Abstract
Rock fragments have major effect on soil macropores and water movement. However, the characteristics of rock fragments and their relationship with macropore characteristics remain elusive in forest stony soils in northern mountainous area of China. The objectives of this study are to (1) use Industrial Computed Tomography (CT) scanning to quantitatively analyze rock fragment characteristics in intact soil columns in different forest lands and (2) identify the relationship between characteristics of rock fragments and that of the macropores. Intact soil columns that were 100 mm in diameter and 300 mm long were randomly taken from six local forest stony soils in Wuzuolou Forest Station in Miyun, Beijing. Industrial CT was used to scan all soil column samples, and then the scanned images were utilized to obtain the three-dimensional (3D) images of rock fragments and macropore structures. Next, the parameters of the rock fragments and macropore structure were measured, including the volume, diameter, surface area, and number of rock fragments, as well as the volume, diameter, surface area, length, angle, tortuosity and number of macropores. The results showed that no significant difference was found in soil rock fragments content in the 10-30 cm layer between mixed forest and pure forest, but in the 0-10 cm soil layer, the rock fragments in mixed forest were significantly less than in pure forest. The number density of macropores has significant negative correlation with the number of rock fragments in the 0-10 cm soil layer, whereas this correlation is not significant in 10-20 cm and 20-30 cm soil layers. The volume density of macropore was not correlated with the volume density of rock fragments, and there is no correlation between the density of macropore surface area and the density of rock fragment surface area. Industrial CT scanning combined with image processing technology can provide a better way to explore 3D distribution of rock fragments in soil. The content of rock fragments in soil is mainly determined by parent rocks. The surface soil (0-10 cm) of forest contains fewer rock fragments and more macropores, which may be caused by bioturbation, root systems, gravitational settling and faunal undermining.
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Aalders IH, Augustinus PGEF, Nobbe JM (1989) The contribution of ants to soil erosion: a reconnaissance survey. Catena 16: 4–5, 449–459. https://doi.org/10.1016/0341-8162(89)90027-1
Ahmad, Muhammad Arslan (2016) Quantifying relationships between X-ray imaged macropore structure and hydraulic conductivity. Second cycle, A2E. Uppsala: SLU, Dept. of Soil and Environment.
Balek CL (2002) Buried artifacts in stable upland sites and the role of bioturbation: a review. Geoarchaeology 17: 41–51. https://doi.org/10.1002/gea. 10002
Brakensiek DL, Rawls WJ (1994) Soil containing rock fragments: effects on infiltration. Catena 23(1–2): 99–110. https://doi.org/10.1016/-341-8162(94)90056-6
Bundt M, Widmer F, Pesaro M, et al. (2001) Preferential flow paths: biological ‘hot spots’ in soils. Soil Biology and Biochemistry 33(6): 729–738. https://doi.org/10.1016/S0038-0717(00)00218-2
Bunte K, Poesen J (1993) Effects of rock fragment covers on erosion and transport of noncohesive sediment by shallow overland flow. Water Resources Research 29(5): 1415–1424. https://doi.org/10.1029/92WR02706
Cerda A (2001) Effects of rock fragment cover on soil infiltration, inter-rill runoff and erosion. European Journal of Soil Science 52(1): 59–68. https://doi.org/10.1046/j.1365-2389.2001.00354.x
Cerda A, Jurgensen MF (2008) The influence of ants on soil and water losses from an orange orchard in eastern Spain. Journal of Applied Entomology 132(4): 306–314. https://doi.org/10.1111/j.1439-0418.2008.01267.x
Cerdà A, Jurgensen MF, Bodi MB (2009) Effects of Ants on Water and Soil Losses from Organically-Managed Citrus Orchards in Eastern Spain. Biologia 64 (3): 527–531. https://doi.org/10.2478/s11756-009-0114-7
Cerdà A, Jurgensen MF (2011) Ant Mounds as a Source of Sediment on Citrus Orchard Plantations in Eastern Spain. A Three-Scale Rainfall Simulation Approach. Catena 85 (3): 231–236. https://doi:10.1016/j.catena.2011.01.008
Dal Ferro N, Strozzi AG, Duwig C, et al. (2015) Application of smoothed particle hydrodynamics (SPH) and pore morphologic model to predict saturated water conductivity from X-ray CT imaging in a silty loam Cambisol. Geoderma 255: 27–34. https://doi.org/10.1016/j.geoderma.2015.04.019
Danalatos NG, Kosmas CS, Moustakas NC, et al. (1995) Rock fragments II. Their impact on soil physical properties and biomass production under Mediterranean conditions. Soil Use and Management 11: 121–126. https://doi.org/10.1111/j.1475-2743.1995.tb00509.x
De Figueiredo T, Poesen J (1998) Effects of surface rock fragment characteristics on inter-rill runoff and erosion of a silty loam soil. Soil and Tillage Research 46(1–2): 81–95. https://doi.org/10.1016/S0167-1987(98)80110-4
De Witte E (2003) Hydrofoberen van natuursteenherstelmortels-Anti-graffiti. Renovation Course. Session 3.
