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Distribution of phosphorus and the effect of physicochemical properties and clay minerals on phosphorus release in some calcareous soils | ||
| Iran Agricultural Research | ||
| مقاله 9، دوره 39، شماره 2، اسفند 2020، صفحه 79-90 اصل مقاله (411.89 K) | ||
| نوع مقاله: Full Article | ||
| شناسه دیجیتال (DOI): 10.22099/iar.2021.38152.1405 | ||
| نویسندگان | ||
| S Shakeri* 1؛ A azadi2؛ M Saffari3 | ||
| 1Department of Agriculture, Payame Noor University, Tehran, I. R. Iran | ||
| 2Department of Soil and Water Research, Khuzestan Agricultural and Natural Resources Research and Education Center, AREEO, Ahvaz, I. R. Iran | ||
| 3Department of Environments, Institute of Science and High Technology and Environmental Sciences, Graduate University of Advanced Technology, Kerman, I. R. Iran | ||
| چکیده | ||
| Phosphorus (P) is a nutrient essential for plant, which its availability in soils changes with aging process, leaching, precipitation processes, and the landform change. There is limited information available on kinetics release of P in calcareous soils. Therefore, the purpose of this study was to investigate distribution of P and the effect of physicochemical properties and clay minerals on its release in some dominant orders of the calcareous soils in Kohgiluyeh-and-Boyer-Ahmad province, using the 0.01 M calcium chloride ( ) extractant. The results showed that the P released rapidly from the soil and continued slowly. After 72 h, the amount of P released in the studied soils ranged between 3.2 and 25.4 mg kg-1. Evaluation of the fitted different equations on P released in the studied soils revealed that the Simple Elovich and power function equations could well predict the P release process in the studied soils. The results of the correlation between soil properties and released P contents showed that P release coefficients (including the slope and intercept in the Simple Elovich equation) have a significant negative relationship with the amount of smectite and vermiculite minerals. Also, the release coefficient of the parabolic diffusion equation had a significant negative relationship with pH and the amount of illite and palygorskite minerals. | ||
| کلیدواژهها | ||
| Calcareous soils؛ Clay minerals؛ Phosphorus release | ||
| مراجع | ||
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