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Abstract
The primary factor that influences release of zinc (Zn) for plants is the rhizosphere. However, information about Zn-desorption characteristics in the rhizosphere is limited. A greenhouse experiment was performed to determine Zn-release characteristics in the bulk and the rhizosphere soils using a rhizobox. The kinetics of Zn release was determined by successive extraction with diethylenetriaminepentaacetic acid (DTPA)– triethanolamine (TEA) in a period of 1 to 504 h at 25 ± 1 °C in the bulk and the rhizosphere soils. Moreover, Zn extracted by using three extractants [DTPA-TEA, ammonium bicarbonate (AB)-DTPA, and Mehlich 3] in the bulk and the rhizosphere soils. The results showed that Zn extracted in the rhizosphere soils were significantly (P < 0.01) lower than the bulk soils. The mean of Zn release in the bulk and the rhizosphere soils were 5.31 and 4.91 mg kg−1, respectively. Release kinetics of Zn conformed fairly well to power function, first order, parabolic diffusion, and simplified Elovich equations. The results of kinetics study indicated that release-rate coefficients decreased in the rhizosphere soils compare to the bulk soils. The correlation studies showed that Zn release after 504 h was significantly correlated (P < 0.05) with Zn extracted by using DTPA-TEA, AB-DTPA, and Mehlich 3 in the bulk and the rhizosphere soils. The results of this research showed that Zn-release characteristics in the bean rhizosphere soils were different from the bulk soils.