Temperature Effects on Properties of Rice Husk Biochar and Calcinated Burkina Phosphate Rock

• Published in: Agriculture (Basel) Vol. 11; no. 5; p. 432
• Main Authors: Avornyo, Vincent K., Manu, Andrew, Laird, David A., Thompson, Michael L.
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.05.2021
• Subjects: agriculture; ash content; biochar; Charcoal; Farmers; feedstocks; Fertilizers; Formic acid; Hydroxyapatite; Laboratories; Mineralogy; Minerals; phosphate rock; phosphorous; phosphorus; Pyrolysis; Quartz; Raw materials; Rice; rice hulls; rice husk biochar; Roasting; rock phosphate; Rocks; Silicon dioxide; solubility; Sub-Saharan Africa; Subsidies; temperature; Temperature effects; Ghana; Togo; West Africa; Africa; Sub-Saharan Africa
• ISSN: 2077-0472; 2077-0472
• DOI: 10.3390/agriculture11050432

Rice husk biochar (RHB) and phosphate rock (PR) are locally accessible resources that poor farmers in Sub-Saharan Africa (SSA) can utilize to increase rice productivity. However, biochars are variable depending on feedstock, pyrolysis temperature, and duration. Phosphate rocks from SSA are of low solubility. The goal of this study was to determine whether pyrolysis of rice husk (RH), calcination of PR, and the calcination/pyrolysis of a RHB-PR mixture at 300 °C, 500 °C, and 700 °C can increase formic acid (FA)- extractable phosphorous (P). The properties of these RHBs were compared to the properties of RHB produced through a simple farmer-friendly pyrolysis technique termed “Kun-tan”. Properties of calcinated PR were also compared to the raw PR. Quartz formed from amorphous SiO2 during RH pyrolysis and was the dominant mineral phase in the biochars, irrespective of the pyrolysis temperature. Formic acid-extractable P content, pH, and ash content of the biochars increased with increasing pyrolysis temperature. At 700 °C, FA-extractable P content of the RHB was 219% more than the feedstock. Hydroxyapatite and quartz were the dominant minerals in the PR irrespective of calcination temperature, indicating that hydroxyapatite and quartz were stable to at least 700 °C. Rather, calcination decreased the FA-extractable P content of the PR.