Descroix L, Viramontes D, Vauclin M (2001) Influence of soil surface features and vegetation on runoff and erosion in the Western Sierra Madre (Durango, Northwest Mexico). Catena 43(2): 115–135. https://doi.org/10.1016/S0341-8162(00)00124-7
Elyeznasni N, Sellami F, Pot V, et al. (2012) Exploration of soil micromorphology to identify coarse-sized OM assemblages in X-ray CT images of undisturbed cultivated soil cores. Geoderma 179: 38–45. https://doi.org/10.1016/j.geoderma. 2012.02.023
Eriksson CP, Holmgren P (1996) Estimating stone and boulder content in forest soils-evaluating the potential of surface penetration methods. Catena 28(1–2): 121–134. https://doi. org/10.1016/S0341-8162(96)00031-8
Flanagan DC, Nearing MA (1995) USDA-Water Erosion Prediction Project: Hillslope profile and watershed model documentation. Vol. 10. NSERL report.
Fao I, Isric I (2009) JRC: Harmonized World Soil Database (version 1.1). FAO, Rome, Italy and IIASA, Laxenburg, Austria
Fu SH (2005) Effect of soil containing rock fragment on infiltration. Journal of Soil and Water Conservation 19(1): 171–175.
Govers G, Van Oost K, Poesen J (2006) Responses of a semiarid landscape to human disturbance: a simulation study of the interaction between rock fragment cover, soil erosion and land use change. Geoderma 133(1): 19–31. https://doi.org/10.1016/j.geoderma.2006.03.034
Hendriks CMA, Bianchi FJJA (1995) Root density and root biomass in pure and mixed forest stands of Douglas-fir and beech. NJAS wageningen journal of life sciences 43(3): 321–331.
Hu X, Li ZC, Li XY, et al. (2016) Quantification of soil macropores under alpine vegetation using computed tomography in the Qinghai Lake Watershed, NE Qinghai–Tibet Plateau. Geoderma 264 (Part A): 244–251. https://doi.org/10.1016/j.geoderma.2015.11.001
Hu X, Li ZC, Li XY, Liu LY (2015) Influence of shrub encroachment on CT-measured soil macropore characteristics in the Inner Mongolia grassland of northern China. Soil and Tillage Research 150: 1–9. https://doi.org/10.1016/j.still. 2014.12.019
Ingelmo F, Cuadrado S, Ibaez A, et al. (1994) Hernandez J. Hydric properties of some Spanish soils in relation to their rock fragment content: implications for runoff and vegetation. Catena 23: 73–85. https://doi.org/10.1016/0341-8162 (94)90054-X
Ji Y, Baud P, Wong T (2016) Characterization of Pore Geometry in Limestones Using X-ray Computed Microtomography. 78th EAGE Conference and Exhibition 2016. https://doi.org/10.3997/2214-4609.201600892
Johnson DL (1990) Biomantle evolution and the redistribution of earth materials and artifacts. Soil Science 149: 84–102.
Keesstra SD, Quinton JN, Vander Putten WH, et al. (2016) The significance of soils and soil science towards realization of the United Nations Sustainable Development Goals. Soil 2(2): 111–118. https://doi:10.5194/soil-2-111-2016
Leigh D (1998) Evaluating artifact burial by eolian versus bioturbation processes, South Carolina sand hills, USA. Geoarchaeology 13(3): 309–330. https://doi.org/10.1002/(SICI) 1520-6548(199802)13:3<309::AID-GEA4>3.0.CO;2-8.
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(3): 266–275. https://doi.org/10.1111/ejss.12330
Luo L, Lin H, Li S (2010) Quantification of 3-D soil macropore networks in different soil types and land uses using computed tomography. Journal of Hydrology 393(1–2): 53–64. https://doi.org/10.1016/j.jhydrol.2010.03.031
Masselink R, Temme AJAM, Giménez R, et al. (2017) Assessing hillslope-channel connectivity in an agricultural catchment using rare-earth oxide tracers and random forests models. Cuadernos de Investigación Geográfica. http://doi.org/10.18172/cig.3169
Mekonnen M, Keesstra SD, Baartman JE, et al. (2017) Reducing Sediment Connectivity Through man-Made and Natural Sediment Sinks in the Minizr Catchment, Northwest Ethiopia. Land Degradation & Development 28(2): 708–717. https://doi.org/10.1002/ldr.2629
Meng C, Niu J, Li X, et al. (2016) Quantifying soil macropore networks in different forest communities using industrial computed tomography in a mountainous area of North China. Journal of Soils and Sediments 17(9): 2357–2370. https://doi.org/10.1007/s11368-016-1441-2.
Miller FT, Guthrie RL (1984) Classification and distribution of soils containing rock fragments in the United States. Soil Science Society of America 13: 1–6.
