Skip to main content
Log in

Impact of roots on ground water quality

  • Published:
Plant and Soil Aims and scope Submit manuscript

Abstract

Preferential flow is perhaps the major chemical transport process influencing the rapid and typically unexpected movement of agricultural chemicals to ground water. Plant roots are a major contributor to preferential flow mechanics as they form spatial voids which can be used as preferential flow pathways. Chemical transport of atrazine, deethylatrazine, and bromide solutions concentrations under tilled and no-tilled corn fields was evaluated below the active root zone. Additionally, the impact of roots on flow pathways was visualized using a soluble dye (Brilliant Blue FCF). Pictures of the dye-stained pattern were subsequently digitized to determine the cross-sectional area used for transport as a function of depth. Bromide transit times through the field soils were not influenced by tillage practice, whereas atrazine transport was strongly influenced by tillage practice. Under no-till field conditions, atrazine was rarely detected but deethylatrazine concentrations were greater than those observed under tilled field conditions. Visual observation indicated that the dye under no-tillage was more predominant in the corn row, indicative of transport through void root channels. No-tillage practices may decrease the likelihood of ground water contamination through leaching due to the formation of stable root channels where an organic carbon source and microbial population are preferentially located to degrade pesticides.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Baker R S and Hillel D 1990 Laboratory tests of a theory of fingering during infiltration into layered soils. Soil Sci. Soc. Am. J. 54, 20-30.

    Google Scholar 

  • Bouma J 1981 Soil morphology and preferential flow along macropores. Agric. Water Mgmt. 3, 235-250.

    Google Scholar 

  • Brasino J S 1986 A simple stochastic model predicting conservative mass transport through the unsaturated zone into groundwater. Ph.D. Thesis, Univ. Wisconsin-Madison, WI.

    Google Scholar 

  • Edwards W M, Norton L D and Edmond C E 1988 Characterizing macropores that effect infiltration into no-tilled soil. Soil Sci. Soc. Am. J. 2: 483-487.

    Google Scholar 

  • Edwards W M, Shipitalo M J, Owens L B and Norton L D 1990 Effect of Lumbricus Terrestries L. Burrows on hydrology of continous no-till corn fields. Geoderma. 46, 73-84.

    Google Scholar 

  • Edwards W M, Shipitalo M J, Owens L B and Dick W A 1993 Factors affecting preferential flow of water and atrazine through earthworm burrows under no-till corn. J. Environ. Qual. 22, 453-457.

    Google Scholar 

  • Flury M, Fluhler H, Jury W A and Leuenberger J 1994 Susceptibility of soils to preferential flow of water: A field study. Water Resour. Res. 30, 1945-1954.

    Google Scholar 

  • Germann P F and Beven K 1981 Water flow in soil macropores. I: An experimental approach. J. Soil Sci. 18, 363-368.

    Google Scholar 

  • Gish T J, Isensee A R, Nash R G and Helliug C S 1991 Impact of pesticides on shallow ground water quality. Trans. Am. Soc. Agric. Eng. 34, 1745-1753.

    Google Scholar 

  • Gish T J and Jury W A 1983 Effect of plant roots and root channels on solute transport. Trans. Am. Soc. Agric. Eng. 26, 440-444, 451.

    Google Scholar 

  • Gish T J, Shirmohammadi A, Vyravipillai R and Wienhold B J 1995 Herbicide leaching under tilled and no-tillage fields. Soil Sci. Soc. Am. J. 59, 895-901.

    Google Scholar 

  • Gish T J, Shirmohammadi A, Helling C S, Kung K-J S, Wienhold B J F and Rawls W J 1997 Mechanisms of herbicide leaching and volatilization and innovative approaches for sampling, prediction and control. In Integrated Weed and Soil Management. Ed. J L Hatfield and B A Stewart. pp 107-134. Ann Arbor Press, Chelsea, Michigan.

    Google Scholar 

  • Glass R J, Steenhuis T S and Parlange J-Y 1988 Wetting front instability as a rapid and far reaching hydrologic process in the vadose zone. In Rapid and Far Reaching Hydrological Processes in the Vadose Zone. Ed. P F Germann. J. Contam. Hydrol. 3, 207-226.

  • Greenland D L 1979. The physics and chemistry of the soil-root interface: Some comments. In The Soil-Root Interface. Eds. J L Harley and R Scott Russell. pp 81-98. Academic Press, New York.

    Google Scholar 

  • Hatano R, Kawamura N, Ikeda J and Sakuma T. 1992. Evaluation of the effect of morphological features of flow paths on solute transport by using fractal dimensions of methylene blue staining pattern. Geoderma 53, 31-44.

    Google Scholar 

  • Helling C S and Gish T J 1991 Physical and chemical processes affecting preferential flow. In Preferential Flow. Eds. T J Gish and A Shirmohammadi. pp 77-86. Proc. Natl. Symp., 16–17 Dec. 1991, Chicago, IL. Am Soc. Agric. Eng., St. Joseph, MI.

    Google Scholar 

  • Hill D E and Parlange J Y 1972 Wetting front instability in layered soils. Soil Sci. Soc. Am. Proc. 36, 697-702.

