Skip to main content
Log in

Characteristics of preferential flow during simulated rainfall events in an arid region of China

  • Original Article
  • Published:
Environmental Earth Sciences Aims and scope Submit manuscript

Abstract

Little is known about preferential flow and its effects on vegetation under natural conditions in an arid oasis ecotone. In this study, we performed dye-tracer experiments using 5, 15, 35, and 55 mm water-sprinkling treatments at three sites: Grass (G), Haloxylon (H), and Populus (P). At each site, we determined soil texture and saturated hydraulic conductivity of the soil (K s) and water flow parameters; we also defined characteristics of soil fracturing and measured plant biomass at site P. The tracer experiments revealed that the three sites displayed significant differences in the degree of preferential flow. Soil structure and surface characteristics were the primary controlling factors, however, they played a different role in different rainfall events. For small rainfall events, soil surface characteristics controlled the preferential flow pattern; for large or extreme rainfall events, soil structure was the critical factor. The effects of different rainfall events were complex and strongly varied among sites. Our results further indicated that preferential flow could impact the growth of annual plants. We conclude that preferential flow in an arid oasis ecotone is a common phenomenon affected by complex factors, and it may be important in soil water distribution and plant growth.

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

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

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

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

References

  • Agrawal YC, McCave IN, Riley JB (1991) Laser diffraction size analysis. In: Syvitski JPM (ed) Principles, methods, and application of particle size analysis. Cambridge University Press, Cambridge, pp 119–128

    Chapter  Google Scholar 

  • Alexander LV, Zhang X, Peterson TC, Caesar J, Gleason B, Klein Tank AMG, Haylock M, Collins D, Trewin B, Rahimzadeh F, Tagipour A, Rupa Kummar K, Revadekar J, Griffiths G, Vincent L, Stephenson DB, Burn J, Aguilar E, Brunet M, Taylor M, New M, Zhai P, Rusticucci M, Vazquez-Agrirre JL (2006) Global observed changes in daily climate extremes of temperature and precipitation. J Geophys Res. doi:10.1029/2005JD006290

    Google Scholar 

  • Allaire SE, Roulier S, Cessna AJ (2009) Quantifying preferential flow in soils: a review of different techniques. J Hydrol 378:179–204

    Article  Google Scholar 

  • Bachmair S, Werler M, Nützmann G (2009) Controls of land use and soil structure on water movement: lesson for pollutant transfer through the unsaturated zone. J Hydrol 369:241–252

    Article  Google Scholar 

  • Bauters TWJ, Steenhuis TS, Parlange J, DiCarlo DA (1998) Preferential flow in water-repellent sands. Soil Sci Soc Am J 62:1185–1190

    Article  Google Scholar 

  • Berndtsson R, Nodomi K, Yasuda H, Persson T, Chen HS, Jinno K (1996) Soil water and temperature patterns in an arid desert dune sand. J Hydrol 185:221–240

    Article  Google Scholar 

  • Blake G, Schlicht E, Zimmerman U (1973) Water recharge in a soil with shrinkage cracks. Soil Sci Soc Am J 37:669–672

    Article  Google Scholar 

  • Bormann H, Klaassen K (2008) Seasonal and land use dependent varibility of soil hydraulic and soil hydrological properties of two Northern German soils. Geoderma 145:295–302

    Article  Google Scholar 

  • Dekker LW, Ritsema CJ (1996a) Variation in water content and wetting patterns in Dutch water repellent peaty clay and clayed peat soils. Catena 28:89–105

    Article  Google Scholar 

  • Dekker LW, Ritsema CJ (1996b) Preferential flow paths in a water repellent clay soil with grass cover. Water Resour Res 32:1239–1249

    Article  Google Scholar 

  • Dekker LW, Ritsema CJ (2000) Wetting patterns and moisture variability in water repellent Dutch soils. J Hydrol 231:148–164

    Article  Google Scholar 

  • Doerr SH, Shakesby R, Walsh R (2000) Soil water repellency: its causes, characteristics and hydro-geomorphological significance. Earth Sci Rev 51:33–65

