parameter Values in the Same Study

It is also possible to compare results between two parameters in the same study or between two times in a transient study. If we, instead of using two studies in our example, use only one study with a parameterized temperature on the right-hand side, we can similarly find the difference between the two temperatures. However, we need to use an expanded version of the *withsol* operator to not only specify which solution we want to extract results from, but also which parameter value. This time, the operator will look like this:

`withsol('tag',expr, setval(par,value))`

Here, `'tag'`

, and `expr`

are the same as before. What is new is `setval(par,value)`

. The operator *setval* is an operator commonly used together with *withsol* to specify which value the parameter `par`

should have.

*A screenshot of the model tree on the left, with the Solution and Surface nodes selected, and the Surface Settings window on the right, with the Expression highlighted and including the withsol and setval operators.*

*The*Settings

*window for one of the*Surface

*plot nodes, wherein the*withsol

*and*setval

*operators are used in the expression. The solution for*Study 3

*is included in the expression and is highlighted in the*Model Builder

*window.*

Here, *T* is taken from the setting for our plot, so *Study 3* and a parameter value of 200ºC. The *withsol* operator picks up the values of the variable *T* from the same study (with the tag `'sol3'`

), but when the parameter *Temp* is 100ºC. This is done by setting the value of the parameter *Temp* to '100[degC]' with the *setval* operator. This plot gives the same result as the plot above.

Please note that while this can be accomplished with the expanded use of the *withsol* operator outlined above, there are other more efficient options also available. When comparing results inside the same solution, the at operator using the expression `at(`

and with operator using the expression `with(`

are preferred. Since they don’t need to map solutions from one solution/xmesh to another and just read from another position in the same solution, this method can be expected to be faster. Additionally, the syntax involved is simplified since you don't need to know the solution tag and don't need to use the *setval* operator.

### Using Results from One Study as Input in Another

In the model Slope Stability in an Embankment Dam, the *in situ* stresses from pore pressure and gravity are calculated, and the results from that study are used as an initial stress for the safety factor calculation. The *in situ* stresses are accessed using the *withsol* operator.

*A screenshot of the model tree and Settings window for the Initial Stress and Strain feature.*

*The*Settings

*window for the*Initial Stress and Strain

*feature, wherein the*withsol

*operator is used.*

It is additionally possible to use the *setind* and *setval* operators as additional arguments to the *withsol* operator. These operators work with results from a time-dependent solver, an eigenvalue solver, a frequency sweep, or an Auxiliary sweep over one or more more parameters.

The *setind* operator indexes into the time-domain solution, or the index of the list of eigenvalues, or the index into a sweep over frequency or any other parameter. Positive indices start from the beginning, and negative from the end of the list.

For example, when working with time-domain solutions:

`withsol('sol1',expr,setind(t,1))`

will return the first timestep. Alternatively, use `withsol('sol1',expr,setind(t,'first'))`

`withsol('sol1',expr,setind(t,2))`

will return the second timestep.

`withsol('sol1',expr,setind(t,-2))`

will return the second-to-last timestep.

`withsol('sol1',expr,setind(t,-1))`

will return the last timestep. Alternatively, use `withsol('sol1',expr,setind(t,'last'))`

For eigenvalue solutions, the index variable is `lambda`

, and for frequency sweep the frequency variable is `freq`

.

The *setval* operator instead extracts the solution at a user-specified value, and interpolates between stored time-domain solutions. For example:

`withsol('sol1',expr,setval(t,0.5))`

will return the solution at time of 0.5 seconds. If there is no stored data at this timestep, then a solution is interpolated from the nearest stored timesteps. This interpolation will make usage of the time derivatives, if they are stored as shown in the screenshot below of the *Time-Dependent Solver*. A Hermite interpolation is used if time derivatives are available, otherwise linear interpolation is used. If a value outside of the time range is specified then the nearest timestep (first or last) is used.

*Within the* Time-Dependent Solver *settings, the default option is to store time derivatives.*

When used in conjunction with eigenvalue solutions, the setval operator will return a solution that is within a tolerance of the actual eigenvalue. For example:

`withsol('sol1',expr, setval(lambda,-100i))`

will return the solution even if the eigenvalue is actually -100.01i.

When used with a frequency sweep or auxiliary sweep, the exact numeric value of the frequency or parameter must be specified. If sweeping over multiple frequencies and/or parameters, it is possible to pass multiple arguments to setval, as well as setind, to make the syntax more compact. For example:

`withsol('sol1',expr, setval(freq,60,param,5))`

is equivalent to `withsol('sol1',expr, setval(freq,60),setval(param,5))`

.

### More Advanced Usage of the withsol Operator

For an example of more advanced usage of the *withsol* operator, see the model Bracket - General Periodic Dynamic Analysis. You can find it among the tutorials for the Structural Mechanics Module in the Application Library in the following files:

- bracket_general_periodic.mph
- models.sme.bracket_general_periodic.pdf

In that model, the *withsol* operator is used to extract frequency-dependent loads from one study and use them as input for the corresponding frequencies in a second study.

请提交与此页面相关的反馈，或点击此处联系技术支持。