Determining critical soil pH for phosphorus uptake efficiency in an acidic Ultisol for maize | ||||
Egyptian Journal of Soil Science | ||||
Volume 64, Issue 4, December 2024, Page 1525-1536 PDF (360.63 K) | ||||
Document Type: Original Article | ||||
DOI: 10.21608/ejss.2024.308115.1827 | ||||
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Authors | ||||
M. Abdulaha-Al Baquy ![]() | ||||
1Department of Soil Science, Faculty of Agriculture, Hajee Mohammad Danesh Science and Technology University, Dinajpur, 5200, Bangladesh | ||||
2State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, P. O. Box 821, Nanjing, China | ||||
3Shenzhen Key Laboratory of Marine Bioresource and Eco-Environmental Science, Guangdong Provincial Key Laboratory for Plant Epigenetics, College of Life Sciences and Oceanography, Shenzhen University, Shenzhen 518060, China | ||||
Abstract | ||||
The scarcity of phosphorus (P) restricts crop growth due to reduced P uptake in acidic soil. Due to significant variations in soil pH in acidic Ultisol, it is still unclear how such variations would affect P uptake efficiency by maize plants. Thus, under different pH (3.75, 4.0, 4.5, 5.0 and 5.5) conditions, this study investigated the growth and P uptake efficiency during the growth of maize plants as influenced by the distribution of P species in Ultisols. Our results showed that increased soil acidity had a negative impact on plant height, dry matter yield (shoots and roots biomass), and chlorophyll content of maize plants. Also, the P uptake efficiency increased with decreased soil acidity, and the critical value for P uptake efficiency was pH 5.00. Generally, as soil pH was increased, soil available P decreased significantly and was consistent with higher uptake of available P by the plant and variations in different P species including those bound to iron, aluminum, and calcium. | ||||
Keywords | ||||
Acidification; Phosphorus speciation; Chlorophyll; Plant biomass; Nutrient availability | ||||
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