    Article  Google Scholar 

  • Flury M, Flühler H (1994) Brilliant Blue FCF as a dye tracer for solute transport studies—a toxicological overview. J Environ Qual 23:1108–1112

    Article  Google Scholar 

  • Forrer I, Papritz A, Kasteel R, Flühler H, Luca D (2000) Quantifying dye tracers in soil profiles by image processing. Eur J Soil Sci 51:313–322

    Article  Google Scholar 

  • Ganz C, Bachmann J, Lamparter A, Woche SK, Duijnisveld WHM, Gobel MO (2013) Specific processes during in situ infiltration into a sandy soil with low-level water repellency. J Hydrol 484:45–54

    Article  Google Scholar 

  • Gerke HH (2006) Preferential flow descriptions for structured soils. J Plant Nutr Soil Sci 169:382–400

    Article  Google Scholar 

  • Ghodrati M, Jury WA (1990) A field study using dyes to characterize preferential flow of water. Soil Sci Soc Am J 54:1558–1563

    Article  Google Scholar 

  • Ghodrati M, Ernst FF, Jury WA (1990) Automated spray system for application of solutes to small field plots. Soil Sci Soc Am J 54:287–290

    Article  Google Scholar 

  • Greve A, Andersen MS, Acworth RI (2010) Investigations of soil cracking and preferential flow in a weighing lysimeter filled with cracking clay soil. J Hydrol 393:105–113

    Article  Google Scholar 

  • Hardie M, Lisson S, Doyle R, Cotching W (2013) Determining the frequency, depth and velocity of preferential flow by high frequency of soil moisture monitoring. J Contam Hydrol 144:66–77

    Article  Google Scholar 

  • Heijs AWJ, Ritsema CJ, Dekker LW (1996) Three-dimensional visualization of preferential flow patterns in two soils. Geoderma 70:101–116

    Article  Google Scholar 

  • Heisler-White JL, Knapp AK, Kelly EF (2008) Increasing precipitation event size increases aboveground net primary productivity in a semi-arid grassland. Oecologia 158:129–140

    Article  Google Scholar 

  • IPCC (2007) The physical science basis: contribution of working group I to the fourth assessment of the intergovernmental panel on climate change. Cambridge University Press, Cambridge

    Google Scholar 

  • Jarvis N, Koestel J, Messing I, Moeys J, Lindahl A (2013) Influence of soil, land use and climatic factors on the hydraulic conductivity of soil. Hydrol Earth Syst Sci 17:5185–5195

    Article  Google Scholar 

  • Joshi B, Maulé C (2000) Simple analytical models for interpretation of envrionmental tracer profiles in the vadose zone. Hydrol Process 14:1503–1521

    Article  Google Scholar 

  • Klute A, Dirksen C (1986) Hydraulic conductivity of saturated soils. Klute A(ed) Methods of soil analysis. ASA and SSSA, Madison, pp 694–700

    Google Scholar 

  • Kulasekera PB, Parkin GW, von Bertoldi P (2011) Using soil water content sensors to characterize tillage effects on preferential flow. Vodose Zone J 10:683–696

    Article  Google Scholar 

  • Kung KJS (1990a) Preferential flow in a sandy vadose zone: 1. Field observation. Geoderma 46:51–58

    Article  Google Scholar 

  • Kung KJS (1990b) Preferential flow in a sandy vadose zone: 2. mechanism and implications. Geoderma 46:59–71

    Article  Google Scholar 

  • Legout C, Molenat J, Aquilina L, Gascuel-Odoux C, Faucheux M, Fauvel Y, Bariac T (2007) Solute transfer in the unsaturated zone-groundwater continuum of a headwater catchment. J Hydrol 332:427–441

    Article  Google Scholar 

  • Legout A, Legout C, Nys C, Dambrine E (2009) Preferential flow and slow convective chloride transport through the soil of a forested landscape (Fougeres, France). Geoderma 151:179–190

    Article  Google Scholar 

  • Li XR, Ma FY, Xiao HL, Wang XP, Kim KC (2004) Long-term effects of revegetation on soil water content of sand dunes in arid region of Northern China. J Arid Environ 57:1–16