    Google Scholar 

  • Isensee A R, Nash R G and Helling C S 1990 Effect of conventional vs. no-tillage on pesticide leaching to groundwater. J. Environ. Qual. 19, 434-440.

    Google Scholar 

  • Ju S H and Kung K J S 1993 Finite element simulation of funnel flow and overall flow property induced by multiple soil layers. J. Environ. Qual. 22, 432-442.

    Google Scholar 

  • Ju S H, Kung K J S and Helling C S 1996 Simulating impact of funnel flow on contaminant sampling. Soil Sci. Soc. Am. J. (In press).

  • Kladivko E J, Van Scoyoc C E, Monke E J, Oates K M and Pask W 1991 Pesticide and nutrient movement into subsurface the drains on a silt loam soil in Indiana. J. Environ. Qual. 20, 264-270.

    Google Scholar 

  • Kung K J S 1990a Preferential flow in a sandy vadose zone: 1. Field observation. Geoderma 46, 51-58.

    Google Scholar 

  • Kung K J S 1990b Preferential flow in a sandy vadose zone: Mechanism and implications. Geoderma 46, 59-71.

    Google Scholar 

  • Kung K T S and Donohue S V 1991 Improved solute-sampling protocol in a sandy vadose zone using ground-penetrating radar. Soil Sci. Soc. Am. J. 55, 1543-1545.

    Google Scholar 

  • Luxmoore R J 1991 On preferential flow and its measurement. In Preferential Flow. Eds. T J Gish and A Shirmohammadi. pp 113-121. Proc. Natl. Symp. 16–17 Dec. 1991, Chicago, IL. Am. Soc. Agric. Eng., St. Joseph, MI.

    Google Scholar 

  • McCoy E L, Boast C W, Stehouwer R C and Kladivko E J 1994 Macropore hydraulics: Taking a sledgehammer to classical theory. In Soil Processes and Water Quality. Eds. R Lal and B A Stewart. pp 308-348. Lewis Publ., Ann Arbor, MI.

    Google Scholar 

  • Nordquist A W, Tsang Y W, Tsang C F, Dverstrop B and Andersson J 1992 A variable aperture fracture network model for flow and transport in fractured rocks. Water Resour. Res. 28, 1703-1713.

    Google Scholar 

  • Nash R G 1990 Solid-phase extraction of carbofuran, atrazine, simazine, alachlor, and cyanazine from shallow well water. J. Assoc. Off. Anal. Chem. 73, 438-442.

    Google Scholar 

  • Owens L B and Edwards W M 1992 Long-term groundwater quality from a one-time surface bromide application. J. Environ. Qual. 21, 406-410.

    Google Scholar 

  • Parker J C and van Genuchten M Th 1984 Determining transport parameters from laboratory and field experiments. Virginia Agric. Exp. Stn. Bull. 84-3.

  • Pivetz B E and Steenhuis T S 1995 Soil matrix and macropore biodegradation of 2,4-D. Environ. Qual. 24: 564-570.

    Google Scholar 

  • Quisenbeny V L, Phillips R E, Nelson P A and Hatfield M W 1991 Preferential flow in structured and non-structured soils. In Characterization of Transport Phenomena in the Vadose Zone. pp 50-51. Tucson, AZ, 2–5 Apr. 1991.

  • Richards T L and Steenhuis T S 1988 The drain sampling of preferential flow on a field scale. In Rapid and Far Reaching Hydrological Processes in the Vadose Zone. Ed. P F Germann. J. Contam. Hydrol 3, 307-325.

  • Roth K, Jury W A, Fluhler H and Attinger W 1991 Transport of chloride through an unsaturated fields soil. Water Resour. Res. 27, 2533-2541.

    Google Scholar 

  • Stearman G K, Lewis F J, Tortorelli L J and Taylor D D 1989 Herbicide reactivity of soil organic matter in no-tilled and tilled cotton. Soil Sci. Soc. Am. J. 53, 1690-1694.

    Google Scholar 

  • Tsang C F, Tsang Y W and Hale F V 1991 Tracer transport in fractures: Analysis of field data based on variable-aperture channel model. Water Resour. Res. 27, 3095-3106.

    Google Scholar 

  • Van Ommen H C, Dekker L W, Dijksma R, Hulshof J and van der Molen W H 1988 A new technique for evaluating the presence of preferential flow paths in nonstructured soils. Soil Sci. Soc. Am. J. 52, 1192-1193.

    Google Scholar 

  • Wyman J A, Jensen J O, Curwen D, Jones R L and Marquardt T E 1985 Effects of application procedures and irrigation on degradation and movement of aldicarb residues in soil. Environ. Toxicol. Chem. 4, 641-651.

    Google Scholar 

  • Wyman J A, Medina J, Curwen D, Hansen J L and Jones R L 1986 Movement of aldicarb and aldoxycarb residues in soil. Environ. Toxicol. Chem. 5, 545-555.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Gish, T.J., Gimenez, D. & Rawls, W.J. Impact of roots on ground water quality. Plant and Soil 200, 47–54 (1998). https://doi.org/10.1023/A:1004202013082

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1023/A:1004202013082

Navigation