OR/15/002 Appendix 3: Tables for vulnerability classification: Difference between revisions
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These tables are used, with the rules in Section 3, to define the assigned vulnerability class for each given combination of input parameters. They have been slightly modified from the tables used to derive Version 1 of the groundwater vulnerability dataset (Ball et al. 2004), as follows: | These tables are used, with the rules in Section 3, to define the assigned vulnerability class for each given combination of input parameters. They have been slightly modified from the tables used to derive Version 1 of the groundwater vulnerability dataset (Ball et al. 2004<ref>Ball D, MacDonald A, Ó Dochartaigh B, del Rio M, FitzSimons V, Auton C and Lilly A. 2004. Development of a groundwater vulnerability screening methodology for the Water Framework Directive. SNIFFER Report Project WFD28 / BGS Commissioned Report CR/03/294C. </ref>), as follows: | ||
* Vulnerability Class 4 has been subdivided throughout into two sub-classes, Class 4a and Class 4b. Class 4a includes areas where superficial deposits have low permeability; Class 4b includes areas where superficial deposits have moderate or high permeability. The tables have been amended to reflect this. | * Vulnerability Class 4 has been subdivided throughout into two sub-classes, Class 4a and Class 4b. Class 4a includes areas where superficial deposits have low permeability; Class 4b includes areas where superficial deposits have moderate or high permeability. The tables have been amended to reflect this. | ||
* Because of this change, one table (the original Table 2) has been removed as no longer needed. | * Because of this change, one table (the original Table 2) has been removed as no longer needed. | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A3 Bedrock Flow Type = Fractured; superficial deposits are mapped, Clay Thickness <5m (Rule 2). | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Superficial deposits thickness (m)''' | | colspan="4" | '''Superficial deposits thickness (m)''' | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A4 Bedrock Flow Type = Fractured; superficial deposits are mapped; Clay Thickness => 5 m (Rule 2) | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Superficial deposits thickness (m)''' | | colspan="4" | '''Superficial deposits thickness (m)''' | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A5 Superficial Deposits Permeability at surface = High or Very High; there is a water table in superficial deposits (Superficial Deposits Thickness > Depth to Water in Superficial Deposits) (Rule 1). | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Depth to Water in Superficial Deposits (m)''' | | colspan="4" | '''Depth to Water in Superficial Deposits (m)''' | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A6 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); no soil or superficial deposits (Rule 6) | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Depth to Water in Bedrock (m)''' | | colspan="4" | '''Depth to Water in Bedrock (m)''' | ||
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| rowspan="3" | '''Bedrock permeability''' | | rowspan="3" | '''Bedrock permeability''' | ||
| width="100pt" | <p align="center">VH or H</p> | | width="100pt" | <p align="center">VH or H</p> | ||
| style="background-color:#fd0e35" |<p align="center">'''5'''</p> | | style="background-color:#fd0e35" | <p align="center">'''5'''</p> | ||
| style="background-color:#fd0e35" |<p align="center">'''5'''</p> | | style="background-color:#fd0e35" | <p align="center">'''5'''</p> | ||
| style="background-color:#ffb300" | <p align="center">'''4a'''</p> | | style="background-color:#ffb300" | <p align="center">'''4a'''</p> | ||
| style="background-color:#9acd32<p align="center">'''3'''</p> | | style="background-color:#9acd32" | <p align="center">'''3'''</p> | ||
|- | |- | ||
| <p align="center">M</p> | | <p align="center">M</p> | ||
| style="background-color:#fd0e35" |<p align="center">'''5'''</p> | | style="background-color:#fd0e35" | <p align="center">'''5'''</p> | ||
| style="background-color:#ffb300" | <p align="center">'''4a'''</p> | | style="background-color:#ffb300" | <p align="center">'''4a'''</p> | ||
| style="background-color:#9acd32<p align="center">'''3'''</p> | | style="background-color:#9acd32" | <p align="center">'''3'''</p> | ||
| style="background-color:#9acd32<p align="center">'''3'''</p> | | style="background-color:#9acd32" | <p align="center">'''3'''</p> | ||
|- | |- | ||
| <p align="center">L</p> | | <p align="center">L</p> | ||
| style="background-color:#fd0e35" |<p align="center">'''5'''</p> | | style="background-color:#fd0e35" | <p align="center">'''5'''</p> | ||
| style="background-color:#ffb300" | <p align="center">'''4a'''</p> | | style="background-color:#ffb300" | <p align="center">'''4a'''</p> | ||
| style="background-color:#9acd32<p align="center">'''3'''</p> | | style="background-color:#9acd32" | <p align="center">'''3'''</p> | ||
| style="background-color:#9acd32<p align="center">'''3'''</p> | | style="background-color:#9acd32" | <p align="center">'''3'''</p> | ||
|} | |} | ||
