Serveur d'exploration sur les relations entre la France et l'Australie

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Interrelationships between biological, chemical, and physical processes as an analog to clogging in aquifer storage and recovery (ASR) wells

Identifieur interne : 00BE96 ( Main/Curation ); précédent : 00BE95; suivant : 00BE97

Interrelationships between biological, chemical, and physical processes as an analog to clogging in aquifer storage and recovery (ASR) wells

Auteurs : Stéphanie Rinck-Pfeiffer [Australie] ; Santo Ragusa [Australie] ; Pascale Sztajnbok [Australie] ; Thierry Vandevelde [France]

Source :

RBID : ISTEX:FA4EE358E9D978E5BAE0F52FF947E8149408F581

Descripteurs français

English descriptors

Abstract

Abstract: Laboratory columns were used to understand and predict bore clogging issues at a South Australian recycled water aquifer storage and recovery site, before field trials proceeded. The columns were used to study biogeochemical processes resulting from the continuous injection of recycled water into an aquifer matrix. The results showed that despite levels of suspended solids (SS) between 3–4 mg/l in the influent, flow rates (hydraulic conductivities) were maintained at 20–50% of initial flow through three identical columns for a period of 22 days. An initial decline in the hydraulic conductivity (K) through the columns was evident early in the experiment, and decreased from 0.78 m/day to 0.062 m/day in the first 7 days of the experiment. This was thought to be due to physical clogging by suspended solids and then biological clogging by biomass accumulation and polysaccharide production at the inflow end of the columns. The physical bioclogging was relieved midway through the experiment due to calcite dissolution mainly at the inlet end of the columns. Calcite reprecipitation at the outflow end of the columns was evident from SEM micrographs.

Url:
DOI: 10.1016/S0043-1354(99)00356-5

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ISTEX:FA4EE358E9D978E5BAE0F52FF947E8149408F581

