红树林
磷酸盐
酸性磷酸酶
磷酸酶
海湾
生态系统
土壤盐分
盐度
土工试验
环境化学
化学
环境科学
生物
生态学
土壤水分
地质学
生物化学
酶
海洋学
作者
Sanjukta Das,Tapan Kumar Jana,Tarun Kumar De
标识
DOI:10.1080/01490451.2013.866705
摘要
AbstractImpact of phosphate solubilizing bacteria along with soil phosphatase activity on phosphorous cycle was found to be quiet interesting in the Sundarban mangrove ecosystem. Soil phosphatase activity showed a decreasing pattern with increase in depth [soil phosphatase activity (μg pnp produced g−1 dry wt of soil) = 906.85 – 5.6316 Depth (cm)] from the deep forest region of the Sundarban forest ecosystem. Soil salinity showed a very little effect on soil phosphatase activity whereas soil temperature and pH was found to show significant impact on the soil phosphatase activity. This ensured that the microbes associated with phosphate mineralization present in the Sundarban forest ecosystem are more tolerant to fluctuation in salinity than that of temperature and pH. A direct correlation was perceptible between the number of phosphate solubilizing bacteria and phosphatase activity in the soil during the study period from 2007 to 2012. Soil phosphate concentration was found to be directly governed by the soil phosphatase activity [The regression equation is: avg PO4−3-P (μg g−1 dry wt of soil) = 0.0311 + 0.000606 soil phosphatase activity (μg pnp produced g−1 dry wt of soil); R2 = 63.2%, p < 0.001, n = 62].Keywords: phosphate solubilizing bacteriasoil phosphatase activitySundarban mangrove ecosystem
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