Abstract
In order to investigate the differences of macropores vertical distribution under different surface plants, and to assess the influences of root systems, organic matter and texture on macropore flow paths, two dye tracer infiltration experiments were performed in slopes under two different plants (Campylotropis polyantha (Franch.) Schindl vs. Cynodon dactylon (Linn.) Pers). Dye tracer infiltration experiments with field observations and measurements of soil properties were combined. Results show that the discrepancy in macropores distribution between two slopes under different plants is significant. Root systems have significant effects on macropore flow paths distribution and the effect become more pronounced as the diameter of roots become larger. Organic matter and stone are important factors to affect macropores distribution. Root-soil interface, inter-aggregate macropore and stone-soil interface are important macropore flow paths in well vegetated slopes.
Similar content being viewed by others
References
WANG Lan-min, WU Zhi-jian, WANG Ping, CHEN Tuo. Characteristics, causation, and rehabilitation of Zhouqu extraordinarily serious debris flows in 2010, China [J]. Journal of Central South University of Technology, 2013, 20(8): 2342–2348.
CHIANG S H, CHANG K T. The potential impact of climate change on typhoon-triggered landslides in Taiwan, 2010-2099 [J]. Geomorphology, 2011, 133(3): 143–151
GUZZETTI F, PERUCCACCI S, ROSSI M, STARK C P. The rainfall intensity–duration control of shallow landslides and debris flows: An update [J]. Landslides, 2008, 5(1): 3–17.
NOBLES M M, WILDING L P, LIN H S. Flow pathways of bromide and brilliant blue FCF tracers in caliche soils [J]. Journal of Hydrology, 2010, 393(1): 114–122.
SCHWÄRZEL K, EBERMANN S, SCHALLING N. Evidence of double-funneling effect of beech trees by visualization of flow [J]. Journal of Hydrology, 2012, 470: 184–192.
UCHIDA T, KOSUGI K, MIZUYAMA T. Effects of pipeflow on hydrological process and its relation to landslide: A review of pipeflow studies in forested headwater catchments [J]. Hydrological Processes, 2001, 15(11): 2151–2174.
ANDERSON E, WEILER M, ALILA Y, HUDSON R O. Dye staining and excavation of a lateral preferential flow network [J]. Hydrology and Earth System Sciences, 2009, 13(6): 935–944.
WANG K, ZHANG R D. Heterogeneous soil water flow and macropores described with combined tracers of dye and iodine [J]. Journal of Hydrology, 2011, 397(1): 105–117.
ALAOUI A, GOETZ B. Dye tracer and infiltration experiments to investigate macropore flow [J]. Geoderma, 2008, 144(1): 279–286.
BOUMA J, JONGERIUS A, BOERSMA O, JAGER A, SCHOONDERBEEK D. The function of different types of macropores during saturated flow through four swelling soil horizons [J]. Soil Science Society of America Journal, 1977, 41(5): 945–950.
NOGUCHI S, NIK A R, KASRAN B, TANI M, SAMMORI T, MORISADE K. Soil physical properties and preferential flow pathways in tropical rain forest [J]. Journal of Forest Research, 1997, 2(2): 115–120.
WEILER M, FLÜHLER H. Inferring flow types from dye patterns in macroporous soils [J]. Geoderma, 2004, 120(1): 137–153.
BOGNER C, WOLF B, SCHLATHER M, HUWE B. Analysing flow patterns from dye tracer experiments in a forest soil using extreme value statistics [J]. European Journal of Soil Science, 2008, 59(1): 103–113.
SCHLATHER M, HUWE B. A risk index for characterising flow pattern in soils using dye tracer distributions [J]. Journal of Contaminant Hydrology, 2005, 79(1): 25–44.
DEVITT D A, SMITH S D. Root channel macropores enhance downward movement of water in a Mojave Desert ecosystem [J]. Journal of Arid Environments, 2002, 50(1): 99–108.
GRAHAM C B, WOODS R A, MCDONNELL J J. Hillslope threshold response to rainfall: (1) A field based forensic approach [J]. Journal of Hydrology, 2010, 393(1): 65–76.
KASTEEL R, GARNIER P, VACHIER P, COQUET Y. Dye tracer infiltration in the plough layer after straw incorporation [J]. Geoderma, 2007, 137(3): 360–369.
HANGEN R, GERKE H H, SCHAAF W, HÜTTL R F. Flow path visualization in a lignitic mine soil using iodine–starch staining [J]. Geoderma, 2004, 120(1): 121–135.
KEITH D M, JOHNSON E A, VALEO C. A hillslope forest floor (duff) water budget and the transition to local control [J]. Hydrological Processes, 2010, 24(19): 2738–2751.
