Application of X‐ray tomography to quantify macropore characteristics of loess soil under two perennial plants

European Journal of Soil Science - Tập 67 Số 3 - Trang 266-275 - 2016
T. C. Li1, M. A. Shao1,2, Yuhua Jia3,2
1College of Resources and Environment Northwest A&F University Yangling 712100 China
2Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
3College of Water Conservancy, Shenyang Agricultural University, Shenyang 110866, China

Tóm tắt

SummaryWith the advent of large‐scale restoration of vegetation in the Loess Plateau, northwest China, there has been an increase in concern about the suitability of loess soil to support permanent vegetation cover. The quantification of soil macropore characteristics could be critical in determining the architecture and hydrological processes of loess soil on the plateau. In this research, we compared the effects of Purple alfalfa (Medicago sativa L.) and Korshinsk peashrub (Caragana korshinskii K.) on the macropore characteristics of a soil profile on the plateau with computed tomography (CT). To achieve this, undisturbed cores of soil were excavated from beneath purple alfalfa (ALF), 22‐year‐old Korshinsk peashrub (KOP22) and 40‐year‐old Korshinsk peashrub (KOP40) vegetation types in the Liudaogou watershed for evaluation. The soil macropore characteristics (including macroporosity, largest pore area, amounts of macropores, circularity, surface area density, branch density, junction density and connectivity) were determined with image analysis software. Soil under KOP22 and KOP40 treatments had approximately the same amounts of macropores (17 per 6359‐mm2 area), which was three times greater than those under ALF plants. Macroporosity ratios of soil under KOP22 and KOP40 plants to that under ALF plants were 2.3 and 3.6, respectively. Compared with KOP22, KOP40 had a larger macroporosity and the largest pore area at the 100–300‐mm soil depth. The KOP plants, in particular KOP40, apparently improved the macropore network structure of the soil more than ALF. However, the macropores under ALF were much rounder at the 100–300‐mm soil depth than those under the other two plants. There was no correlation between macropore characteristics and organic matter content of the soil at 100–400‐mm depth. Nevertheless, macroporosity was strongly correlated with the largest pore area. The findings of this research are critical for developing strategies for the restoration of vegetation in the Loess Plateau through improvement of the hydrological process of loess soil.Highlights We examined macropore characteristics of loess soil on the Loess Plateau in China. We determined the effects of different plants on soil macropore characteristics. Soil under Korshinsk peashrub had better macropore structure than that under Purple alfalfa. Long‐term recovery of KOP benefits the macropore structure most on the northern Loess Plateau.

Từ khóa


Tài liệu tham khảo

10.1016/j.still.2011.06.002

10.1111/j.1365-2664.2008.01605.x

10.1016/j.geoderma.2007.10.013

10.1016/j.earscirev.2013.04.003

10.1016/j.geoderma.2005.09.002

10.1016/j.bone.2010.08.023

10.1016/j.geoderma.2010.02.010

FAO, 1989, Carte mondiale des sols. Légende révisée

10.1016/S0167-8809(02)00039-7

10.1016/j.geoderma.2008.12.016

10.1016/j.still.2014.12.019

10.1111/j.1365-2389.2007.00915.x

10.1016/j.catena.2011.12.008

10.1016/j.jhydrol.2014.07.043

10.1016/j.catena.2011.03.001

10.1016/j.geoderma.2010.09.030

10.1097/00010694-200203000-00001

10.1016/j.jaridenv.2005.04.005

10.5194/hess-13-1133-2009

Li W.Z., 2014, Characterization of aggregate microstructures of paddy soils under different patterns of fertilization with synchrotron radiation micro‐CT, Acta Pedologica Sinica, 51, 67

10.1016/j.jhydrol.2010.03.031

10.1016/j.geoderma.2012.02.024

10.1016/j.geoderma.2013.08.037

10.2136/sssaj2004.0312

Rasband W., 2002, NIH ImageJ

Ruan X.Z., 2015, Soil macropore characteristics of different wood land and their influencing factors on Simiansan mountain in Chongqing, Journal of Soil & Water Conservation, 29, 68

Scott H.D., 2000, Soil Physics: Agricultural and Environmental Applications

10.2136/sssaj2004.0280

10.1016/S0031-0182(02)00690-9

10.2136/sssaj2006.0307

10.2134/agronj1996.00021962008800050025x

Wan S.M., 2004, Study on root system development ability of alfalfa cultivars, Acta Botanica Boreali‐Occidentalia Sinica, 24, 2048

10.1016/j.jhydrol.2009.09.042

10.1016/j.jaridenv.2012.09.003

Wu X.W., 2007, Study on root system development ability and comparison of root and crown traits among alfalfa cultivar, Acta Agriculturae Boreali‐occidentalis Sinica, 16, 80

10.1016/j.catena.2014.03.016

Yang Y.H., 2013, Using computed tomography scanning to study soil pores under different soil structure improvement measures, Transactions of the Chinese Society of Agricultural Engineering, 29, 99

10.1007/s11430-010-0029-8

10.1016/j.landusepol.2008.11.006

10.1016/j.ecolind.2012.03.021