Difference between revisions of "Aquifer properties"

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[[Africa Groundwater Atlas Home | Africa Groundwater Atlas]] >> [[Additional resources | Additional resources]] >> Aquifer Properties
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[[Africa Groundwater Atlas Home | Africa Groundwater Atlas]] >> [[Additional resources | Resource pages]] >> Aquifer Properties
  
==Aquifer properties==
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Please cite page as: Africa Groundwater Atlas. 2019. Aquifer properties. British Geological Survey. Accessed [date you accessed the information]. ''Weblink''.
  
Aquifer properties are the hydraulic characteristics of aquifers, which we use to describe the aquifer, and understand how groundwater exists and behaves in that aquifer - in other words, the hydrogeology of that aquifer. Key aquifer properties are '''permeability''' (or '''transmissivity'''); '''storage'''; and '''thickness'''.
 
  
To get reliable information on aquifer properties, aquifer testing must be carried out. Drilling and carrying out controlled '''test pumping''' of boreholes allows estimates of aquifer thickness, permeability, transmissivity and storage to be made. Without controlled test pumping, it is not possible to accurately estimate these aquifer properties.  
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  This page is still in development. Please check back soon for updates.
  
In many parts of Africa, quantitative aquifer properties data are scarce, and surrogate data and information must be used instead in order to characterise aquifers. The most commonly available hydrogeological data are geology; borehole depth; and borehole yield. These have been used to develop the [[Hydrogeology Map | hydrogeology map]] used in this Atlas.
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==Aquifer properties==
  
==Classification of aquifer properties==
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Aquifer properties are the hydraulic characteristics of aquifers, which are used to describe an aquifer and understand how groundwater in the aquifer exists and behaves. Aquifer properties are the most important way to describe the hydrogeology of an aquifer.
  
 +
Key aquifer properties are '''permeability''' (or '''transmissivity'''); '''storage'''; and '''thickness'''.
  
To produce the aquifer properties maps values of aquifer yield, storage type and saturated
+
To get reliable information on aquifer properties, aquifer testing must be carried out. Drilling and carrying out controlled '''test pumping''' of boreholes allows estimates of aquifer thickness, permeability, transmissivity and storage to be made. Without controlled test pumping, it is not possible to accurately estimate these aquifer properties.  
thickness were divided into significant ranges.
 
 
 
 
 
===Storage and Flow Type===
 
 
 
A semi-quantitative assessment of aquifer storage type can be made based on geology and inferred porosity. The main distinction is whether groundwater is stored in, and flows through, fractures in a consolidated rock; or via intergranular flow in a porous rock or sediment matrix. Storage and flow in unconsolidated sedimentary aquifers is always dominantly intergranular. Younger sedimentary rocks (e.g. Cenozoic and Mesozoic in age) tend to be more loosely consolidated, and groundwater storage and flow is often dominantly intergranular. Older sedimentary rocks tend to be well consolidated, and groundwater storage and flow is typically dominated by fracture flow. Karstic rocks are entirely dominated by rapid fracture flow. Volcanic and intrusive igneous rocks are typically dominated by fracture flow, although some intergranular flow can occur in weathered zones. In Precambrian basement, fracture flow dominates in unweathered rocks, and a mixture of fracture and intergranular flow and storage in weathered basins (MacDonald et al. 2010).
 
 
 
 
 
{| class = "wikitable"
 
|+ Aquifer Flow and Storage type
 
|Description of Flow and Storage type||Main aquifers
 
|-
 
|Intergranular
 
||Intergranular storage is highly significant. Rock porosity is generally >0.25. Intergranular flow is dominant.
 
|-
 
|Intergranular and fracture
 
||Significant intergranular storage, with mixed intergranular and fracture flow. The average porosity of rocks is approximately 0.1 – 0.25.
 
|-
 
|Fracture
 
||Predominantly fracture flow and storage, with only a minor component of intergranular storage. Average rock porosity is < 0.1.
 
|-
 
|+ Special cases
 
|Fracture (karst)
 
||Predominantly fracture flow and storage within karst rocks.
 
|-
 
|Fracture (weathered)
 
||Significant fracture flow, with some intergranular storage in weathered zones of otherwise very low porosity <0.01) rocks. All crystalline basement rocks belong to this category - i.e., most Precambrian rocks, with the exception of metasedimentary rocks that show little deformation.
 
|}
 
 
 
 
Special cases
 
 
 
 
For more information see [[Hydrogeological environments of Africa | hydrogeological environments of Africa].
 
