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The concentration and flux of organic carbon in aquifers is influenced by recharge and abstraction, and surface and subsurface processing.In this study groundwater was abstracted from a shallow fractured rock aquifer and dissolved organic carbon (DOC) was measured in observation bores at different distances from the abstraction bore.The analysis of the variations in DOC within an aquifer during an abstraction experiment has not been undertaken before. The fractured rock system outcrops in the upper reaches of the slope (approximately 100 metres south of the bore field) and becomes deeper down the slope to approximately 7 mbgl at the abstraction location.The experiment was undertaken at the UNSW Wellington Research Station in the central west of NSW, Australia (Fig. Figure 1: Site location, regional topography and relative bore locations (3.1.1 LPI asserts the right to be attributed as author of the original material in the following manner: ©Land and Property Information (date of extraction 19/02/2015)).
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We are not aware of any research on OM accumulation and removal in fractured rock aquifers and none that considers the effects of intense groundwater extraction on native DOM.