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Recharge systems for protecting and enhancing groundwate

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TOPIC 1<br />

Alternative recharge <strong>systems</strong> / <strong>Recharge</strong> <strong>systems</strong> 205<br />

METHODOLOGY<br />

The technical effectiveness of the recharge structures is evaluated at two scales:<br />

1. Impact at recharge structure scale;<br />

2. Impact on the <strong>groundwate</strong>r resources in the local aquifer.<br />

Emphasis is thereby placed on the development of simple numerical solutions to help evaluate technical effectiveness,<br />

which can be applied locally without detailed knowledge of artificial recharge processes.<br />

Impact at recharge structure scale<br />

At the recharge structure scale, the decline in water level in the structure is an indicator of the per<strong>for</strong>mance of a<br />

recharge structure. The water balance <strong>for</strong> the structure can be simplified during periods of no precipitation <strong>and</strong><br />

when surface inflow <strong>and</strong> outflow can be neglected. A further simplification can be made if losses due to leakage,<br />

direct abstraction etc. can be neglected, <strong>and</strong> if the structure is under effluent conditions in relation to the aquifer.<br />

With these simplifications the water balance can be summarized as:<br />

Infiltration = Change of volume of water in the structure - Evaporation<br />

Under such conditions, the balance between evaporation <strong>and</strong> infiltration will determine the effectiveness of the artificial<br />

recharge scheme.<br />

The change of volume in the reservoirs at the Indian case study sites is monitored by recording the change in reservoir<br />

water level with time. For periods without direct abstraction <strong>and</strong> rainfall, this is translated into infiltration rates<br />

after subtracting estimated open water evaporation rates. Assuming the overall change in unsaturated zone storage<br />

is negligible, this infiltration is equal to <strong>groundwate</strong>r recharge.<br />

Impact of artificial recharge on the <strong>groundwate</strong>r resources<br />

in the local aquifer<br />

Besides estimating <strong>groundwate</strong>r recharge from structures, the distribution of this additional water recharged is<br />

important in determining its availability to the user. This was assessed by developing both analytical <strong>and</strong> numerical<br />

models. Setting up of data intensive detailed numerical models to evaluate site-specific recharge schemes is not<br />

always feasible, especially <strong>for</strong> low-technology schemes, e.g. small check dams, in developing countries. Emphasis<br />

was there<strong>for</strong>e placed on the development of a simple numerical tool to allow the order-of-magnitude impact of artificial<br />

recharge to be examined <strong>and</strong> visualized <strong>for</strong> aquifers of various hydraulic properties. The aim of developing an<br />

analytical model was to provide a tool <strong>for</strong> assessing the impact of artificial recharge structures <strong>for</strong> users not familiar<br />

with numerical modelling codes, such as MODFLOW (McDonald <strong>and</strong> Harbaugh, 1988). It allows users to investigate<br />

homogeneous aquifer <strong>systems</strong> <strong>and</strong> their responses to recharge using Excel spreadsheets. The numerical model<br />

was used to verify the analytical code by simulating responses of homogenous aquifers to recharge events <strong>and</strong> comparing<br />

model results. Additionally, it was used to simulate the impact of artificial recharge on non-homogenous<br />

aquifers <strong>and</strong> to incorporate abstraction from boreholes. The analytical <strong>and</strong> numerical models allow:<br />

• Estimation of expected water level rise following recharge events within various hydrogeological settings.<br />

• Assessment of the likely impact zone of a recharge structure, i.e. the area in which a rise in water level is<br />

experienced.<br />

• Simulation of the dissipation of the <strong>groundwate</strong>r mound with time.<br />

10 – 16 June 2005, Berlin ■ 5th International Symposium ■ AQUIFER RECHARGE ■ ISMAR 2005

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