Impact of high-permeability preferential flow zones on pumping-induced airflow in unconfined aquifer
Jipeng Shan
State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China
Search for more papers by this authorZhenlei Yang
Key Laboratory of Coastal Environment and Resources of Zhejiang Province, School of Engineering, Westlake University, Hangzhou, China
Search for more papers by this authorCorresponding Author
Xingxing Kuang
State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China
Correspondence
Xingxing Kuang, State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China.
Email: [email protected]
Search for more papers by this authorJiu Jimmy Jiao
Department of Earth Sciences, The University of Hong Kong, Hong Kong, China
Search for more papers by this authorJipeng Shan
State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China
Search for more papers by this authorZhenlei Yang
Key Laboratory of Coastal Environment and Resources of Zhejiang Province, School of Engineering, Westlake University, Hangzhou, China
Search for more papers by this authorCorresponding Author
Xingxing Kuang
State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China
Correspondence
Xingxing Kuang, State Environmental Protection Key Laboratory of Integrated Surface Water-Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China.
Email: [email protected]
Search for more papers by this authorJiu Jimmy Jiao
Department of Earth Sciences, The University of Hong Kong, Hong Kong, China
Search for more papers by this authorAbstract
When the unsaturated zone of the unconfined aquifer is covered by a low-permeability upper layer, significant airflow will be generated in the unsaturated zone during water pumping. However, high permeability preferential flow zones (PFZs) such as fractures and macropores are frequently present in the unsaturated zone, forming the preferential fluid flow paths, which may change the original airflow pattern in the unsaturated zone during the pumping test and consequently affect the precision of obtained aquifer hydraulic parameters. The main objective of this paper is to investigate the effect of PFZs in low-permeability upper layer on pumping-induced airflow in the unsaturated zone by numerical simulations of transient three-dimensional air-water two-phase flow and to quantify errors in the aquifer hydraulic parameters obtained during pumping test. The results demonstrate that a large amount of air flows quickly from the atmosphere into the unsaturated zone through the PFZs, and that the PFZs can draw some air from the nearby low-permeability soils as well. The significant influx of air through PFZs also reduces the negative air pressure in the unsaturated zone and decreases the drawdown in the saturated zone at intermediate times, which are nevertheless still greater than the results obtained in the homogeneous aquifer. Estimations of the aquifer hydraulic parameters reveal that errors of these parameters obtained are smaller when the PFZs with favourable combinations of permeability, width and quantities facilitate more air to flow into the unsaturated zone.
Open Research
DATA AVAILABILITY STATEMENT
Data sharing not applicable to this article as no datasets were generated or analysed during the current study.
REFERENCES
- Allaire, S. E., Roulier, S., & Cessna, A. J. (2009). Quantifying preferential flow in soils: A review of different techniques. Journal of Hydrology, 378(1–2), 179–204.
- Amanambu, A. C., Obarein, O. A., Mossa, J., Li, L., Ayeni, S. S., Balogun, O., Oyebamiji, A., & Ochege, F. U. (2020). Groundwater system and climate change: Present status and future considerations. Journal of Hydrology, 589, 125163.
- Berg, S. J., & Illman, W. A. (2012). Improved predictions of saturated and unsaturated zone drawdowns in a heterogeneous unconfined aquifer via transient hydraulic tomography: Laboratory sandbox experiments. Journal of Hydrology, 470, 172–183.
10.1016/j.jhydrol.2012.08.044 Google Scholar
- Berkowitz, B., Silliman, S. E., & Dunn, A. M. (2004). Impact of the capillary fringe on local flow, chemical migration, and microbiology. Vadose Zone Journal, 3(2), 534–548.
- Beven, K., & Germann, P. (1982). Macropores and water flow in soils. Water Resources Research, 18(5), 1311–1325.
- Beven, K., & Germann, P. (2013). Macropores and water flow in soils revisited. Water Resources Research, 49(6), 3071–3092.
