Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)

<p>The geothermal reservoir at Waiwera has been subject to active exploitation for a long time. It is located below the village on the Northern Island of New Zealand and has been used commercially since 1863. The continuous production of geothermal water, to supply hotels and spas, had a negat...

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Autores principales: M. Kühn, L. Grabow
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Publicado: Copernicus Publications 2021
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spelling oai:doaj.org-article:7e435017dc7b446f91a930b7d07ade0b2021-11-12T07:12:29ZDeconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)10.5194/adgeo-56-107-20211680-73401680-7359https://doaj.org/article/7e435017dc7b446f91a930b7d07ade0b2021-11-01T00:00:00Zhttps://adgeo.copernicus.org/articles/56/107/2021/adgeo-56-107-2021.pdfhttps://doaj.org/toc/1680-7340https://doaj.org/toc/1680-7359<p>The geothermal reservoir at Waiwera has been subject to active exploitation for a long time. It is located below the village on the Northern Island of New Zealand and has been used commercially since 1863. The continuous production of geothermal water, to supply hotels and spas, had a negative impact on the reservoir. So far, the physical relation between abstraction rates and water level change of the hydrogeological system is only fairly understood. The aim of this work was to link the influence of rates to the measured data to derive reservoir properties. For this purpose, the daily abstraction history was investigated by means of a variable production rate well test analysis. For the analysis, a modified deconvolution algorithm was implemented. The algorithm derives the reservoir response function by solving a least square problem with the unique feature of imposing only implicit constraints on the solution space. To further investigate the theoretical performance of the algorithm a simulation with synthetic data was conducted for three possible reservoir scenarios. Results throughout all years indicate radial flow during middle-time behaviour and a leaky flow boundary during late-time behaviour. For middle-time behaviour, the findings agree very well with prior results of a pumping test. For the future, a more extensive investigation of different flow conditions under different parametrisations should be conducted.</p>M. KühnM. KühnL. GrabowL. GrabowL. GrabowCopernicus PublicationsarticleScienceQGeologyQE1-996.5Dynamic and structural geologyQE500-639.5ENAdvances in Geosciences, Vol 56, Pp 107-116 (2021)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
Geology
QE1-996.5
Dynamic and structural geology
QE500-639.5
spellingShingle Science
Q
Geology
QE1-996.5
Dynamic and structural geology
QE500-639.5
M. Kühn
M. Kühn
L. Grabow
L. Grabow
L. Grabow
Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
description <p>The geothermal reservoir at Waiwera has been subject to active exploitation for a long time. It is located below the village on the Northern Island of New Zealand and has been used commercially since 1863. The continuous production of geothermal water, to supply hotels and spas, had a negative impact on the reservoir. So far, the physical relation between abstraction rates and water level change of the hydrogeological system is only fairly understood. The aim of this work was to link the influence of rates to the measured data to derive reservoir properties. For this purpose, the daily abstraction history was investigated by means of a variable production rate well test analysis. For the analysis, a modified deconvolution algorithm was implemented. The algorithm derives the reservoir response function by solving a least square problem with the unique feature of imposing only implicit constraints on the solution space. To further investigate the theoretical performance of the algorithm a simulation with synthetic data was conducted for three possible reservoir scenarios. Results throughout all years indicate radial flow during middle-time behaviour and a leaky flow boundary during late-time behaviour. For middle-time behaviour, the findings agree very well with prior results of a pumping test. For the future, a more extensive investigation of different flow conditions under different parametrisations should be conducted.</p>
format article
author M. Kühn
M. Kühn
L. Grabow
L. Grabow
L. Grabow
author_facet M. Kühn
M. Kühn
L. Grabow
L. Grabow
L. Grabow
author_sort M. Kühn
title Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
title_short Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
title_full Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
title_fullStr Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
title_full_unstemmed Deconvolution well test analysis applied to a long-term data set of the Waiwera geothermal reservoir (New Zealand)
title_sort deconvolution well test analysis applied to a long-term data set of the waiwera geothermal reservoir (new zealand)
publisher Copernicus Publications
publishDate 2021
url https://doaj.org/article/7e435017dc7b446f91a930b7d07ade0b
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