    Article  Google Scholar 

  • Li XY, Yang ZP, Li YT, Lin H (2009) Connecting ecohydrology and hydropedology in desert shrubs: stemflow as a source of preferential flow in soils. Hydrol Earth Syst Sci 13:1133–1144

    Article  Google Scholar 

  • Lichner L, Eldridge DJ, Schacht K, Zhukova N, Holko L, Sir M, Pecho J (2011) Grass cover influences hydrophysical parameters and heterogeneity of water flow in a sandy soil. Pedosphere 21:719–729

    Article  Google Scholar 

  • Lichner L, Holko L, Zhukova N, Schacht K, Rajkai K, Fodor N, Sandor R (2012) Plants and biological soil crust influence the hydrophysical parameters and water flow in an Aeolian sandy soil. J Hydrol Hydromech 60:309–318

    Google Scholar 

  • Lichner L, Hallett PD, Drongová Z, Czachor H, Kovacik L, Mataix-Solera J, Homolák M (2013) Algae influence the hydrophysical parameters of a sandy soil. Catena 108:58–68

    Article  Google Scholar 

  • Lipsius K, Mooney S (2006) Using image analysis of tracer staining to examine the infiltration patterns in a water repellent contaminated sandy soil. Geoderma 136:865–875

    Article  Google Scholar 

  • Liu JL, Li FR, Liu CA, Liu QJ (2012) Influences of shrub vegetation on distribution and diversity of a ground beetle community in a Gobi desert ecosystem. Biodivers Conserv 21:2601–2619

    Article  Google Scholar 

  • Loik ME, Breshears DD, Lauenroth WK, Belnap J (2004) A multi-scale perspective of water pulses in dryland ecosystems: climatology and ecohydrology of the western USA. Oecologia 141:269–281

    Article  Google Scholar 

  • Martínez-Fernández J, Ceballos A (2003) Temporal stabiltiy of soil moisture in a large-field experiment in Spain. Soil Sci Soc Am J 67:1647–1656

    Article  Google Scholar 

  • Martinez-Meza E, Whitford WG (1996) Stemflow, throughfall and channelization of stemflow by roots in three Chihuahuan desert shrubs. J Arid Envrion 32:271–287

    Article  Google Scholar 

  • Nyman P, Sheridan GJ, Smith HG, Lane PNJ (2014) Modeling the effects of surface storage, macropore flow and water repellency on infiltration after wildfire. J Hydrol 513:301–313

    Article  Google Scholar 

  • Rezanezhad F, Vogel H, Roth K (2006) Experimental study of fingered flow through initially dry sand. Hydrol Earth Syst Sci Discuss 3:2595–2620

    Article  Google Scholar 

  • Ritsema CJ, Dekker LW, Hendrickx JMH, Hamminga W (1993) Preferential flow mechanism in a water repellent sandy soil. Water Resour Res 29:2183–2193

    Article  Google Scholar 

  • Sala OE, Lauenroth WK (1982) Small rainfall events: an ecological role in semiarid regions. Oecologia 53:301–304

    Article  Google Scholar 

  • Schlesinger WH, Reynolds JF, Whitfor WG (1990) Biological feedbacks in global desertification. Science 247:1043–1048

    Article  Google Scholar 

  • Schwartz RC, Evett SR, Unger PW (2003) Soil hydraulic properties of cropland compared with reestablished and native grassland. Geoderma 116:47–60

    Article  Google Scholar 

  • Schwinning S, Sala OE (2004) Hierarchy of responses to resource pulses in arid and semi-arid ecosystems. Oecologia 141:211–220

    Article  Google Scholar 

  • Seyfried MS, Schwinning S, Walvoord MA, Pockman WT, Newman BD, Jackson RB, Phillips FM (2005) Ecohydrological control of deep drainage in arid and semiarid regions. Ecology 86:277–287

    Article  Google Scholar 

  • Shabtai IA, Shenker M, Edeto WL, Warburg A, Ben-Hur M (2014) Effects of land use on structure and hydraulic properties of Vertisols containing a sodic horizon in northern Ethiopia. Soil Till Res 136:19–27

    Article  Google Scholar 

  • Su YZ, Wang XF, Yang R, Lee J (2010) Effects of sandy desertified land rehabilitation on soil carbon sequestration and aggregation in an arid region in China. J Environ Manag 91:2109–2116

