Abstract

Abstract. The main objective of this study was to assess the impact of biochar rate (0, 8, 16 and 32 Mg ha−1) on the water retention capacity (WRC) of a sandy loam Dystric Plinthosol. The applied biochar was a by-product of slow pyrolysis (∼450 °C) of eucalyptus wood, milled to pass through a 2000 μm sieve that resulted in a material with an intrinsic porosity ≤10 μm and a specific surface area of ∼3.2 m2 g−1. The biochar was incorporated into the top 15 cm of the soil under an aerobic rice system. Our study focused on both the effects on WRC and rice yields 2 and 3 years after its application. Undisturbed soil samples were collected from 16 plots in two soil layers (5–10 and 15–20 cm). Soil water retention curves were modelled using a nonlinear mixed model which appropriately accounts for uncertainties inherent of spatial variability and repeated measurements taken within a specific soil sample. We found an increase in plant-available water in the upper soil layer proportional to the rate of biochar, with about 0.8% for each Mg ha−1 biochar amendment 2 and 3 years after its application. The impact of biochar on soil WRC was most likely related to an effect in overall porosity of the sandy loam soil, which was evident from an increase in saturated soil moisture and macro porosity with 0.5 and 1.6% for each Mg ha−1 of biochar applied, respectively. The increment in soil WRC did not translate into an increase in rice yield, essentially because in both seasons the amount of rainfall during the critical period for rice production exceeded 650 mm. The use of biochar as a soil amendment can be a worthy strategy to guarantee yield stability under short-term water-limited conditions. Our findings raise the importance of assessing the feasibility of very high application rates of biochar and the inclusion of a detailed analysis of its physical and chemical properties as part of future investigations.

Highlights

  • Soil water retention capacity (WRC) is a potential indicator of soil quality and productivity

  • The consistent soil water retention curve (SWRC) underestimation at high matric potential was likely due to increases in soil moisture content with biochar application, which was evident from SWRCs for treatments with 8 and 32 Mg ha−1 in the upper and lower soil layers in S2

  • We found a consistent increase in plant-available water and rice-available water in the upper soil layer of around 0.8 and 1 % for each Mg ha−1 biochar amendment, respectively, 2 and 3 years after its application

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Summary

Introduction

Soil water retention capacity (WRC) is a potential indicator of soil quality and productivity. Several agronomic practices such as no-tillage, mulching and cover crops are implemented aiming to improve soil physical properties. According to Mcdonagh et al (2014), improved soil management practices likely to be adopted by land users are multi-purpose technologies.

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