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首页> 外文期刊>Archives of Agronomy and Soil Science >Distribution of different forms of Mn and their association with soil properties in arid zone soils of Punjab, India.
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Distribution of different forms of Mn and their association with soil properties in arid zone soils of Punjab, India.

机译:印度旁遮普邦干旱地区土壤中不同形式锰的分布及其与土壤性质的关系。

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Six pedons from arid zones soils of Punjab, north western India, were investigated for different forms of manganese (Mn): total Mn, diethylenetriamine penta-acetic acid (DTPA)-extractable Mn, soil solution plus exchangeable Mn, adsorbed Mn onto inorganic sites, and oxide surfaces, and Mn bound by organic sites. Total Mn content ranged from 241-517 mg kg-1, DTPA-extractable Mn content ranged from 1.40-4.52 mg kg-1, soil solution plus exchangeable Mn content ranged from 0.04-0.30 mg kg-1, Mn adsorbed onto inorganic sites ranged from 34-109 mg kg-1, and that onto oxide surfaces ranged from 28-173 mg kg-1. The Mn bound by organic sites ranged from 14-56 mg kg-1. The forms of Mn did not exhibit any consistent pattern of distribution. Irrespective of the different fractions of Mn their content was higher in the fine textured soils as compared to the coarse textured soils. The soil solution plus exchangeable Mn held onto organic site and oxide surface (amorphous) increased with increase in organic carbon, silt and clay contents. The Mn adsorbed onto inorganic site (crystalline) increased with only silt and clay content. The DTPA-Mn increased with increase in organic carbon content, whereas Mn adsorbed onto oxide surfaces increased with an increase in organic carbon, silt and clay. However, both these fractions decreased with an increase in calcium carbonate and pH. Total Mn was strongly correlated with organic carbon, silt and clay content of soil. Among the forms, Mn held on the organic site, water soluble+exchangeable and Mn adsorbed onto oxide surface were positively correlated with DTPA-extractable Mn. DTPA-extractable Mn and soil solution plus exchangeable Mn seem to be good indices of Mn availability in soils and are helpful for correction of Mn deficiency in the soils of the region.
机译:研究了印度西北部旁遮普邦干旱地区土壤中的六种ons,研究了不同形式的锰(Mn):总锰,二亚乙基三胺五乙酸(DTPA)可萃取的锰,土壤溶液加上可交换的锰,将锰吸附到无机位点上,氧化物表面和Mn被有机位点键合。总锰含量范围为241-517 mg kg -1 ,DTPA可萃取锰含量范围为1.40-4.52 mg kg -1 ,土壤溶液加可交换锰含量范围为0.04-0.30 mg kg -1 ,Mn吸附在无机位点上的范围为34-109 mg kg -1 ,氧化物表面的Mn范围为28-173 mg kg < sup> -1 。有机位点结合的Mn为14-56 mg kg -1 。 Mn的形式没有表现出任何一致的分布模式。不管Mn的不同含量如何,与粗糙纹理土壤相比,精细纹理土壤中的含量都较高。随着有机碳,淤泥和粘土含量的增加,土壤溶液加上可交换的Mn保留在有机位点和氧化物表面(无定形)上。吸附在无机位点(晶体)上的Mn仅随淤泥和粘土含量的增加而增加。 DTPA-Mn随着有机碳含量的增加而增加,而吸附到氧化物表面的Mn随着有机碳,粉砂和粘土的增加而增加。然而,随着碳酸钙和pH值的增加,这两个部分均降低。总锰与土壤中的有机碳,泥沙和粘土含量密切相关。在其中的形式中,保持在有机位点上的Mn,水溶性+可交换和吸附在氧化物表面上的Mn与可通过DTPA提取的Mn成正相关。 DTPA可萃取的Mn和土壤溶液加上可交换的Mn似乎是土壤中Mn有效性的良好指标,并且有助于纠正该地区土壤中的Mn缺乏症。

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