{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A7 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); no superficial deposits; high or moderate soils (HOST classes in Group B – see Rule 7). | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Depth to Water in Bedrock (m)''' | | colspan="4" | '''Depth to Water in Bedrock (m)''' | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A8 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); no superficial deposits; low permeability soils (HOST classes in Group A – see Rule 7) | ||
| rowspan="2" colspan="2" | | | rowspan="2" colspan="2" | | ||
| colspan="4" | '''Depth to Water in Bedrock (m)''' | | colspan="4" | '''Depth to Water in Bedrock (m)''' | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A9 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); Superficial Deposits Permeability at surface = Very High or High (Rule 5). | ||
| rowspan="2" | <p align="center">'''Depth to Water<br>in Bedrock (m)'''</p> | | rowspan="2" | <p align="center">'''Depth to Water<br>in Bedrock (m)'''</p> | ||
| rowspan="2" | <p align="center">'''Bedrock<br>permeability'''</p> | | rowspan="2" | <p align="center">'''Bedrock<br>permeability'''</p> | ||
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| width="100pt" | <p align="center">'''10-30'''</p> | | width="100pt" | <p align="center">'''10-30'''</p> | ||
| width="100pt" | <p align="center">'''>30'''</p> | | width="100pt" | <p align="center">'''>30'''</p> | ||
| width="100pt" | <p align="center">=>5m clay<br>in sequence'''</p> | | width="100pt" | <p align="center">'''=>5m clay<br>in sequence'''</p> | ||
|- | |- | ||
| rowspan="3" | <p align="center"><10 m'''</p> | | rowspan="3" | <p align="center">'''<10 m'''</p> | ||
| <p align="center">VH or H</p> | | <p align="center">VH or H</p> | ||
| style="background-color:#ffb300" | <p align="center">'''4a'''</p> | | style="background-color:#ffb300" | <p align="center">'''4a'''</p> | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A10 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); Superficial Deposits Permeability at surface = Moderate (Rule 5) | ||
| rowspan="2" | <p align="center">'''Depth to Water in Bedrock (m)'''</p> | | rowspan="2" | <p align="center">'''Depth to Water in Bedrock (m)'''</p> | ||
| rowspan="2" | <p align="center">''' | | rowspan="2" | <p align="center">'''BedrocK<br>permeability'''</p> | ||
| colspan="5" | <p align="center">'''Moderate permeability superficial deposits thickness (m)'''</p> | | colspan="5" | <p align="center">'''Moderate permeability superficial deposits thickness (m)'''</p> | ||
|- | |- | ||
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| width="100pt" | <p align="center">'''=>5m clay<br>in sequence'''</p> | | width="100pt" | <p align="center">'''=>5m clay<br>in sequence'''</p> | ||
|- | |- | ||
| rowspan="3" | | rowspan="3" width="100pt" | <p align="center">'''<10 m'''</p> | ||
| <p align="center">VH or H</p> | | <p align="center">VH or H</p> | ||
| style="background-color:#ffb300" | <p align="center">'''4a'''</p> | | style="background-color:#ffb300" | <p align="center">'''4a'''</p> | ||
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{| class="wikitable" | {| class="wikitable" | ||
| | |+ Table A11 Bedrock Flow Type = Significantly Intergranular (including mixed fracture/intergranular); Superficial Deposits Permeability at surface = Low (Rule 5) | ||
| rowspan="2" | <p align="center">'''Depth to Water<br>in Bedrock (m)'''</p> | | rowspan="2" | <p align="center">'''Depth to Water<br>in Bedrock (m)'''</p> | ||
| rowspan="2" | <p align="center">'''Bedrock | | rowspan="2" | <p align="center">'''Bedrock permeability'''</p> | ||
| colspan="5" | <p align="center">'''Low permeability superficial deposits thickness (m)'''</p> | | colspan="5" | <p align="center">'''Low permeability superficial deposits thickness (m)'''</p> | ||
|- | |- | ||
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| width="100pt" | <p align="center">'''=>5m clay<br>in sequence'''</p> | | width="100pt" | <p align="center">'''=>5m clay<br>in sequence'''</p> | ||
|- | |- | ||
| rowspan="3" | p align="center">'''<10 m'''</p> | | rowspan="3" | <p align="center">'''<10 m'''</p> | ||
| <p align="center">VH or H</p> | | <p align="center">VH or H</p> | ||
| style="background-color:#ffff66" | <p align="center">'''4b'''</p> | | style="background-color:#ffff66" | <p align="center">'''4b'''</p> | ||
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|} | |} | ||
==Reference== | |||
[[category:OR/15/002 User Guide: Groundwater Vulnerability (Scotland) GIS dataset, Version 2. Revised Report | 09]] | [[category:OR/15/002 User Guide: Groundwater Vulnerability (Scotland) GIS dataset, Version 2. Revised Report | 09]] |
Latest revision as of 15:06, 23 July 2015
Ó Dochartaigh B É,Doce D D, Rutter H K and MacDonald A M. 2015. User Guide: Groundwater Vulnerability (Scotland) GIS dataset, Version 2. Revised Report. British Geological Survey Internal Report, OR/15/002. |
These tables are used, with the rules in Section 3, to define the assigned vulnerability class for each given combination of input parameters. They have been slightly modified from the tables used to derive Version 1 of the groundwater vulnerability dataset (Ball et al. 2004[1]), as follows:
- Vulnerability Class 4 has been subdivided throughout into two sub-classes, Class 4a and Class 4b. Class 4a includes areas where superficial deposits have low permeability; Class 4b includes areas where superficial deposits have moderate or high permeability. The tables have been amended to reflect this.
