Characterising macropores and preferential flow of mountainous forest soils with contrasting human disturbances
Jun Yi A , Ye Yang A , Muxing Liu
A D , Wei Hu B D , Shulan Lou A , Hailin Zhang A and Dongyou Zhang C
+ Author Affiliations
- Author Affiliations
A Hubei Province Key Laboratory for Geographical Process Analysis and Simulation, Central China Normal University, Wuhan 430079, China.
B New Zealand Institute for Plant & Food Research Limited, Private Bag 4704, Christchurch 8140, New Zealand.
C Department of Imaging, Wuhan First Hospital, Wuhan 430079, China.
D Corresponding authors. Email: liumuxing@mail.ccnu.edu.cn; Wei.Hu@plantandfood.co.nz
Soil Research 57(6) 601-614 https://doi.org/10.1071/SR18198
Submitted: 15 July 2018 Accepted: 31 March 2019 Published: 13 June 2019
Abstract
Preferential flow can develop in soil macropores, and macropores are sensitive to human disturbances. This study investigated soil macropore features and the main factors controlling preferential flow at four sites with different levels of human disturbance in a mountainous area in Central China. The level of human disturbance decreased with increasing elevation, with the lowest elevation areas covered with coniferous trees (LF) > middle mountain areas covered with tea gardens (TG) > middle mountain areas covered with deciduous trees and mixed shrubs (MF) > subalpine areas covered with evergreen coniferous trees (HF). At each site, the soil macropore structure at 0–20 cm soil depth was analysed using computed tomography scans (0.6 mm resolution) and Image J software. Preferential flow was determined by analysing the breakthrough curve (BTC) of nitrate. The macroporosity, surface area density, mean macropore size, macropore number density, length density and node density were all ranked in the order of HF ≥ MF ≥ TG = LF. Less disturbed sites had stronger evidence of preferential flow as shown by faster breakthrough, longer tails and greater asymmetry of the BTCs. There were significant (P < 0.05) positive influences of soil macropore properties on pore water velocity and the solute dispersion coefficient. The dispersivity parameter was mainly affected by the macropore equivalent hydraulic radius. This study showed that human disturbance in the mountain forest areas significantly decreased soil macropores by changing soil physical properties (e.g. bulk density, texture and soil organic matter content) and root distribution, thus increasing the risk of surface runoff and nutrient losses.
Additional keywords: breakthrough curve, CDE equation, computed tomography, MIM model, root distribution, soil physical properties.
References
Allaire SE, Roulier S, Cessna AJ (2009) Quantifying preferential flow in soils: A review of different techniques. Journal of Hydrology 378, 179–204.| Quantifying preferential flow in soils: A review of different techniques.Crossref | GoogleScholarGoogle Scholar |
Anderson SH, Peyton RL, Gantzer CJ (1990) Evaluation of Constructed and Natural Soil Macropores Using X-Ray Computed-Tomography. Geoderma 46, 13–29.
| Evaluation of Constructed and Natural Soil Macropores Using X-Ray Computed-Tomography.Crossref | GoogleScholarGoogle Scholar |
Angulo-Jaramillo R, Vandervaere JP, Roulier S, Thony JL, Gaudet JP, Vauclin M (2000) Field measurement of soil surface hydraulic properties by disc and ring infiltrometers - A review and recent developments. Soil & Tillage Research 55, 1–29.
| Field measurement of soil surface hydraulic properties by disc and ring infiltrometers - A review and recent developments.Crossref | GoogleScholarGoogle Scholar |
Beven K, Germann P (1982) Macropores and water-flow in soils. Water Resources Research 18, 1311–1325.
| Macropores and water-flow in soils.Crossref | GoogleScholarGoogle Scholar |
Beven K, Germann P (2013) Macropores and water flow in soils revisited. Water Resources Research 49, 3071–3092.
| Macropores and water flow in soils revisited.Crossref | GoogleScholarGoogle Scholar |
Cnudde V, Boone MN (2013) High-resolution X-ray computed tomography in geosciences: a review of the current technology and applications. Earth-Science Reviews 123, 1–17.
