Abstract

Abstract. Soil erosion is a major threat to soil functioning. The use of vegetation to control erosion has long been a topic for research. Much of this research has focused on the above-ground properties of plants, demonstrating the important role that canopy structure and cover plays in the reduction of water erosion processes. Less attention has been paid to plant roots. Plant roots are a crucial yet under-researched factor for reducing water erosion through their ability to alter soil properties, such as aggregate stability, hydraulic function and shear strength. However, there have been few attempts to specifically manipulate plant root system properties to reduce soil erosion. Therefore, this review aims to explore the effects that plant roots have on soil erosion and hydrological processes, and how plant root architecture might be manipulated to enhance its erosion control properties. We demonstrate the importance of root system architecture for the control of soil erosion. We also show that some plant species respond to nutrient-enriched patches by increasing lateral root proliferation. The erosional response to root proliferation will depend upon its location: at the soil surface dense mats of roots may reduce soil erodibility but block soil pores thereby limiting infiltration, enhancing runoff. Additionally, in nutrient-deprived regions, root hair development may be stimulated and larger amounts of root exudates released, thereby improving aggregate stability and decreasing erodibility. Utilizing nutrient placement at specific depths may represent a potentially new, easily implemented, management strategy on nutrient-poor agricultural land or constructed slopes to control erosion, and further research in this area is needed.

Highlights

  • Soil is a vital component of the earth system fundamental for many aspects of science (Brevik et al, 2015)

  • Plant roots are crucial in reducing soil erosion rates due to overland flow, as their presence affects soil properties such as aggregate stability, hydraulic function and shear strength

  • The effect of roots on soil erodibility is determined by root length density (RLD) and, lateral root (LR) density and length, and the distribution of roots within the soil

Read more

Summary

Introduction

Soil is a vital component of the earth system fundamental for many aspects of science (Brevik et al, 2015). Vegetation covers modify intrinsic soil properties determining a soil’s erodibility (Gyssels et al, 2005) creating a microclimate and supplying OM, which affect the activity of microorganisms, and nutrient availability, resulting in a positive feedback on plant productivity Both additional OM as well as microbial and fungal secretions enhance the formation of stable aggregates (Boer and Puidgefábregas, 2005, Vásquez-Méndez et al, 2010), which affect hydraulic conductivity and, water storage capacity (Boer and Puidgefábregas, 2005) and may increase soil shear strength (Tengbeh, 1993; De Baets et al, 2008). We explore the factors influencing RSA especially lateral root (LR) growth, and the potential of fertilizer applications to stimulate LR proliferation, and form the basis for a soil erosion control method, will be discussed

The effects of roots on soil erodibility
Root system architecture and its manipulation
Lateral root proliferation in response to local nutrient availability
Effects of LR proliferation on aerial growth
Findings
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call