Mol G, Keesstra SD (2012) Soil science in a changing world. Current Opinions in Environmental Sustainability 4: 473–477.
Muñoz-Ortega FJ, Martínez FS, Monreal FC (2015) Volume, surface, connectivity and size distribution of soil pore space in CT images: Comparison of samples at different depths from nearby natural and tillage areas. Pure and Applied Geophysics 172(1): 167–179. https://doi.org/10.1007/s00024-014-0897-5
Ni XM, Miao J, Lv RS, et al. (2017) Quantitative 3D spatial characterization and flow simulation of coal macropores based on CT technology. Fuel 200: 199–207. https://doi.org/10.1016/j.fuel.2017.03.068
Parsons AJ, Bracken L, Peoppl R, et al. (2015) Connectivity in water and sediment dynamics. In press in Earth Surface Processes and Landforms. https://doi.org/10.1002/esp.3714
Perez FL (1998) Conservation of soil moisture by different stone covers on alpine talus slopes (Lassen, California). Catena 33(3–4): 155–177. https://doi.org/10.1016/S0341-8162(98)00091-5
Phillips JD, Luckow K, Marion DA, et al. (2005) Rock fragment distributions and regolith evolution in the Ouachita Mountains, Arkansas, USA. Earth Surface Processes and Landforms 30(4): 429–442. https://doi.org/10.1002/esp.1152
Qiao JC, Zeng JH, Yang ZF, et al. (2015) The Nano–Macro Pore Network and the Characteristics of Petroleum Migration and Accumulation in Chang 8 Tight Sandstone Reservoir in Heshui, Ordos Basin. Acta Geologica Sinica (English Edition) 89(s1): 207–209. https://doi.org/10.1111/1755-6724.12303_23
Rodrigo comino JR, Quiquerez A, Follain S, et al. (2016) Soil erosion in sloping vineyards assessed by using botanical indicators and sediment collectors in the Ruwer-Mosel valley. Agriculture, Ecosystems & Environment 233: 158–170. https://doi.org/10.1016/j.agee.2016.09.009
Rodrigo comino J, García Díaz A, Brevik EC, et al. (2017). Role of rock fragment cover on runoff generation and sediment yield in tilled vineyards. European Journal of Soil Science. https://doi.org/10.1111/ejss.12483
Shi ZJ, Xu LH, Wang YH, Yet al. (2012) Effect of rock fragments on macropores and water effluent in a forest soil in the stony mountains of the Loess Plateau, China. African Journal of Biotechnology 11(39): 9350–9361. https://doi.org/10.5897/AJB12.1450
Stewart JB, Moran CJ, Wood JT (1999) Macropore sheath: quantification of plant root and soil macropore association. Plant and Soil 211(1): 59–67. https://doi.org/10.1023/A:1004405422847
Torri D, Poesen J, Monaci F, et al. (1994) Rock fragment content and fine soil bulk density. Catena 23(1–2): 65–71. https://doi.org/10.1016/0341-8162(94)90053-1
Valentin C (1994) Surface sealing as affected by various rock fragment covers in West Africa. Catena 23(1–2): 87–97. https://doi.org/10.1016/0341-8162(94)90055-8
Walmsley A, Cerdà A (2017) Soil macrofauna and organic matter in irrigated orchards under Mediterranean climate. Biological Agriculture & Horticulture 1-11. https://doi.org/10.1080/01448765.2017.1336486
Wang J, Guo L, Bai Z, et al. (2016) Using computed tomography (CT) images and multi-fractal theory to quantify the pore distribution of reconstructed soils during ecological restoration in opencast coal-mine. Ecological Engineering 92: 148–157. https://doi.org/10.1016/j.ecoleng.2016.03.029
Yan H, Li K, Ding H, et al. (2011) Root morphological and proteomic responses to growth restriction in maize plants supplied with sufficient N. Journal of plant physiology 168(10): 1067–1075. https://doi.org/10.1016/j.jplph.2010.12.018
Yang JL, Zhang GL (2011) Water infiltration in urban soils and its effects on the quantity and quality of runoff. Journal of soils and sediments 11(5): 751–761. https://doi.org/10.1007/s11368-011-0356-1
Zhang Z, Lin L, Wang Y, et al. (2015) Temporal change in soil macropores measured using tension infiltrometer under different land uses and slope positions in subtropical China. Journal Soil Sediment 16(3):854–863. https://doi.org/10.1007/s11368-015-1295-z
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The research reported in this manuscript is funded by the Natural Science Foundation of China (Grants No. 41741024 and 41271044) and Beijing Municipal Education Commission.
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Meng, C., Niu, Jz., Yin, Zc. et al. Characteristics of rock fragments in different forest stony soil and its relationship with macropore characteristics in mountain area, northern China. J. Mt. Sci. 15, 519–531 (2018). https://doi.org/10.1007/s11629-017-4638-y
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DOI: https://doi.org/10.1007/s11629-017-4638-y