<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-23T15:43:11Z</responseDate><request verb="GetRecord" identifier="oai:univendspace.univen.ac.za:11602/1417" metadataPrefix="dim">https://univendspace.univen.ac.za/server/oai/request</request><GetRecord><record><header><identifier>oai:univendspace.univen.ac.za:11602/1417</identifier><datestamp>2024-09-10T14:42:21Z</datestamp><setSpec>com_11602_1930</setSpec><setSpec>com_11602_1915</setSpec><setSpec>com_11602_1897</setSpec><setSpec>com_11602_737</setSpec><setSpec>col_11602_2152</setSpec><setSpec>col_11602_738</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Odiyo, J.  O.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Ndiritu, J. G.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="advisor">Mwaka, B.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Makungo, Rachel</dim:field>
   <dim:field mdschema="dc" element="date">2019</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2019-10-07T10:50:03Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="available">2019-10-07T10:50:03Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued">2019-09-20</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="citation">Makungo, Rachel (2019)  Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa, University of Venda, South Africa.&amp;lt;http://hdl.handle.net/11602/1417&amp;gt;.</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">http://hdl.handle.net/11602/1417</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="vancouvercitation" lang="en_ZA">Makungo R. Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa. []. , 2019 [cited yyyy month dd]. Available from: http://hdl.handle.net/11602/1417</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="apacitation" lang="en_ZA">Makungo, R. (2019). &amp;lt;i&amp;gt;Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa&amp;lt;/i&amp;gt;. (). . Retrieved from http://hdl.handle.net/11602/1417</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="chicagocitation" lang="en_ZA">Makungo, Rachel. &amp;lt;i&amp;gt;&amp;quot;Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa.&amp;quot;&amp;lt;/i&amp;gt; ., , 2019. http://hdl.handle.net/11602/1417</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="ris" lang="en_ZA">&#xd;
TY  - Thesis&#xd;
AU  - Makungo, Rachel&#xd;
AB  - This study developed operating rules for groundwater supply from a probabilistic (risk-based)&#xd;
approach. Groundwater supply systems are often operated without relating groundwater&#xd;
yield/availability to demand which makes groundwater resource planning and management&#xd;
challenging and unpredictable. Risk-based approaches for developing groundwater operating rules&#xd;
comprehensively incorporate assurance of supply and also account for uncertainty due to model&#xd;
inputs, model structure and climate variability. A groundwater resource unit (GRU) was delineated&#xd;
and its hydrogeological conceptual model developed. Automatic curve matching was used to identify&#xd;
appropriate aquifer models and test solutions for estimating hydraulic characteristics (storativity,&#xd;
transmissivity and hydraulic conductivity) based on Aquifer Test Solver (AQTESOLV) Pro version 4.5.&#xd;
Limited groundwater levels and rainfall data were infilled and/or extended using Output Error-Nonlinear&#xd;
Hammerstein Weiner (OE-NLHW) and non-parametric regression (NPR), respectively.&#xd;
Performances of these models were based on relative error (RE), correlation coefficient (COR), root&#xd;
mean square error (RMSE), coefficient of determination (R2) and Nash Sutcliffe coefficient of efficiency&#xd;
(NSE). A program for generation of monthly groundwater levels for the GRU was coded in FORTRAN&#xd;
based on the revised version of the Pitman model (referred to as GW-PITMAN model). The model was&#xd;
calibrated using groundwater levels from a neighbouring borehole due to lack of observed&#xd;
representative data for the GRU. Validation was done by establishing the realistic nature of simulated&#xd;
runoff, recharge and groundwater levels. A Variable Length Block (VLB) bootstrapping model was used&#xd;
for simultaneous generation of stochastic inputs (rainfall, evaporation and groundwater levels) of the&#xd;
groundwater operating rules model. Operating rules were developed from statistical analysis of 100&#xd;
base yields for the GRU simulated from 5-year long stochastically generated sequences (with length&#xd;
of 34 years) of rainfall, evaporation and groundwater levels. The hydrogeological conceptual model&#xd;
indicated presence of faults and diabase dykes which influence preferential flow paths and storage of&#xd;
water in the aquifer. Identified aquifer test solutions were found to be suitable for estimation of&#xd;
hydraulic characteristics, since they had generally good model fits and low mean residual errors.&#xd;
Heterogeneous aquifer types were identified though leaky aquifer dominated. Storativity,&#xd;
transmissivity and hydraulic conductivity values ranged from 0.0003-0.060, 0.78-12.3 m2/day and&#xd;
0.074-0.460 m/day, respectively, indicating limited storage with potential for local groundwater&#xd;
supply for private consumption. Graphical fits for observed and estimated rainfall and groundwater&#xd;