- Bishop, J. M., Callaghan, M. V., Cey, E. E., & Bentley, L. R. (2015). Measurement and simulation of subsurface tracer migration to tile drains in low permeability, macroporous soil. Water Resources Research, 51(6), 3956–3981.
- Boulton, N. S. (1954). Unsteady radial flow to a pumped well allowing for delayed yield from storage. International Association of Scientific Hydrology Publications, 2, 472–477.
- Boulton, N. S. (1963). Analysis of data from non-equilibrium pumping tests allowing for delayed yield from storage. Proceedings of the Institution of Civil Engineers, 26(3), 469–482.
10.1680/iicep.1963.10409 Google Scholar
- Bouma, J. (1981). Soil morphology and preferential flow along macropores. Agricultural Water Management, 3(4), 235–250.
- Bouwer, H., & Rice, R. C. (1978). Delayed aquifer yield as a phenomenon of delayed air entry. Water Resources Research, 14(6), 1068–1074.
- Bundt, M., Widmer, F., Pesaro, M., Zeyer, J., & Blaser, P. (2001). Preferential flow paths: Biological ‘hot spots’ in soils. Soil Biology and Biochemistry, 33(6), 729–738.
- Bunn, M. I., Jones, J. P., Endres, A. L., & Rudolph, D. L. (2010). Effects of hydraulic conductivity heterogeneity on vadose zone response to pumping in an unconfined aquifer. Journal of Hydrology, 387(1–2), 90–104.
- Butler, J. J., Jr., & Healey, J. M. (1998). Relationship between pumping-test and slug-test parameters: Scale effect or artifact? Groundwater, 36(2), 305–312.
- Carsel, R. F., & Parrish, R. S. (1988). Developing joint probability distributions of soil water retention characteristics. Water Resources Research, 24(5), 755–769.
- Dunkerley, D. (2012). Effects of rainfall intensity fluctuations on infiltration and runoff: Rainfall simulation on dryland soils, fowlers gap, Australia. Hydrological Processes, 26(15), 2211–2224.
- Endres, A. L., Jones, J. P., & Bertrand, E. A. (2007). Pumping-induced vadose zone drainage and storage in an unconfined aquifer: A comparison of analytical model predictions and field measurements. Journal of Hydrology, 335(1–2), 207–218.
- Flury, M., Flühler, H., Jury, W. A., & Leuenberger, J. (1994). Susceptibility of soils to preferential flow of water: A field study. Water Resources Research, 30(7), 1945–1954.
- Ghodrati, M., & Jury, W. A. (1990). A field study using dyes to characterize preferential flow of water. Soil Science Society of America Journal, 54(6), 1558–1563.
- Guo, H. P., & Jiao, J. J. (2008). Numerical study of airflow in the unsaturated zone induced by sea tides. Water Resources Research, 44(6), W06402.
10.1029/2007WR006532 Google Scholar
- Guo, H., Jiao, J. J., & Weeks, E. P. (2008). Rain-induced subsurface airflow and Lisse effect. Water Resources Research, 44(7), W07409.
10.1029/2007WR006294 Google Scholar
- Halford, K. J. (1997). Effects of unsaturated zone on aquifer test analysis in a shallow-aquifer system. Groundwater, 35(3), 512–522.
- Jarvis, N., Koestel, J., & Larsbo, M. (2016). Understanding preferential flow in the vadose zone: Recent advances and future prospects. Vadose Zone Journal, 15(12), 1–11.
- Jiao, J. J., & Guo, H. (2009). Airflow induced by pumping tests in unconfined aquifer with a low-permeability cap. Water Resources Research, 45(10), W10445.
10.1029/2009WR007760 Google Scholar
- Jiao, J. J., & Li, H. (2004). Breathing of coastal vadose zone induced by sea level fluctuations. Geophysical Research Letters, 31(11), L11502.