| High-resolution X-ray computed tomography in geosciences: a review of the current technology and applications.Crossref | GoogleScholarGoogle Scholar |
Cnudde V, Masschaele B, Dierick M, Vlassenbroeck J, Van Hoorebeke L, Jacobs P (2006) Recent progress in X-ray CT as a geosciences tool. Applied Geochemistry 21, 826–832.
| Recent progress in X-ray CT as a geosciences tool.Crossref | GoogleScholarGoogle Scholar |
Doube M, Kłosowski MM, Arganda-Carreras I, Cordelières FP, Dougherty RP, Jackson JS, Schmid B, Hutchinson JR, Shefelbine SJ (2010) BoneJ: free and extensible bone image analysis in ImageJ. Bone 47, 1076–1079.
| BoneJ: free and extensible bone image analysis in ImageJ.Crossref | GoogleScholarGoogle Scholar | 20817052PubMed |
Gantzer CJ, Anderson SH (2002) Computed tomographic measurement of macroporosity in chisel-disk and no-tillage seedbeds. Soil & Tillage Research 64, 101–111.
| Computed tomographic measurement of macroporosity in chisel-disk and no-tillage seedbeds.Crossref | GoogleScholarGoogle Scholar |
Hardie MA, Doyle RB, Cotching WE, Mattern K, Lisson S (2012) Influence of antecedent soil moisture on hydraulic conductivity in a series of texture-contrast soils. Hydrological Processes 26, 3079–3091.
| Influence of antecedent soil moisture on hydraulic conductivity in a series of texture-contrast soils.Crossref | GoogleScholarGoogle Scholar |
Heijs AWJ, Delange J, Schoute JFT, Bouma J (1995) Computed-tomography as a tool for nondestructive analysis of flow patterns in macroporous clay soils. Geoderma 64, 183–196.
| Computed-tomography as a tool for nondestructive analysis of flow patterns in macroporous clay soils.Crossref | GoogleScholarGoogle Scholar |
Hu X, Li Z-C, Li X-Y, Liu Y (2015) Influence of shrub encroachment on CT-measured soil macropore characteristics in the Inner Mongolia grassland of northern China. Soil & Tillage Research 150, 1–9.
| Influence of shrub encroachment on CT-measured soil macropore characteristics in the Inner Mongolia grassland of northern China.Crossref | GoogleScholarGoogle Scholar |
Jarvis N, Koestel J, Larsbo M (2016) Understanding preferential flow in the vadose zone: recent advances and future prospects. Vadose Zone Journal 15, 11
| Understanding preferential flow in the vadose zone: recent advances and future prospects.Crossref | GoogleScholarGoogle Scholar |
Kohne JM, Kohne S, Simunek J (2009) A review of model applications for structured soils: a) water flow and tracer transport. Journal of Contaminant Hydrology 104, 4–35.
| A review of model applications for structured soils: a) water flow and tracer transport.Crossref | GoogleScholarGoogle Scholar | 19012994PubMed |
Laine-Kaulio H, Backnäs S, Koivusalo H, Laurén A (2015) Dye tracer visualization of flow patterns and pathways in glacial sandy till at a boreal forest hillslope. Geoderma 259–260, 23–34.
| Dye tracer visualization of flow patterns and pathways in glacial sandy till at a boreal forest hillslope.Crossref | GoogleScholarGoogle 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. Hydrology and Earth System Sciences 13, 1133–1144.
| Connecting ecohydrology and hydropedology in desert shrubs: stemflow as a source of preferential flow in soils.Crossref | GoogleScholarGoogle Scholar |
Li TC, Shao MA, Jia YH (2016) Application of X-ray tomography to quantify macropore characteristics of loess soil under two perennial plants. European Journal of Soil Science 67, 266–275.
| Application of X-ray tomography to quantify macropore characteristics of loess soil under two perennial plants.Crossref | GoogleScholarGoogle Scholar |
Liu H, Forsmann DM, Kjærgaard C, Saki H, Lennartz B (2017) Solute transport properties of fen peat differing in organic matter content. Journal of Environmental Quality 46, 1106–1113.
