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Enumeration of Microbes and Microbial Activities in Coastal Saline Soils of Eastern India

机译:印度东部沿海盐水土壤中微生物和微生物活性的枚举

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An investigation was carried out to study the effect of salinity on microbes and enzyme activities of the salt-affected soils in five districts of Odisha, India adjacent to Bay of Bengal in relation to physicochemical properties. The soils are strongly acidic to slightly alkaline, and having a salinity of 2.28 to 8.11 dS m1, low in organic C and available N, and medium in available P and K. The microbial populations were relatively lower in these saline soils, and bacterial population dominant over that of fungi and actinomycetes. Soil biological activity in terms of dehydrogenase and fluorescein diacetate activities in the saline soils varied from 0.89 - 2.11 ug TPF Ir1 g-1 soil and 0.91 to 2.31 ug g"1 h"1, respectively. Acid phosphatase activity was relatively higher (27.8 - 64.2 (ig p-nitrophenol g"1 soil h') than alkaline phosphatase activity (17.8 - 55.9 ug p-nitrophenol g"1 soil h-1) and influencing the P transformations. Among the various soil groups, Vertisols had higher status of availablenutrients and enzyme activities followed by Inceptisols, Alfisols and Entisols. Salinity had negative relationship with all microbial variables and chemical properties of the soil, indicating that the increase in soluble salt content affects severely the biochemical transformations that regulate inherent soil fertility. Since majority of soil biochemical transformations are dependent on presence of microbes and microbial activities, the present investigation emphasized the intervention of suitable strategies for maintenance of soil quality in order to realize higher crop productivity in the coastal regions.
机译:进行了调查,以研究盐度对Microbes和酶活性的影响,含盐的土壤中的盐受影响的土壤,与孟加拉湾相邻的物理化学性质。土壤是强烈的酸性至略微碱性的,并且盐度为2.28至8.11dsm1,有机C中的低,可用N和可用的培养基和k。在这些盐水中的微生物群体相对较低,细菌群体相对较低占据真菌和放线菌的占主导地位。盐水土壤中脱氢酶和荧光素二乙酸酯活性的土壤生物活性从0.89-2.11μgTPFIR1G-1土壤和0.91至2.31ugg“1 h”1不同。酸性磷酸酶活性比碱性磷酸酶活性相对较高(27.8-44.2(Ig P-硝基苯酚G“1土壤H')(17.8-55.9 ug p-硝基苯酚G”1土壤H-1)并影响P变换。其中各种土壤基团,vertisols具有较高的可用营养素和酶活性的地位,然后是酶,αα和氧化剂。盐度与所有微生物变量和土壤的化学性质有负面关系,表明可溶性盐含量的增加严重影响生化转化调节固有的土壤肥力。由于土壤生化转化大多数依赖于微生物和微生物活动的存在,本研究强调了适当的维护土壤质量策略的干预,以实现沿海地区的较高作物生产率。

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