- Köhne, J. M., Köhne, S., & Šimůnek, J. (2009). A review of model applications for structured soils: A water flow and tracer transport. Journal of Contaminant Hydrology, 104, 4–35.
- Kroszynski, U. I., & Dagan, G. (1975). Well pumping in unconfined aquifers: The influence of the unsaturated zone. Water Resources Research, 11(3), 479–490.
- Kuang, X., Jiao, J. J., Huang, H., & Qian, J. (2013). Air and water flows in a large sand box with a two-layer aquifer system. Hydrogeology Journal, 21(5), 977–985.
- Kuang, X., Jiao, J. J., & Li, H. (2013). Review on airflow in unsaturated zones induced by natural forcings. Water Resources Research, 49(10), 6137–6165.
- Kuang, X., Jiao, J. J., Wan, L., Wang, X., & Mao, D. (2011). Air and water flows in a vertical sand column. Water Resources Research, 47(4), W04506.
- Kuang, X., Jiao, J. J., Zhang, K., & Mao, D. (2014). Air and water flows induced by pumping tests in unconfined aquifers with low-permeability zones. Hydrological Processes, 28(21), 5450–5464.
- Kung, K. S. (1990). Preferential flow in a sandy vadose zone: 1. Field observation. Geoderma, 46(1–3), 51–58.
- Kung, K. J., Steenhuis, T. S., Kladivko, E. J., Gish, T. J., Bubenzer, G., & Helling, C. S. (2000). Impact of preferential flow on the transport of adsorbing and non-adsorbing tracers. Soil Science Society of America Journal, 64(4), 1290–1296.
- Kurtzman, D., Baram, S., & Dahan, O. (2016). Soil–aquifer phenomena affecting groundwater under vertisols: A review. Hydrology and Earth System Sciences, 20, 1–12.
- Kurylyk, B. L., MacQuarrie, K. T., & McKenzie, J. M. (2014). Climate change impacts on groundwater and soil temperatures in cold and temperate regions: Implications, mathematical theory, and emerging simulation tools. Earth-Science Reviews, 138, 313–334.
- Logsdon, S. D. (2002). Determination of preferential flow model parameters. Soil Science Society of America Journal, 66(4), 1095–1103.
- Mao, D., Wan, L., Yeh, T. C. J., Lee, C. H., Hsu, K. C., Wen, J. C., & Lu, W. (2011). A revisit of drawdown behavior during pumping in unconfined aquifers. Water Resources Research, 47(5), W05502.
- Moench, A. F. (1993). Computation of type curves for flow to partially penetrating wells in water-table aquifers. Groundwater, 31(6), 966–971.
- Moench, A. F. (1994). Specific yield as determined by type-curve analysis of aquifer-test data. Groundwater, 32(6), 949–957.
- Moench, A. F. (1996). Flow to a well in a water-table aquifer: An improved Laplace transform solution. Groundwater, 34(4), 593–596.
- Moench, A. F. (2004). Importance of the vadose zone in analyses of unconfined aquifer tests. Groundwater, 42(2), 223–233.
- Morales, V. L., Parlange, J. Y., & Steenhuis, T. S. (2010). Are preferential flow paths perpetuated by microbial activity in the soil matrix? A review. Journal of Hydrology, 393(1–2), 29–36.
- Mualem, Y. (1976). A new model for predicting the hydraulic conductivity of unsaturated porous media. Water Resources Research, 12(3), 513–522.
- Narasimhan, T. N., & Zhu, M. (1993). Transient flow of water to a well in an unconfined aquifer: Applicability of some conceptual models. Water Resources Research, 29(1), 179–191.
- Neuman, S. P. (1972). Theory of flow in unconfined aquifers considering delayed response of the water table. Water Resources Research, 8(4), 1031–1045.
- Neuman, S. P. (1974). Effect of partial penetration on flow in unconfined aquifers considering delayed gravity response. Water Resources Research, 10(2), 303–312.
