Effect of Increasing Phosphorus Doses Application on Some Physical, Chemical and Biological Properties of Soil, Under Long-Term Experiment Conditions.
Authors:
- Mehmet IşikMIMehmet Işik
- Serra AldoğanSASerra Aldoğan
- Mert SönmezMSMert Sönmez
- Seher İlHanSISeher İlHan
- İbRahim OrtaşIOİbRahim Ortaş
- 30 June 2023
- journal article
- research article
- Published by Agricultural & Environmental Technology Development Society in International Journal of Agricultural and Applied Sciences
- Vol. 4 (1) , 143-149
Abstract
Phosphorus (P) fertilizers are produced from rock phosphate (apatite); however, they are low-mobility in soil for plant nutrient absorption and uptake. In addition, the rock phosphate quantity is a limited source for future P fertilizer. At the same time, high phosphorus fertilization will cause environmental pollution (such as eutrophication in rivers). Also, a great proportion of applied P fertilizer remains in the soil, reducing the viable soil organisms. Therefore, the effect of different doses of P on some properties of soil (physical, chemical, and biological) is not entirely understood in the literature under long-term experiment conditions. Also, phosphorus fertilizer applications indirectly decrease the plant growth and yield. Under long-term experimental conditions, this research aims to understand the effect of increasing P doses on some physical, chemical and biological properties of the soil. The hypothesis to be tested is that under long-term field experiment conditions, increasing doses of phosphorus fertilizer negatively affect the soil properties. The field experiment was established in 1998 and has continued uninterruptedly to the present time under maize and wheat rotations. Four doses of P fertilizers were applied; such as 0, 50, 100 and 200 kg P2O5 ha-1 application with three replications. P2105 Maize (Zea mays L.) species seeds were sown in June 2022 and harvested in November 2022. At harvest, the soil samples were taken at 0-15 cm and 15-30 cm depth in each plot. Soil pH, EC and available P were analyzed as soil chemical properties. The number of mycorrhizal spores and Soil Organic Matter (by walkley-black method) were determined as soil biological properties. Furthermore, soil bulk density (BD), water stable aggregated (WSA) and mean weight diameter (MWD) were analyzed as soil physical properties. Phosphorus application in increasing doses negatively affects the soil physical properties (such as WSA, MWD and BD) under long-term field experiment condition. The research finding showed that depending on increasing P doses application soil WSA and MWD were decreased but BD was increased. While depending on increasing P doses application soil organic carbon is increased, however, the numerical value of mycorrhizal spores and root colonization was decreased. The results are revealed that for sustainable and eco-friendly crop production, 50 and 100 kg P2O5 ha-1 P fertilizer can be used in maize production.Keywords
This publication has 40 references indexed in Scilit:
- Management of soil phosphorus and plant adaptation mechanisms to phosphorus stress for sustainable crop production: a reviewJournal of Soil Science and Plant Nutrition, 2012
- Transgenic Plants and Associated Bacteria for Phytoremediation of Organic Pollutants2011
- Potential Negative Consequences of Adding Phosphorus‐Based Fertilizers to Immobilize Lead in SoilJournal of Environmental Quality, 2008
- Factors controlling the aggregate stability and bulk density in two different degraded soils amended with biosolidsSoil and Tillage Research, 2005
- Soil and fertilizer phosphorus: Effects on plant P supply and mycorrhizal developmentCanadian Journal of Plant Science, 2005
- GEOCHEMISTRY | Soil, Organic Components2005
- MYCORRHIZAL FUNGI2005
- Bulk Density1986
- Spores of mycorrhizal Endogone species extracted from soil by wet sieving and decantingTransactions of the British Mycological Society, 1963
- AN EXAMINATION OF THE DEGTJAREFF METHOD FOR DETERMINING SOIL ORGANIC MATTER, AND A PROPOSED MODIFICATION OF THE CHROMIC ACID TITRATION METHODSoil Science, 1934