Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8873216 | Geoderma Regional | 2018 | 7 Pages |
Abstract
An understanding of the rate at which fluorine (F) accumulates in soil from phosphorus fertiliser and how much is lost via leaching are important because of the challenge elevated F may pose to soil, plant and animal health. This study measured F accumulation in a soil under pasture (Inceptisol) that received single superphosphate (SSP) fertiliser over 63â¯years in a long-term fertiliser trial. It also assessed the downward movement of F in soil and effect of irrigation in a long-term irrigation trial. Results showed total F concentrations in topsoil (0-7.5â¯cm) that received 188â¯kg SSPâ¯haâ1 and 376â¯kg SSPâ¯haâ1 fertiliser increased from 251â¯mgâ¯kgâ1 to 349 and 430â¯mgâ¯kgâ1, respectively. The rates of F accumulation were estimated at 1.1 and 2.1â¯kgâ¯haâ1â¯yrâ1 respectively, low compared to previous studies. The F concentration in the 376â¯kg SSP haâ1 treatment decreased with depth, but was significantly higher than the control treatment to 50â¯cm, suggesting movement of F down the soil. Fluorine concentrations also decreased with depth to 50â¯cm in soils that received either no irrigation or up to 770â¯mmâ¯yrâ1 from irrigation. However there was no significant difference in the amount of F with depth between irrigation treatments. We postulate that F was moving predominately in drainage water in the period immediately after P fertiliser application in mid-winter and wasn't enhanced by irrigation. This study should be repeated for other soil types to help our understanding of the potential for ongoing F accumulation in soil and implications this may have on future land use.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Colin William Gray,