KEITH D M, JOHNSON E A, VALEO C. Moisture cycles of the forest floor organic layer (F and H layers) during drying [J]. Water Resources Research, 2010, 46(7): 1–14.
LAUREN A, MANNERKOSKI H. Hydraulic properties of mor layers in Finland [J]. Scandinavian Journal of Forest Research, 2001, 16(5): 429–441.
GUEVARA-ESCOBAR A, GONZÁLEZ-SOSA E, RAMOSSALINAS M, HERNANDEZ-DELGADO G D. Experimental analysis of drainage and water storage of litter layers [J]. Hydrology and Earth System Sciences, 2007, 11(5): 1703–1716.
DESCROIX L, VIRAMONTES D, VAUCLIN M, GONZALEZ BARRIOS J L, ESTEVES M. Influence of soil surface features and vegetation on runoff and erosion in the Western Sierra Madre (Durango, Northwest Mexico) [J]. Catena, 2001, 43(2): 115–135.
NERIS J, TEJEDOR M, RODRIGUEZ M, FUENTES J, JIMÉNEZ C. Effect of forest floor characteristics on water repellency, infiltration, runoff and soil loss in Andisols of Tenerife (Canary Islands, Spain) [J]. Catena, 2013, 108: 50–57.
AUBERTIN G M. Nature and extent of macropores in forest soils and their influence on subsurface water movement [M]. Forest Service, Broomall, PA: Northeastern Forest Experiment Station, 1971.
LAMANDÉ M, LABOURIAU R, HOLMSTRUP M, TORP S B, GREVE M H, HECKRATH G, IVERSEN B V, de JONGER L W, MOLDRUP P, JACOBSEN O H. Density of macropores as related to soil and earthworm community parameters in cultivated grasslands [J]. Geoderma, 2011, 162(3): 319–326.
PETH S, HORM R, BECHMANN F, DONATH T, FISCHER J, SMUCKER A J M. Three-dimensional quantification of intraaggregate pore-space features using synchrotron-radiation-based microtomography [J]. Soil Science Society of America Journal, 2008, 72(4): 897–907.
PASSIOURA J B. Soil conditions and plant growth [J]. Plant, Cell & Environment, 2002, 25(2): 311–318.
SIX J, BOSSUYT H, DEGRYZE S, DENEF K. A history of research on the link between (micro) aggregates, soil biota, and soil organic matter dynamics [J]. Soil and Tillage Research, 2004, 79(1): 7–31.
SAHA D, KUKAL S S, SHARMA S. Landuse impacts on SOC fractions and aggregate stability in typic ustochrepts of Northwest India [J]. Plant and Soil, 2011, 339(1-2): 457–470.
OADES J M, WATERS A G. Aggregate hierarchy in soils [J]. Soil Research, 1991, 29(6): 815–828.
BOSSUYT H, DENEF K, SIX J, FREY S D, MERCKX R, PAUSTIAN K. Influence of microbial populations and residue quality on aggregate stability [J]. Applied Soil Ecology, 2001, 16(3): 195–208.
ALAGÖZ Z, YILMAZ E. Effects of different sources of organic matter on soil aggregate formation and stability: A laboratory study on a lithic rhodoxeralf from Turkey [J]. Soil and Tillage Research, 2009, 103(2): 419–424.
JARVIS N J. A review of non-equilibrium water flow and solute transport in soil macropores: Principles, controlling factors and consequences for water quality [J]. European Journal of Soil Science, 2007, 58(3): 523–546.
SAUER T J, LOGSDON S D. Hydraulic and physical properties of stony soils in a small watershed [J]. Soil Science Society of America Journal, 2002, 66(6): 1947–1956.
LAINE-KAULIO H. Development and analysis of a dualpermeability model for subsurface stormflow and solute transport in a forested hillslope [D]. Aalto: Aalto University, 2011.
WEILER M H. Mechanisms controlling macropore flow during infiltration [D]. Freiburg: Albert-Ludwigs University of Freiburg, 2001.
Author information
Authors and Affiliations
Corresponding author
Additional information
Foundation item: Project(U1502232) supported by the National Natural Science Foundation of China-Yunan Joint Fund; Project(KKSY201406009) supported by the Natural Science Foundation of Kunming University of Science and Technology, China; Project(2014FD007) supported by the Natural Science Foundation of Yunnan Province, China
Rights and permissions
About this article
Cite this article
Zhang, Jm., Xu, Zm. Dye tracer infiltration technique to investigate macropore flow paths in Maka Mountain, Yunnan Province, China. J. Cent. South Univ. 23, 2101–2109 (2016). https://doi.org/10.1007/s11771-016-3266-y
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11771-016-3266-y