| Solute transport properties of fen peat differing in organic matter content.Crossref | GoogleScholarGoogle Scholar | 28991978PubMed |
Liu MX, Guo L, Y J, Lin H, Lou SL, Zhang HL, Li T (2018) Characterizing preferential flow and its interaction with the soil matrix using dye tracing in the Three Gorges Reservoir Area of China. Soil Research
| Characterizing preferential flow and its interaction with the soil matrix using dye tracing in the Three Gorges Reservoir Area of China.Crossref | GoogleScholarGoogle Scholar |
Luo L, Lin H, Halleck P (2008) Quantifying soil structure and preferential flow in intact soil using X-ray computed tomography. Soil Science Society of America Journal 72, 1058–1069.
| Quantifying soil structure and preferential flow in intact soil using X-ray computed tomography.Crossref | GoogleScholarGoogle Scholar |
Luo L, Lin H, Li S (2010a) Quantification of 3-D soil macropore networks in different soil types and land uses using computed tomography. Journal of Hydrology 393, 53–64.
| Quantification of 3-D soil macropore networks in different soil types and land uses using computed tomography.Crossref | GoogleScholarGoogle Scholar |
Luo LF, Lin H, Schmidt J (2010b) Quantitative relationships between soil macropore characteristics and preferential flow and transport. Soil Science Society of America Journal 74, 1929–1937.
| Quantitative relationships between soil macropore characteristics and preferential flow and transport.Crossref | GoogleScholarGoogle Scholar |
Luxmoore RJ, Jardine PM, Wilson GV, Jones JR, Zelazny LW (1990) Physical and chemical controls of preferred path flow through a forested hillslope. Geoderma 46, 139–154.
| Physical and chemical controls of preferred path flow through a forested hillslope.Crossref | GoogleScholarGoogle Scholar |
Muller K, Katuwal S, Young I, McLeod M, Moldrup P, de Jonge LW, Clothier B (2018) Characterising and linking X-ray CT derived macroporosity parameters to infiltration in soils with contrasting structures. Geoderma 313, 82–91.
| Characterising and linking X-ray CT derived macroporosity parameters to infiltration in soils with contrasting structures.Crossref | GoogleScholarGoogle Scholar |
Naveed M, Moldrup P, Arthur E, Wildenschild D, Eden M, Lamand M, Vogel HJ, de Jonge LW (2013) Revealing soil structure and functional macroporosity along a clay gradient using X-ray computed tomography. Soil Science Society of America Journal 77, 403–411.
| Revealing soil structure and functional macroporosity along a clay gradient using X-ray computed tomography.Crossref | GoogleScholarGoogle Scholar |
Peyton RL, Gantzer CJ, Anderson SH, Haeffner BA, Pfeifer P (1994) Fractal dimension to describe soil macropore structure using X-ray computed-tomography. Water Resources Research 30, 691–700.
| Fractal dimension to describe soil macropore structure using X-ray computed-tomography.Crossref | GoogleScholarGoogle Scholar |
Qiao J, Zhu Y, Jia X, Huang L, Ma S (2018) Estimating the spatial relationships between soil hydraulic properties and soil physical properties in the critical zone (0–100m) on the Loess Plateau, China: a state-space modeling approach. Catena 160, 385–393.
| Estimating the spatial relationships between soil hydraulic properties and soil physical properties in the critical zone (0–100m) on the Loess Plateau, China: a state-space modeling approach.Crossref | GoogleScholarGoogle Scholar |
Rab MA, Haling RE, Aarons SR, Hannah M, Young IM, Gibson D (2014) Evaluation of X-ray computed tomography for quantifying macroporosity of loamy pasture soils. Geoderma 213, 460–470.
| Evaluation of X-ray computed tomography for quantifying macroporosity of loamy pasture soils.Crossref | GoogleScholarGoogle Scholar |
Schindelin J, Arganda-Carreras I, Frise E, Kaynig V, Longair M, Pietzsch T, Preibisch S, Rueden C, Saalfeld S, Schmid B, Tinevez JY, White DJ, Hartenstein V, Eliceiri K, Tomancak P, Cardona A (2012) Fiji: an open-source platform for biological-image analysis. Nature Methods 9, 676–682.