Le document en format XML

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<div type="abstract" xml:lang="en">Abstract: Laboratory columns were used to understand and predict bore clogging issues at a South Australian recycled water aquifer storage and recovery site, before field trials proceeded. The columns were used to study biogeochemical processes resulting from the continuous injection of recycled water into an aquifer matrix. The results showed that despite levels of suspended solids (SS) between 3–4 mg/l in the influent, flow rates (hydraulic conductivities) were maintained at 20–50% of initial flow through three identical columns for a period of 22 days. An initial decline in the hydraulic conductivity (K) through the columns was evident early in the experiment, and decreased from 0.78 m/day to 0.062 m/day in the first 7 days of the experiment. This was thought to be due to physical clogging by suspended solids and then biological clogging by biomass accumulation and polysaccharide production at the inflow end of the columns. The physical bioclogging was relieved midway through the experiment due to calcite dissolution mainly at the inlet end of the columns. Calcite reprecipitation at the outflow end of the columns was evident from SEM micrographs.</div>
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<title level="a">Interrelationships between biological, chemical, and physical processes as an analog to clogging in aquifer storage and recovery (ASR) wells</title>
<author>
<name sortKey="Rinck Pfeiffer, Stephanie" sort="Rinck Pfeiffer, Stephanie" uniqKey="Rinck Pfeiffer S" first="Stéphanie" last="Rinck-Pfeiffer">Stéphanie Rinck-Pfeiffer</name>
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<country xml:lang="fr">Australie</country>
<wicri:regionArea>VIVENDI-Générale des Eaux, Private Bag 2, Glen Osmond, 5064</wicri:regionArea>
<wicri:noRegion>5064</wicri:noRegion>
</affiliation>
<affiliation></affiliation>
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</author>
<author>
<name sortKey="Ragusa, Santo" sort="Ragusa, Santo" uniqKey="Ragusa S" first="Santo" last="Ragusa">Santo Ragusa</name>
<affiliation wicri:level="1">
<country xml:lang="fr">Australie</country>
<wicri:regionArea>CSIRO Land & Water, Private Bag 2, Glen Osmond, 5064</wicri:regionArea>
<wicri:noRegion>5064</wicri:noRegion>
</affiliation>
</author>
<author>
<name sortKey="Sztajnbok, Pascale" sort="Sztajnbok, Pascale" uniqKey="Sztajnbok P" first="Pascale" last="Sztajnbok">Pascale Sztajnbok</name>
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<country xml:lang="fr">Australie</country>
<wicri:regionArea>United Water, 180 Greenhill Road, Parkside, 5063</wicri:regionArea>
<wicri:noRegion>5063</wicri:noRegion>
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</author>
<author>
<name sortKey="Vandevelde, Thierry" sort="Vandevelde, Thierry" uniqKey="Vandevelde T" first="Thierry" last="Vandevelde">Thierry Vandevelde</name>
<affiliation wicri:level="3">
<country xml:lang="fr">France</country>
<wicri:regionArea>VIVENDI-Générale des Eaux, 52 rue d’Anjou, 75384 Paris Cedex 08</wicri:regionArea>
<placeName>
<region type="region" nuts="2">Île-de-France</region>
<settlement type="city">Paris</settlement>
</placeName>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Water Research</title>
<title level="j" type="abbrev">WR</title>
<idno type="ISSN">0043-1354</idno>
<imprint>
<publisher>ELSEVIER</publisher>
<date type="published" when="2000">2000</date>
<biblScope unit="volume">34</biblScope>
<biblScope unit="issue">7</biblScope>
<biblScope unit="page" from="2110">2110</biblScope>
<biblScope unit="page" to="2118">2118</biblScope>
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<idno type="ISSN">0043-1354</idno>
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<idno type="ISSN">0043-1354</idno>
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<keywords scheme="KwdEn" xml:lang="en">
<term>Aquifer</term>
<term>Aquifer material</term>
<term>Aquifer matrix</term>
<term>Aquifer storage</term>
<term>Aquifer system</term>
<term>Bacterial biomass</term>
<term>Bacterial production</term>
<term>Baveye</term>
<term>Biomass</term>
<term>Biomass accumulation</term>
<term>Biomass density</term>
<term>Calcareous aquifer</term>
<term>Calcite</term>
<term>Calcite dissolution</term>
<term>Calcium concentration</term>
<term>Calcium concentrations</term>
<term>Calcium levels</term>
<term>Column studies</term>
<term>Conductivity</term>
<term>Continuous injection</term>
<term>Core material</term>
<term>Csiro land water</term>
<term>Dissolution</term>
<term>Earth sciences</term>
<term>Elsevier science</term>
<term>Fatty acids</term>
<term>Flinders university</term>
<term>Glen osmond</term>
<term>Groundwater</term>
<term>Groundwater recharge</term>
<term>Hydraulic</term>
<term>Hydraulic conductivities</term>
<term>Hydraulic conductivity</term>
<term>Initial drop</term>
<term>Injection</term>
<term>Inlet</term>
<term>Laboratory columns</term>
<term>Long island</term>
<term>Northern adelaide plains</term>
<term>Organic carbon</term>
<term>Physical properties</term>
<term>Polysaccharide</term>
<term>Polysaccharide production</term>
<term>Pressure sensors</term>
<term>Previous research</term>
<term>Recharge</term>
<term>Recharge water</term>
<term>Recharge wells</term>
<term>Sand columns</term>
<term>Sand grains</term>
<term>Schematic representation</term>
<term>Slight increase</term>
<term>Total biomass</term>
<term>Vandevivere</term>
<term>Wastewater</term>
<term>Wastewater injection</term>
<term>Water quality parameters</term>
</keywords>
<keywords scheme="Teeft" xml:lang="en">
<term>Aquifer</term>
<term>Aquifer material</term>
<term>Aquifer matrix</term>
<term>Aquifer storage</term>
<term>Aquifer system</term>
<term>Bacterial biomass</term>
<term>Bacterial production</term>
<term>Baveye</term>
<term>Biomass</term>
<term>Biomass accumulation</term>
<term>Biomass density</term>
<term>Calcareous aquifer</term>
<term>Calcite</term>
<term>Calcite dissolution</term>
<term>Calcium concentration</term>
<term>Calcium concentrations</term>
<term>Calcium levels</term>
<term>Column studies</term>
<term>Conductivity</term>
<term>Continuous injection</term>
<term>Core material</term>
<term>Csiro land water</term>
<term>Dissolution</term>
<term>Earth sciences</term>
<term>Elsevier science</term>
<term>Fatty acids</term>
<term>Flinders university</term>
<term>Glen osmond</term>
<term>Groundwater</term>
<term>Groundwater recharge</term>
<term>Hydraulic</term>
<term>Hydraulic conductivities</term>
<term>Hydraulic conductivity</term>
<term>Initial drop</term>
<term>Injection</term>
<term>Inlet</term>
<term>Laboratory columns</term>
<term>Long island</term>
<term>Northern adelaide plains</term>
<term>Organic carbon</term>
<term>Physical properties</term>
<term>Polysaccharide</term>
<term>Polysaccharide production</term>
<term>Pressure sensors</term>
<term>Previous research</term>
<term>Recharge</term>
<term>Recharge water</term>
<term>Recharge wells</term>
<term>Sand columns</term>
<term>Sand grains</term>
<term>Schematic representation</term>
<term>Slight increase</term>
<term>Total biomass</term>
<term>Vandevivere</term>
<term>Wastewater</term>
<term>Wastewater injection</term>
<term>Water quality parameters</term>
</keywords>
<keywords scheme="Wicri" type="topic" xml:lang="fr">
<term>Biomasse</term>
<term>Sciences de la terre</term>
<term>Eau souterraine</term>
<term>Eau usée</term>
</keywords>
</textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
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<front>
<div type="abstract" xml:lang="en">Abstract: Laboratory columns were used to understand and predict bore clogging issues at a South Australian recycled water aquifer storage and recovery site, before field trials proceeded. The columns were used to study biogeochemical processes resulting from the continuous injection of recycled water into an aquifer matrix. The results showed that despite levels of suspended solids (SS) between 3–4 mg/l in the influent, flow rates (hydraulic conductivities) were maintained at 20–50% of initial flow through three identical columns for a period of 22 days. An initial decline in the hydraulic conductivity (K) through the columns was evident early in the experiment, and decreased from 0.78 m/day to 0.062 m/day in the first 7 days of the experiment. This was thought to be due to physical clogging by suspended solids and then biological clogging by biomass accumulation and polysaccharide production at the inflow end of the columns. The physical bioclogging was relieved midway through the experiment due to calcite dissolution mainly at the inlet end of the columns. Calcite reprecipitation at the outflow end of the columns was evident from SEM micrographs.</div>
</front>
</TEI>
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