Recovery of saturated hydraulic conductivity along a forest successional series from abandoned land to mature, evergreen broad-leaved forest in eastern China

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Contents Vol 50(4)

doi:10.1071/SR11149

Soil, Land Care & Environmental Research

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Recovery of saturated hydraulic conductivity along a forest successional series from abandoned land to mature, evergreen broad-leaved forest in eastern China

Shun Lei Peng ^A , Jian Wu ^A ^B and Wen Hui You ^A ^C

^A Department of Environmental Science and Technology, East China Normal University, Shanghai, 200062, China.
^B Shanghai Academy of Environmental Sciences, Shanghai, 200233, China.
^C Corresponding author. Email: youwh@yjsy.ecnu.edu.cn

Soil Research 50(4) 257-266 http://dx.doi.org/10.1071/SR11149
Submitted: 20 June 2011 Accepted: 1 May 2012 Published: 3 July 2012





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Abstract

Saturated hydraulic conductivity (K_s) can be used to indicate changes in soil hydrology resulting from vegetation succession. A constant-head permeameter was used to investigate differences in K_s at five soil depths (10, 20, 40, 60, and 80 cm) along a successional sequence of 155 years in evergreen broad-leaved forest at Tiantong National Forest Park, eastern China. The following six forest successional classes were studied: climax evergreen broad-leaved forest (CE), sub-climax evergreen broad-leaved forest (SE), evergreen broad-leaved mixed coniferous forest (MF), coniferous forest (CF), secondary shrub (SS), and abandoned land (AL). Surface K_s (the geometric mean of K_s at 10 and 20 cm soil depths) significantly increased from AL to CE but declined in CF. The surface K_s value under CE was higher than under other successional stages (CE 271 mm h^–1, AL 58 mm h^–1, SS 124 mm h^–1, CF 90 mm h^–1, MF 170 mm h^–1, SE 231 mm h^–1), and was 4.7 times greater than under AL, 2.2 times greater than under SS, and 3.0 times greater than under CF, but showed no significant difference from SE (P > 0.05). Vertical difference of K_s was detected up to a soil depth of 40 cm along forest successional series. Macroporosity was the main determining factor and played an important role in the process of K_s recovery. The likelihood of overland flow generation was inferred by comparing K_s at soil depths of 10, 20, 40, and 60 cm under the various successional stages at prevailing storm intensities. Overland flow was most likely to occur in the early successional stages. This study suggests that K_s could be restored to climax forest levels along forest successional series, but the recovery time could be as long as 95 years.

Additional keywords: ecosystem service, infiltration, land use, macroporosity, overland flow, soil hydrology.

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