- Because of this change, one table (the original Table 2) has been removed as no longer needed.
The following abbreviations and legend are used in the tables:
- VH = Very High permeability
- H = High permeability
- M = Moderate permeability
- L = Low permeability
- n/a = not applicable
Highest ......................................................................................................................................Lowest | |||||
5 |
4a |
4b |
3 |
2 |
1 |
Fractured bedrock, no soil or superficial deposits | |
Fractured bedrock, no soil or superficial deposits |
5 |
Superficial deposits thickness (m) | ||
<1 | ||
Soil permeability | H |
5 |
M |
5 | |
L |
4a |
Superficial deposits thickness (m) | |||||
1-3 |
3-10 |
10-30 |
> 30 | ||
Superficial deposits |
VH or H |
4a |
4a |
3 |
2 |
M |
4a |
3 |
2 |
1 | |
L |
4b |
2 |
1 |
1 |
Superficial deposits thickness (m) | |||||
<3 |
3-10 |
10-30 |
> 30 | ||
Superficial deposits |
VH or H |
n/a |
1 |
1 |
1 |
M |
n/a |
1 |
1 |
1 | |
L |
n/a |
1 |
1 |
1 |
Depth to Water in Superficial Deposits (m) | |||||
<3 |
3-10 |
10-30 |
> 30 | ||
Superficial deposits |
VH or H | 4a |
4a |
3 |
2 |
Depth to Water in Bedrock (m) | |||||
0-3 |
3-10 |
10-30 |
30+ | ||
Bedrock permeability | VH or H |
5 |
5 |
4a |
3 |
M |
5 |
4a |
3 |
3 | |
L |
5 |
4a |
3 |
3 |
Depth to Water in Bedrock (m) | |||||
0-3 |
3-10 |
10-30 |
30+ | ||
Bedrock permeability | VH or H |
5 |
5 |
4a |
3 |
M |
5 |
4a |
3 |
3 | |
L |
5 |
4a |
3 |
3 |
Depth to Water in Bedrock (m) | |||||
0-3 |
3-10 |
10-30 |
30+ | ||
Bedrock permeability | VH or H |
4a |
4a |
3 |
3 |
M |
4a |
3 |
3 |
3 | |
L |
4a |
3 |
3 |
3 |
Depth to Water |
Bedrock |
High permeability superficial deposits thickness (m) | ||||
<3 |
3-10 |
10-30 |
>30 |
=>5m clay | ||
<10 m |
VH or H |
4a |
4a |
3 |
2 |
1 |
M |
4a |
3 |
3 |
2 |
1 | |
L |
4a |
3 |
2 |
2 |
1 | |
10-30 m |
VH or H |
4a |
3 |
3 |
2 |
1 |
M |
3 |
2 |
2 |
2 |
1 | |
L |
3 |
2 |
2 |
1 |
1 | |
>30 m |
VH or H |
3 |
3 |
2 |
2 |
1 |
M |
3 |
2 |
2 |
1 |
1 | |
L |
3 |
2 |
1 |
1 |
1 |
Depth to Water in Bedrock (m) |
BedrocK |
Moderate permeability superficial deposits thickness (m) | ||||
<3 |
3-10 |
10-30 |
>30 |
=>5m clay | ||
<10 m |
VH or H |
4a |
3 |
2 |
2 |
1 |
M |
4a |
3 |
2 |
2 |
1 | |
L |
3 |
2 |
2 |
1 |
1 | |
10-30 m |
VH or H |
4a |
3 |
2 |
2 |
1 |
M |
3 |
2 |
2 |
2 |
1 | |
L |
3 |
2 |
1 |
1 |
1 | |
>30 m |
VH or H |
3 |
2 |
2 |
2 |
1 |
M |
3 |
2 |
2 |
1 |
1 | |
L |
3 |
1 |
1 |
1 |
1 |
Depth to Water |
Bedrock permeability |
Low permeability superficial deposits thickness (m) | ||||
<3 |
3-10 |
10-30 |
>30 |
=>5m clay | ||
<10 m |
VH or H |
4b |
2 |
1 |
1 |
1 |
M |
4b |
2 |
1 |
1 |
1 | |
L |
3 |
2 |
1 |
1 |
1 | |
10-30 m |
VH or H |
3 |
2 |
1 |
1 |
1 |
M |
3 |
2 |
1 |
1 |
1 | |
L |
3 |
1 |
1 |
1 |
1 | |
>30 m |
VH or H |
3 |
2 |
1 |
1 |
1 |
M |
3 |
1 |
1 |
1 |
1 | |
L |
3 |
1 |
1 |
1 |
1 |
Reference
- ↑ Ball D, MacDonald A, Ó Dochartaigh B, del Rio M, FitzSimons V, Auton C and Lilly A. 2004. Development of a groundwater vulnerability screening methodology for the Water Framework Directive. SNIFFER Report Project WFD28 / BGS Commissioned Report CR/03/294C.