4.5 Article

Field study on influence of root characteristics on soil suction distribution in slopes vegetated with Cynodon dactylon and Schefflera heptaphylla

Journal

EARTH SURFACE PROCESSES AND LANDFORMS
Volume 40, Issue 12, Pages 1631-1643

Publisher

WILEY
DOI: 10.1002/esp.3743

Keywords

soil suction; vegetated slopes; root area index; root biomass; Cynodon dactylon; Schefflera heptaphylla

Funding

  1. National Basic Research Program (973 Program) by the Ministry of Science and Technology of the People's Republic of China [2012CB719805, 2012CB719800]
  2. Research Grants Council (RGC) of the Hong Kong Special Administrative Region [HKUST9/CRF/09, HKUST6/CRF/12R]
  3. Hong Kong PhD Fellowship Scheme (HKPFS)
  4. Hong Kong Observatory (HKO)

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Vegetation evapotranspiration (ET) induced soil water suction reduces hydraulic conductivity and increases shear strength of slopes. Several field studies have been conducted to investigate suction distribution in vegetated slopes. However, these studies were conducted on natural slopes, which are prone to heterogeneity in vegetation and soil conditions. Moreover, studies quantifying the effect of different vegetation species, root characteristics (root depth and root area index) and transpiration reduction function (T-rf) on suction in slopes under natural variation are rare. This study investigated the suction distribution and root characteristics in recompacted slopes vegetated with two different species, i.e. Cynodon dactylon (Bermuda grass) and Schefflera heptaphylla (ivy tree). Bare slope served as a control. Suction distributions during different seasons and rainfall events were monitored. It is found that during the dry season, slope vegetated with young Schefflera heptaphylla seedlings have substantially higher suction within the root zone compared with bare slope and slope vegetated with Cynodon dactylon. This is because Schefflera heptaphylla has a higher root biomass, T-rf and ET than Cynodon dactylon. It was also found that suctions within root zones of vegetated slopes and bare slope were completely destroyed under rainfall events corresponding to 2 years and 20 years return period. Copyright (C) 2015 John Wiley & Sons, Ltd.

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