Influence of pyrolysis temperature on rice straw biochar properties and corresponding effects on dynamic changes in bispyribac-sodium adsorption and leaching behavior in soil
Section snippets
INTRODUCTION
Soil is an important resource for agriculture production and provides a suitable basis for biomass production, water flow regulation, C storage, sustaining biodiversity, and maintenance of gas balance in air (Ogbonnaya and Semple, 2013). The continuous loss of soil organic matter is a major environmental issue in many regions around the world (Jones et al., 2011; Sebiomo et al., 2011), as such losses lead to declines in soil quality and agronomic potential and have an effect on global climate
Soil, RS and biochar
Sandy loam soil (56.60% sand, 29.60% silt, and 13.80% clay) was collected from Shaheed Bhagat Singh Nagar, Punjab, India. Rice straw was prepared by the method of Sharma et al. (2020). The biochars were produced from RS in a closed muffle furnace with limited oxygen supply (oxygen-limited conditions) by carbonizing RS at 350 and 550 °C for 30 min and designated as RS350 and RS550, respectively. Biochar was also produced from RS by purging the pyroformer with N2 (nitrogen purging conditions) at
Properties of RS, its biochars and soil used
Physicochemical properties. The selected physico-chemical properties of RS and biochars are given in Table II. The pH of RS increased as pyrolysis temperature increased, due to the loss of acidic functional groups with increases in pyrolysis temperature. Total organic C (TOC) of RS and biochars was 522 and 79–330 g kg–1, respectively. The lower TOC of RS350 and RS550 (Table II), compared to RSC, arose from the consumption of surface C by the small amount of oxygen present in the muffle furnace.
CONCLUSIONS
The RS biochars were prepared and characterized using XRD, FTIR, TGA, BET, and SEM. Adsorption and desorption of bispyribac-sodium varied significantly with this herbicide's concentration and the type and application rate of soil amendment. The greatest adsorption was observed in SL+RSC, followed by RS550, SL+RS350, SL+RS, and SL, with desorption following the reverse order. Different leaching risk evaluation indices were calculated to assess the susceptibility of groundwater to
ACKNOWLEDGEMENT
The authors are thankful to Head Department of Agronomy and Head Department of Chemistry, PAU, Ludhiana, India for providing research facilities.
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