| Fiji: an open-source platform for biological-image analysis.Crossref | GoogleScholarGoogle Scholar | 22743772PubMed |
Seobi T, Anderson SH, Udawatta RP, Gantzer CJ (2005) Influence of grass and agroforestry buffer strips on soil hydraulic properties for an Albaqualf. Soil Science Society of America Journal 69, 893–901.
| Influence of grass and agroforestry buffer strips on soil hydraulic properties for an Albaqualf.Crossref | GoogleScholarGoogle Scholar |
Toride N, Leij FJ, Van Genuchten MT (1995) ‘The CXTFIT code for estimating transport parameters from laboratory or field tracer experiments.’ (US Salinity Laboratory: Riverside, USA)
Udawatta RP, Anderson SH, Gantzer CJ, Garrett HE (2006) Agroforestry and grass buffer influence on macropore characteristics: a computed tomography analysis. Soil Science Society of America Journal 70, 1763–1773.
| Agroforestry and grass buffer influence on macropore characteristics: a computed tomography analysis.Crossref | GoogleScholarGoogle Scholar |
Valocchi AJ (1985) Validity of the local equilibrium assumption for modeling sorbing solute transport through homogeneous soils. Water Resources Research 21, 808–820.
| Validity of the local equilibrium assumption for modeling sorbing solute transport through homogeneous soils.Crossref | GoogleScholarGoogle Scholar |
Vervoort RW, Radcliffe DE, West LT (1999) Soil structure development and preferential solute flow. Water Resources Research 35, 913–928.
| Soil structure development and preferential solute flow.Crossref | GoogleScholarGoogle Scholar |
Walkley A, Black IA (1934) An examination of the Degtjareff method for determining soil organic matter and a proposed modification of the chromic acid titration method. Soil Science 37, 29–38.
| An examination of the Degtjareff method for determining soil organic matter and a proposed modification of the chromic acid titration method.Crossref | GoogleScholarGoogle Scholar |
Warner GS, Nieber JL, Moore ID, Geise RA (1989) Characterizing macropores in soil by computed-tomography. Soil Science Society of America Journal 53, 653–660.
| Characterizing macropores in soil by computed-tomography.Crossref | GoogleScholarGoogle Scholar |
Yang KJ, Lu CH (2018) Evaluation of land-use change effects on runoff and soil erosion of a hilly basin the Yanhe River in the Chinese Loess Plateau. Land Degradation & Development 29, 1211–1221.
| Evaluation of land-use change effects on runoff and soil erosion of a hilly basin the Yanhe River in the Chinese Loess Plateau.Crossref | GoogleScholarGoogle Scholar |
Zhang ZB, Zhou H, Zhao QG, Lin H, Peng X (2014) Characteristics of cracks in two paddy soils and their impacts on preferential flow. Geoderma 228–229, 114–121.
| Characteristics of cracks in two paddy soils and their impacts on preferential flow.Crossref | GoogleScholarGoogle Scholar |
Zhang ZB, Peng X, Zhou H, Lin H, Sun H (2015) Characterizing preferential flow in cracked paddy soils using computed tomography and breakthrough curve. Soil & Tillage Research 146, 53–65.
| Characterizing preferential flow in cracked paddy soils using computed tomography and breakthrough curve.Crossref | GoogleScholarGoogle Scholar |
Zhang Y, Zhao W, Fu L (2017) Soil macropore characteristics following conversion of native desert soils to irrigated croplands in a desert-oasis ecotone, Northwest China. Soil & Tillage Research 168, 176–186.
| Soil macropore characteristics following conversion of native desert soils to irrigated croplands in a desert-oasis ecotone, Northwest China.Crossref | GoogleScholarGoogle Scholar |
Zhou H, Mooney SJ, Peng XH (2017) Bimodal soil pore structure investigated by a combined soil water retention curve and X-ray computed tomography approach. Soil Science Society of America Journal 81, 1270–1278.
| Bimodal soil pore structure investigated by a combined soil water retention curve and X-ray computed tomography approach.Crossref | GoogleScholarGoogle Scholar |
