TNO Intern

Commit 2a71c1d3 authored by Jan Diederik van Wees's avatar Jan Diederik van Wees
Browse files

doc updated and load profiel madrid cleaned

parent 2e6824e2
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@@ -28,7 +28,8 @@ For running the example, either run the batch script `batch_madrid.py` directly
IDE or use the CLI by:

```bash
geoloop batch-run `path/to/batch_madrid.json` 
cd examples/bore_field/madrid
geoloop batch-run batch_madrid.json
```

---
@@ -69,4 +70,7 @@ Other results have been visualized by running the `Plotmain` command:
Fig. 4: Timeseries plot of the circular borehole field with tilted boreholes; average borehole wall temperature and outlet temperature.
///

## References
- Wawoe, D., XX,YY, Van Wees, J.D.: A Semi-Analytical Model of the Energy Output of Curved Borehole Heat Exchangers,
  in: proceedings European Geothermal Congress. Zurich, 2025
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@@ -29,7 +29,8 @@ For running the example, either run the batch script `batch_me.py` directly from
IDE or use the CLI by:

```bash
geoloop batch-run `path/to/batch_me.json` 
cd examples/bore_field/ME_cooling
geoloop batch-run batch_me.json
```

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@@ -36,7 +36,8 @@ For running the example, either run the batch script `batch_Roermond.py` directl
IDE or use the CLI by:

```bash
geoloop batch-run `path/to/batch_Roermond.json` 
cd examples/lithology/roermond
geoloop batch-run batch_Roermond.json
```

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@@ -20,7 +20,8 @@ For running the example, either run the batch script `batch_COAX_optimization.py
IDE or use the CLI by:

```bash
geoloop batch-run `path/to/batch_COAX_optimization.json` 
cd examples/optimization
geoloop batch-run batch_COAX_optimization.json 
```

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@@ -50,7 +50,8 @@ For running the example, either run the batch script `batch_PYG_benchmark.py` di
IDE or use the CLI by:

```bash
geoloop batch-run `path/to/batch_PYG_benchmark.json` 
cd examples/benchmark/PYG_benchmark
geoloop batch-run batch_PYG_benchmark.json 
```

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@@ -72,12 +73,14 @@ agreement in the plots.

/// caption
Fig. 3: Timeseries plot of inlet ($T_{in}$), outlet ($T_{out}$) and average borehole wall temperature ($T_{b,ave}$) for the Geoloop benchmark simulations of the single U-tube borehole design.
Please note that standard g-function and geoloop outcomes are in perfect agreement.
///

![Fig. 4](images/PYG_SU_P_P_SR_ANALYTICAL_SU_A_P_SR_temperature_depth_8000.0.png)

/// caption
Fig. 4: Depth plot of inlet fluid (Pipe 0), outlet fluid (Pipe 1) and borehole wall ($T_b$) temperatures for the Geoloop benchmark simulations of the single U-tube borehole design.
Please note that resulting temperatures of standard g-function and geoloop  are in perfect agreement.
///

### Double U-tube
@@ -96,6 +99,7 @@ in the calculated temperature field inside the borehole, as shown in Fig. 5 and
/// caption
Fig. 3: Timeseries plot of inlet ($T_{in}$), outlet ($T_{out}$) and average borehole wall temperature ($T_{b,ave}$) for the 
Geoloop benchmark with pygfunction, for the double U-tube borehole design.
Please note that resulting temperatures of standard g-function and geoloop  are in perfect agreement.
///

![Fig. 4](images/PYG_DU_P_P_SR_ANALYTICAL_DU_A_P_SR_temperature_depth_8000.0.png)
@@ -114,7 +118,7 @@ g-function method (top) and by the semi-analytical Geoloop model (bottom).
///

!!! Note
    The aligned results from the benchmark simulation of the semi-analytical model in Geoloop and the standard implementation 
    The results from the benchmark simulation of the semi-analytical model in Geoloop and the standard implementation 
    of g-functions validates the semi-analytical modelling approach that allows for a depth-dependent BHE design and subsurface model.

---
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