    Article  Google Scholar 

  • Tobella AB, Reese H, Almaw A, Bayala J, Malmer A, Laudon H, Ilstedt U (2014) The effect of trees on preferential flow and soil infiltrability in an agroforestry parkland in semiarid Burkina Faso. Water Resour Res 50:3342–3354

    Article  Google Scholar 

  • van der Heijden G, Legout A, Pollier B, Bréchet C, Ranger J, Dambrine E (2013) Tracing and modeling preferential flow in a forest soil—potential impact on nutrient leaching. Geoderma 195–196:12–22

    Article  Google Scholar 

  • van Schaik NLMB (2009) Spatial variability of infiltration patterns related to site characteristics in a semi-arid watershed. Catena 78:36–47

    Article  Google Scholar 

  • Vinton MA, Burke IC (1995) Interactions between individual plant species and soil nutrient status in shortgrass steppe. Ecology 76:1116–1133

    Article  Google Scholar 

  • Vogel HJ, Hoffmann H, Roth K (2005) Studies of crack dynamics in clay soil I. Experimental methods, results, and morphological quantification. Geoderma 125:203–211

    Article  Google Scholar 

  • Vörösmarty CJ, Green P, Salisbury J, Lammers RB (2000) Global water resources: vulnerability from climate change and population growth. Science 289:284–288

    Article  Google Scholar 

  • Walker A, Brown PA (1983) Spatial variability in herbicide degradation rates and residues in soil. Crop Prot 2:17–25

    Article  Google Scholar 

  • Wang XP, Li XR, Xiao HL, Berndtsson R, Pan YX (2007) Effects of surface characteristics on infiltration patterns in an arid shrub desert. Hydrol Process 21:72–79

    Article  Google Scholar 

  • Wang XP, Wang ZN, Berndtsson R, Zhang YF, Pan YX (2011) Desert shrub stemflow and its significance in soil moisture replenishment. Hydrol Earth Syst Sci 15:561–567

    Article  Google Scholar 

  • Wang H, Chen Y, Chen Z (2013a) Spatial distribution and temporal trends of mean precipitation and extremes in the arid region, northwest of China, during 1960–2010. Hydrol Process 27:1807–1818

    Article  Google Scholar 

  • Wang XP, Pan YX, Zhang YF, Dou DQ, Hu R, Zhang H (2013b) Temporal stability analysis of surface and subsurface soil moisture for a transect in artificial revegetation desert area, China. J Hydrol 507:100–109

    Article  Google Scholar 

  • Zehe E, Flühler H (2001) Preferential transport of isoproturon at a plot scale and a field scale tile-drained site. J Hydrol 247:100–115

    Article  Google Scholar 

  • Zhang PP, Shao MA (2013) Temporal stability of surface soil moisture in a desert area of northwestern China. J Hydrol 505:91–101

    Article  Google Scholar 

  • Zhang YF, Wang XP, Hu R, Pan YX, Zhang H (2013) Stemflow in two xerophytic shrubs and its significance to soil water and nutrient enrichment. Ecol Res 28:567–579

    Article  Google Scholar 

  • Zhang J, Lin H, Doolittle J (2014) Soil layering and preferential flow impacts on seasonal changes of GPR signals in two contrasting soils. Geoderma 213:560–569

    Article  Google Scholar 

  • Zhao WZ, Liu B (2010) The response of sap flow in shrubs to rainfall pulses in the desert region of China. Agric Forest Meteorol 150:1297–1306

    Article  Google Scholar 

  • Zhou X, Lin HS, White EA (2008) Surface soil hydraulic properties in four soil series under different land uses and their temporal changes. Catena 73:180–188

    Article  Google Scholar 

Download references

Acknowledgments

This study was supported by National Science Fund for Distinguished Young Scholars (No. 41125002).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Wenzhi Zhao.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Yan, J., Zhao, W. Characteristics of preferential flow during simulated rainfall events in an arid region of China. Environ Earth Sci 75, 566 (2016). https://doi.org/10.1007/s12665-015-5101-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12665-015-5101-4

Keywords

Navigation