levels were mostly comparable, though scatter plots indicated cases of underestimation and&#xd;
overestimation of observed values. R2, COR, NSE, RMSE and RE values were 0.76 and 0.7, 0.87 and&#xd;
0.84, 0.75 and 0.68, 3.67 and 3.03 mm and 30 and 29% for both calibration and validation runs,&#xd;
respectively, for NPR model. R2, COR, NSE, RMSE and RE were 0.99 and 0.86, 0.97 and 0.93, 0.99 and&#xd;
0.84, 0.03 and 0.01 m and 0.08 and 0.11% for both calibration and validation runs, respectively, for&#xd;
OE-NLHW model. The models were therefore found to have efficient calibration and validation, and&#xd;
were thus, suitable for data extension. Estimated groundwater levels, streamflow and groundwater&#xd;
recharge for both calibration and validation runs of the GW-PITMAN model, generally fluctuated with&#xd;
changes in rainfall, indicating that they are realistic. Majority (9 out of 10) of the historical statistics&#xd;
were mostly well preserved by VLB, except for skewness. Historic highest groundwater levels were&#xd;
also not well preserved. Superimposing the cumulative demands on the base yield curves and analysis&#xd;
of percentages of water demands that can be supplied indicated that the groundwater system could&#xd;
not meet the water demands at all times. To promote sustainable multipurpose use of water that can&#xd;
enhance rural livelihoods, allocating water using priority classification was found to be essential.&#xd;
Operating rule curves for groundwater supply were derived using a risk-based approach. The&#xd;
operating rule curves indicated that if priority classification is used all water demands are met up to&#xd;
maximum groundwater level of 25 m. The developed operating rule curves are therefore expected to&#xd;
improve water supply to both domestic and productive water uses, if they are adequately&#xd;
implemented and hence improve livelihoods. The procedures followed in developing risk-based&#xd;
groundwater operating rules for Siloam Village were summarised to assist in their application in any&#xd;
delineated groundwater resource unit. Though minimal infrastructure is available to support&#xd;
implementation of the operating rules, additional monitoring boreholes are required to aid in&#xd;
estimation of average groundwater levels for further calibration and validation of the GW-PITMAN&#xd;
model. Detailed geological and geophysical investigation are required to improve on characterisation&#xd;
of the GRU and its hydrogeological conceptual model. Undertaking a study of this nature in other areas&#xd;
including those which are data-scarce could promote wide implementation of risk-based groundwater&#xd;
operating rules.&#xd;
DA  - 2019-09-20&#xd;
DB  - ResearchSpace&#xd;
DP  - Univen&#xd;
KW  - Groundwater&#xd;
KW  - Planning&#xd;
KW  - Probabilistic approach&#xd;
KW  - Risk-based&#xd;
LK  - https://univendspace.univen.ac.za&#xd;
PY  - 2019&#xd;
T1  - Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa&#xd;
TI  - Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa&#xd;
UR  - http://hdl.handle.net/11602/1417&#xd;
ER  - &#xd;
</dim:field>
   <dim:field mdschema="dc" element="description" lang="en_US">PhDENV (Hydrology)</dim:field>
   <dim:field mdschema="dc" element="description">Department of Hydrology and Water Resources</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract" lang="en_US">This study developed operating rules for groundwater supply from a probabilistic (risk-based)&#xd;
approach. Groundwater supply systems are often operated without relating groundwater&#xd;
yield/availability to demand which makes groundwater resource planning and management&#xd;
challenging and unpredictable. Risk-based approaches for developing groundwater operating rules&#xd;
comprehensively incorporate assurance of supply and also account for uncertainty due to model&#xd;
inputs, model structure and climate variability. A groundwater resource unit (GRU) was delineated&#xd;
and its hydrogeological conceptual model developed. Automatic curve matching was used to identify&#xd;
appropriate aquifer models and test solutions for estimating hydraulic characteristics (storativity,&#xd;
transmissivity and hydraulic conductivity) based on Aquifer Test Solver (AQTESOLV) Pro version 4.5.&#xd;
Limited groundwater levels and rainfall data were infilled and/or extended using Output Error-Nonlinear&#xd;
Hammerstein Weiner (OE-NLHW) and non-parametric regression (NPR), respectively.&#xd;
Performances of these models were based on relative error (RE), correlation coefficient (COR), root&#xd;
mean square error (RMSE), coefficient of determination (R2) and Nash Sutcliffe coefficient of efficiency&#xd;
(NSE). A program for generation of monthly groundwater levels for the GRU was coded in FORTRAN&#xd;
based on the revised version of the Pitman model (referred to as GW-PITMAN model). The model was&#xd;
calibrated using groundwater levels from a neighbouring borehole due to lack of observed&#xd;
representative data for the GRU. Validation was done by establishing the realistic nature of simulated&#xd;
runoff, recharge and groundwater levels. A Variable Length Block (VLB) bootstrapping model was used&#xd;
for simultaneous generation of stochastic inputs (rainfall, evaporation and groundwater levels) of the&#xd;