 
 
===Yield===
 
 
 
To develop the [[Hydrogeology Map | hydrogeology map]] used in this Atlas, borehole yield data were collated for aquifers across Africa. Six yield categories were distinguished and applied to the mapped aquifers, as a proxy for aquifer productivity. The yield values refer to average yields from a single, effectively-sited and developed borehole in the relevant aquifer (MacDonald et al. 2010).
 
 
 
{| class = "wikitable"
 
|+ Aquifer Productivity
 
|Aquifer productivity||Yield range (litres/second or l/s)
 
|-
 
|Very high
 
||> 20
 
|-
 
|High
 
||5 - 20
 
|-
 
|Moderate
 
||2 - 5
 
|-
 
|Low to Moderate
 
||0.5 - 2
 
|-
 
|Low
 
||0.1 - 0.5
 
|-
 
|Very low
 
||< 0.1
 
|}
 
 
 
 
 
 
 
In general non-weathered
 
Precambrian basement is mapped to be of the lowest productivity. The more productive
 
aquifers in Africa are the Cretaceous-Tertiary sedimentary basins (Figure 4).
 
 
 
===Saturated thickness===
 
 
 
 
 
 
 
 Saturated thickness – four significant ranges of saturated thickness were mapped –
 
Table 3. Greatest saturated thickness is mapped for the major sedimentary basins of
 
Africa (e.g. the Sirte and Kufra Basins in North Africa), whilst shallow weathered
 
basement aquifers have been mapped as the thinnest aquifers (Figure 6).
 
 
 
 
Typical borehole yields for each [[Hydrogeological environments of Africa | aquifer group] were
 
 
 
 
 
namely, typical borehole
 
yields, aquifer storage type (e.g. fracture or intergranular), and saturated aquifer thickness.
 
 
 
 
 
; Citations and Links
 
 
 
 
 
MacDonald AM and Davies J. 2000. [http://nora.nerc.ac.uk/501047/ A brief review of groundwater for rural water supply in sub-Saharan Africa]. British Geological Survey Technical Report WC/00/033, 30pp.  
 
  
MacDonald AM, Bonsor HC, Ó Dochartaigh BE and Taylor RG. 2012. Quantitative maps of groundwater resources in Africa. Environmental Research Letters, 7 (2), 024009. 10.1088/1748-9326/7/2/024009
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In many parts of Africa, quantitative aquifer properties data are scarce, and surrogate data and information must be used instead in order to characterise aquifers. The most commonly available hydrogeological data are geology; borehole depth; and borehole yield. Geological and borehole yield data have been used to develop the [[Hydrogeology Map | hydrogeology map]] used in this Atlas.  
  
MacDonald AM, Ó Dochartaigh BE, Bonsor HC, Davies J and Key R. 2010. [http://nora.nerc.ac.uk/501779/ Developing quantitative aquifer maps for Africa]. British Geological Survey Internal Report IR/10/103, Nottingham, UK.
 
  
  
[[Africa Groundwater Atlas Home | Africa Groundwater Atlas]] >> [[Additional resources | Additional resources]] >> Aquifer properties
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Return to: [[Africa Groundwater Atlas Home | Africa Groundwater Atlas]] >> [[Additional resources | Resource pages]] >> Aquifer Properties
  
  
 
[[Category:Additional resources]]
 
[[Category:Additional resources]]
[[Category: Overview of Groundwater in Africa]]
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[[Category:Africa Groundwater Atlas]]

Latest revision as of 11:03, 2 July 2019

Africa Groundwater Atlas >> Resource pages >> Aquifer Properties

Please cite page as: Africa Groundwater Atlas. 2019. Aquifer properties. British Geological Survey. Accessed [date you accessed the information]. Weblink.


  This page is still in development. Please check back soon for updates.

Aquifer properties

Aquifer properties are the hydraulic characteristics of aquifers, which are used to describe an aquifer and understand how groundwater in the aquifer exists and behaves. Aquifer properties are the most important way to describe the hydrogeology of an aquifer.

Key aquifer properties are permeability (or transmissivity); storage; and thickness.

To get reliable information on aquifer properties, aquifer testing must be carried out. Drilling and carrying out controlled test pumping of boreholes allows estimates of aquifer thickness, permeability, transmissivity and storage to be made. Without controlled test pumping, it is not possible to accurately estimate these aquifer properties.

In many parts of Africa, quantitative aquifer properties data are scarce, and surrogate data and information must be used instead in order to characterise aquifers. The most commonly available hydrogeological data are geology; borehole depth; and borehole yield. Geological and borehole yield data have been used to develop the hydrogeology map used in this Atlas.


Return to: Africa Groundwater Atlas >> Resource pages >> Aquifer Properties