Advances in the hydraulic interpretation of water wells using flowmeter logs

Abstract

Abstract. This paper reports on the methodology developed for a new hydraulic interpretation of flowmeter logs, allowing a better characterization of continental hydrological basins. In the course of a flowmeter log, different flow stretches are established, mostly corresponding to permeable layers (aquifers), among which there are other stretches mainly corresponding to less permeable layers (aquitards). In such hydrological basins of sufficient thickness, these flow stretches may not have the same hydraulic head. This fact brings about the need for a new hydraulic interpretation that provides the actual distribution of horizontal permeability throughout the aquifer at depth. The modified hydraulic interpretation developed in this study focuses on the differences of the effective pressure gradient (considered the difference between the hydraulic head in the well and the hydraulic head of each stretch) experienced by the different flow stretches along the well, due to the existence of different hydraulic heads. The methodology has been developed starting from a water well located in a multilayered aquifer within the so-called Madrid basin (the north-western part of the continental basin of the Tagus River), located in the centre of the Iberian Peninsula. In this well, a step-drawdown pumping test was conducted, in which the pumping rate versus drawdown and the specific capacity versus drawdown showed discrepancies with Darcian behaviour and an exponent of the Jacob equation of less than 1. Flowmeter logs were then recorded for different discharge rates and pump depths; the resulting water input from deeper permeable layers did not appear to show the expected relation with respect to drawdown. With the proposed methodology the results comply with the expected linearity and the cited discrepancies are solved.

Correlation of Boreholes through Well Logs: Application to the Western Sector of Madrid

“…However, it is subdivided into great stretches, with some alternating aquifers units separated by non-permeable units (aquitards). This configuration will considerably change the basin model, and the different hydraulic heads obtained in Díaz-Curiel et al, 2022 [ 41 ], allow for a very different hydrogeological interpretation of the basin. The subdivision of a large detrital aquifer into stretches with different hydraulic heads [ 41 ] also requires analyzing whether the different stretches correspond to aquifers of differentiated water quality.…”