groundwater operating rules model. Operating rules were developed from statistical analysis of 100&#xd;
base yields for the GRU simulated from 5-year long stochastically generated sequences (with length&#xd;
of 34 years) of rainfall, evaporation and groundwater levels. The hydrogeological conceptual model&#xd;
indicated presence of faults and diabase dykes which influence preferential flow paths and storage of&#xd;
water in the aquifer. Identified aquifer test solutions were found to be suitable for estimation of&#xd;
hydraulic characteristics, since they had generally good model fits and low mean residual errors.&#xd;
Heterogeneous aquifer types were identified though leaky aquifer dominated. Storativity,&#xd;
transmissivity and hydraulic conductivity values ranged from 0.0003-0.060, 0.78-12.3 m2/day and&#xd;
0.074-0.460 m/day, respectively, indicating limited storage with potential for local groundwater&#xd;
supply for private consumption. Graphical fits for observed and estimated rainfall and groundwater&#xd;
levels were mostly comparable, though scatter plots indicated cases of underestimation and&#xd;
overestimation of observed values. R2, COR, NSE, RMSE and RE values were 0.76 and 0.7, 0.87 and&#xd;
0.84, 0.75 and 0.68, 3.67 and 3.03 mm and 30 and 29% for both calibration and validation runs,&#xd;
respectively, for NPR model. R2, COR, NSE, RMSE and RE were 0.99 and 0.86, 0.97 and 0.93, 0.99 and&#xd;
0.84, 0.03 and 0.01 m and 0.08 and 0.11% for both calibration and validation runs, respectively, for&#xd;
OE-NLHW model. The models were therefore found to have efficient calibration and validation, and&#xd;
were thus, suitable for data extension. Estimated groundwater levels, streamflow and groundwater&#xd;
recharge for both calibration and validation runs of the GW-PITMAN model, generally fluctuated with&#xd;
changes in rainfall, indicating that they are realistic. Majority (9 out of 10) of the historical statistics&#xd;
were mostly well preserved by VLB, except for skewness. Historic highest groundwater levels were&#xd;
also not well preserved. Superimposing the cumulative demands on the base yield curves and analysis&#xd;
of percentages of water demands that can be supplied indicated that the groundwater system could&#xd;
not meet the water demands at all times. To promote sustainable multipurpose use of water that can&#xd;
enhance rural livelihoods, allocating water using priority classification was found to be essential.&#xd;
Operating rule curves for groundwater supply were derived using a risk-based approach. The&#xd;
operating rule curves indicated that if priority classification is used all water demands are met up to&#xd;
maximum groundwater level of 25 m. The developed operating rule curves are therefore expected to&#xd;
improve water supply to both domestic and productive water uses, if they are adequately&#xd;
implemented and hence improve livelihoods. The procedures followed in developing risk-based&#xd;
groundwater operating rules for Siloam Village were summarised to assist in their application in any&#xd;
delineated groundwater resource unit. Though minimal infrastructure is available to support&#xd;
implementation of the operating rules, additional monitoring boreholes are required to aid in&#xd;
estimation of average groundwater levels for further calibration and validation of the GW-PITMAN&#xd;
model. Detailed geological and geophysical investigation are required to improve on characterisation&#xd;
of the GRU and its hydrogeological conceptual model. Undertaking a study of this nature in other areas&#xd;
including those which are data-scarce could promote wide implementation of risk-based groundwater&#xd;
operating rules.</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="sponsorship" lang="en_US">NRF</dim:field>
   <dim:field mdschema="dc" element="format" qualifier="extent">1 online resource (xx, 217 leaves: color illustrations, color maps)</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso" lang="en_US">en</dim:field>
   <dim:field mdschema="dc" element="rights">University of Venda</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Groundwater</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Planning</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Probabilistic approach</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Risk-based</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_ZA">UCTD</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="ddc">553.790968257</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Water -- South Africa -- Limpopo</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Groundwater -- South Africa -- Limpopo</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Hydrology -- South Africa -- Limpopo</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh">Water-supply -- South Africa -- Limpopo</dim:field>
   <dim:field mdschema="dc" element="title" lang="en_US">Development of risk-based groundwater operating rules: a case study of Siloam Village, South Africa</dim:field>
   <dim:field mdschema="dc" element="type" lang="en_US">Thesis</dim:field>
   <dim:field mdschema="others" element="access-status">open.access</dim:field>
</dim:dim></metadata></record></GetRecord></OAI-PMH>