- Nwankwor, G. I., Gillham, R. W., van der Kamp, G., & Akindunni, F. F. (1992). Unsaturated and saturated flow in response to pumping of an unconfined aquifer: Field evidence of delayed drainage. Groundwater, 30(5), 690–700.
- Pruess, K., Oldenburg, C. M., & Moridis, G. J. (1999). TOUGH2 user's guide version 2 (no. LBNL-43134). Lawrence Berkeley National Lab (LBNL).
10.2172/751729 Google Scholar
- Raghavan, R. (2004). A review of applications to constrain pumping test responses to improve on geological description and uncertainty. Reviews of Geophysics, 42(4), RG4001.
10.1029/2003RG000142 Google Scholar
- Ritsema, C. J., Dekker, L. W., Hendrickx, J. M. H., & Hamminga, W. (1993). Preferential flow mechanism in a water repellent sandy soil. Water Resources Research, 29(7), 2183–2193.
- Shao, W., Bogaard, T. A., Bakker, M., & Greco, R. (2015). Quantification of the influence of preferential flow on slope stability using a numerical modelling approach. Hydrology and Earth System Sciences, 19(5), 2197–2212.
- Šimůnek, J., Jarvis, N. J., van Genuchten, M. T., & Gärdenäs, A. (2003). Review and comparison of models for describing non-equilibrium and preferential flow and transport in the vadose zone. Journal of Hydrology, 272(1–4), 14–35.
- Streltsova, T. D. (1973). Flow near a pumped well in an unconfined aquifer under nonsteady conditions. Water Resources Research, 9(1), 227–235.
- Tartakovsky, G. D., & Neuman, S. P. (2007). Three-dimensional saturated-unsaturated flow with axial symmetry to a partially penetrating well in a compressible unconfined aquifer. Water Resources Research, 43(1), W01410.
10.1029/2006WR005153 Google Scholar
- Taylor, R. G., Scanlon, B., Döll, P., Rodell, M., van Beek, R., Wada, Y., Longuevergne, L., Leblanc, M., Famiglietti, J. S., Edmunds, M., Konikow, L., Green, T. R., Chen, J., Taniguchi, M., Bierkens, M. F. P., MacDonald, A., Fan, Y., Maxwell, R. M., Yechieli, Y., … Treidel, H. (2013). Ground water and climate change. Nature Climate Change, 3, 322–329.
- Theis, C. V. (1935). The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage. Eos, Transactions American Geophysical Union, 16(2), 519–524.
10.1029/TR016i002p00519 Google Scholar
- Tsutsumi, D., Sidle, R. C., & Kosugi, K. I. (2005). Development of a simple lateral preferential flow model with steady state application in hillslope soils. Water Resources Research, 41(12), W12420.
- Van Dam, J. C., & Feddes, R. A. (2000). Numerical simulation of infiltration, evaporation and shallow groundwater levels with the Richards equation. Journal of Hydrology, 233(1–4), 72–85.
- Van Genuchten, M. T. (1980). A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal, 44(5), 892–898.
- Weisbrod, N., Dragila, M. I., Nachshon, U., & Pillersdorf, M. (2009). Falling through the cracks: The role of fractures in earth-atmosphere gas exchange. Geophysical Research Letters, 36, L02401.
- Xun, Z., Chao, S., Ting, L., Ruige, C., Huan, Z., Jingbo, Z., & Qin, C. (2015). Estimation of aquifer parameters using tide-induced groundwater level measurements in a coastal confined aquifer. Environmental Earth Sciences, 73(5), 2197–2204.
10.1007/s12665-014-3570-5 Google Scholar
- Ye, J., Shan, J., Zhou, H., & Yan, N. (2021). Numerical modelling of the wave interaction with revetment breakwater built on reclaimed coral reef islands in the South China Sea—Experimental verification. Ocean Engineering, 235, 109325.
10.1016/j.oceaneng.2021.109325 Google Scholar