4.7 Article

Effects of anecic earthworms on runoff and erosion on the slope with soil from the Loess Plateau under a rainfall simulation experiment

Journal

AGRICULTURAL WATER MANAGEMENT
Volume 259, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.agwat.2021.107230

Keywords

Earthworm; Runoff; Erosion; Bare slope; Simulated rain; Loess Plateau

Funding

  1. Strategic Priority Research Program of the Chinese Academy of Sciences [XDA23070202]

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Earthworms play a significant role in reducing runoff but increasing soil erosion. Their activities influence water infiltration and significantly alter the physical and chemical properties of the soil. This study provides insights into the effects of earthworms on runoff and soil erosion, contributing to a better understanding of soil erosion control on the Loess Plateau.
Earthworms are ecological engineers that play an important role in hydrological processes and soil erosion by their burrowing and casting activities. Little is known, however, about the ecological function of the activities of an anecic species (Metaphire guillelmi) from the Loess Plateau in China where the soil is severely eroded. We conducted rain-simulation experiments on artificial slopes (mesocosms) filled with soil from Loess Plateau. Two rain intensities (90 and 120 mm h(-1)) and slope gradients (5 degrees and 15 degrees) were used to investigate the influences of earthworm activity on runoff and soil loss under multiple conditions. Data from 15 d of earthworm activity and 1 h of rain indicated that earthworm activity significantly reduced runoff but aggravated soil erosion. Runoff initiation time increased 2.7-3.1-fold, contributing to the promotion of water infiltration, and the amounts and rates of runoff were 35.8-61.6% and 35.1-60.8% lower under earthworm activity than the controls, respectively. Earthworms greatly influenced the physical and chemical properties of the soil, and these properties were strongly correlated with runoff initiation time and cumulative runoff. The surface casts produced by the earthworms on the soil surface were completely dispersed, increasing the cumulative sediment by a maximum of 169%. Both rain intensity and slope gradient greatly influence runoff and soil detachment, but with earthworm activity, slope gradient was more influential due to its superior contribution to sediment transport. This study quantified the effects of M. guillelmi on runoff and soil erosion and provides basic data for developing a more integrated control of soil erosion on the Loess Plateau.

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