Abstract

Background: Rainfall-triggered shallow landslides on steep slopes cause significant soil loss and can be hazards for property and people in many parts of the world. In New Zealand’s hill country, they are the dominant erosion process and are responsible for soil loss and subsequent impacts on regional water quality. Use of wide-spaced trees and afforestation with fast growing conifers are the primary land management tools in New Zealand to help control erosion and improve water quality. To decide where to implement erosion controls in the landscape requires determining the most susceptible places to these processes and models that incorporate how trees reinforce soils to understand if, and when, such treatments become effective.
 Methods: This paper characterises the mechanical properties of Pinus radiata D.Don roots (the common tree species used for afforestation in New Zealand) by means of field pullout tests and by measuring the root distribution at 360 degrees around trees. The Root Bundle Model (RBM) was used to calculate the root reinforcement. Statistical analysis was carried out to assess the statistical reduction coefficients of root reinforcement that depend on the number of measurements, used in geotechnical analysis to reduce the mean value of a parameter to a so-called characteristic value.
 Results: We show that to reach an effective level of root reinforcement, trees of 0.5 m DBH require a density of about 300 trees per hectare. Trees of this size are about 30 years of age across many sites and have generally reached the recommended conditions for clear-fell harvesting. The analysis of variance shows that 4 trees are the minimum number to be excavated to obtain sufficient root information to obtain less than 5% of error with a 95% of probability on the estimation of a design value of root reinforcement in accord with geotechnical standards.
 Conclusions: We found that the variability of lateral and basal root reinforcement does not limit the implementation of vegetation in slope stability models for Pinus radiata. We adopt for the first time the concept of a minimum sampling requirement and characteristic value, similarly to what is assumed for the value of effective soil cohesion in geotechnical guidelines for slope stability calculations.

Highlights

  • Shallow landslides on steep slopes occur mostly as a result of intense rainfall and are one of the main erosion processes of concern in many countries (Crozier 2005; Goetz et al 2015; Marden & Rowan 2015; Fan et al 2017; Vergani et al 2017; Peruccacci et al 2017; Palladino et al 2018)

  • We found that the variability of lateral and basal root reinforcement does not limit the implementation of vegetation in slope stability models for Pinus radiata

  • We adopt for the first time the concept of a minimum sampling requirement and characteristic value, to what is assumed for the value of effective soil cohesion in geotechnical guidelines for slope stability calculations

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Summary

Introduction

Shallow landslides on steep slopes occur mostly as a result of intense rainfall and are one of the main erosion processes of concern in many countries (Crozier 2005; Goetz et al 2015; Marden & Rowan 2015; Fan et al 2017; Vergani et al 2017; Peruccacci et al 2017; Palladino et al 2018). To aid forest planning and management, models are required to help understand the susceptibility of the landscape to landslides and to quantify the mechanical properties of root systems (Dazio et al 2018, Gehring et al 2019). Models such as SOSlope (Cohen & Schwarz 2017), which are physically based, need information on the root distribution and root tensile strength of trees to define their bio-engineering characteristics. To decide where to implement erosion controls in the landscape requires determining the most susceptible places to these processes and models that incorporate how trees reinforce soils to understand if, and when, such treatments become effective

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