Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile
In the dryland of the Libertador General Bernardo O’Higgins Region in Chile, most farmers rely on wide and shallow hand-dug wells as their primary source of water during the dry summer. Few of these wells have sufficient yield for more than domestic use (human consumption, livestock, and i...
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| Lenguaje: | English |
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Instituto de Investigaciones Agropecuarias, INIA
2011
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oai:scielo:S0718-583920110002000122018-10-01Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, ChileRupp,David EReckmann,OscarVergara,JorgeUribe,HamilSelker,John S. Groundwater well recovery slug-test In the dryland of the Libertador General Bernardo O’Higgins Region in Chile, most farmers rely on wide and shallow hand-dug wells as their primary source of water during the dry summer. Few of these wells have sufficient yield for more than domestic use (human consumption, livestock, and irrigation of a subsistence garden). To more accurately assess available groundwater resources, saturated hydraulic conductivity (K) of aquifers in the eight counties that comprise this region’s dryland was estimated using evacuation and recovery tests in 353 hand-dug wells. K followed a log-normal distribution and ranged over nearly five orders of magnitude. County median K varied by a factor of 5 and a slight increasing K trend in the southward direction. In one northern county, less than 4% of the sites had K > 4 m d-1. In the t two southernmost counties, approximately one-quarter of the K values exceeded 4 m d-1. This is approximately the minimum K required for a typical well (1 m diameter and 3 m depth below the water table) to yield 1 L s-1 of water, which is roughly the yield required to irrigate 1 ha. Aquifers located where parent material was predominantly intrusive granite had slightly higher and statistically significant K than those formed predominantly of metamorphic and sedimentary rock. A semi-variogram of K provided weak evidence of a characteristic length scale of approximately 4 km.info:eu-repo/semantics/openAccessInstituto de Investigaciones Agropecuarias, INIAChilean journal of agricultural research v.71 n.2 20112011-06-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-58392011000200012en10.4067/S0718-58392011000200012 |
| institution |
Scielo Chile |
| collection |
Scielo Chile |
| language |
English |
| topic |
Groundwater well recovery slug-test |
| spellingShingle |
Groundwater well recovery slug-test Rupp,David E Reckmann,Oscar Vergara,Jorge Uribe,Hamil Selker,John S. Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| description |
In the dryland of the Libertador General Bernardo O’Higgins Region in Chile, most farmers rely on wide and shallow hand-dug wells as their primary source of water during the dry summer. Few of these wells have sufficient yield for more than domestic use (human consumption, livestock, and irrigation of a subsistence garden). To more accurately assess available groundwater resources, saturated hydraulic conductivity (K) of aquifers in the eight counties that comprise this region’s dryland was estimated using evacuation and recovery tests in 353 hand-dug wells. K followed a log-normal distribution and ranged over nearly five orders of magnitude. County median K varied by a factor of 5 and a slight increasing K trend in the southward direction. In one northern county, less than 4% of the sites had K > 4 m d-1. In the t two southernmost counties, approximately one-quarter of the K values exceeded 4 m d-1. This is approximately the minimum K required for a typical well (1 m diameter and 3 m depth below the water table) to yield 1 L s-1 of water, which is roughly the yield required to irrigate 1 ha. Aquifers located where parent material was predominantly intrusive granite had slightly higher and statistically significant K than those formed predominantly of metamorphic and sedimentary rock. A semi-variogram of K provided weak evidence of a characteristic length scale of approximately 4 km. |
| author |
Rupp,David E Reckmann,Oscar Vergara,Jorge Uribe,Hamil Selker,John S. |
| author_facet |
Rupp,David E Reckmann,Oscar Vergara,Jorge Uribe,Hamil Selker,John S. |
| author_sort |
Rupp,David E |
| title |
Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| title_short |
Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| title_full |
Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| title_fullStr |
Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| title_full_unstemmed |
Unconfined Aquifer Permeability near hand-dug Wells in the Coastal and Interior dryland of the Libertador General Bernardo O’Higgins Region, Chile |
| title_sort |
unconfined aquifer permeability near hand-dug wells in the coastal and interior dryland of the libertador general bernardo o’higgins region, chile |
| publisher |
Instituto de Investigaciones Agropecuarias, INIA |
| publishDate |
2011 |
| url |
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-58392011000200012 |
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