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首页> 外文期刊>Journal of the Indian Society of Soil Science >Effect of Topography on Characteristics, Fertility Status and Classification of the Soils of Almora District in Uttarakhand
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Effect of Topography on Characteristics, Fertility Status and Classification of the Soils of Almora District in Uttarakhand

机译:地貌对北方阿尔莫拉区土壤特性,生育状况及分类的影响

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摘要

Topographic position is one of the most dominant factors that govern soil development in the hilly areas. Ten soil profiles representing different landform units i.e. hill top, side slope, broad valley and narrow valley terraces were chosen to investigate the soil morphological, physical and chemical characteristics and their relationships with topography in Almora district of Uttarakhand. Soil properties varied remarkably among the studied profiles. The soils were moderately shallow to very deep indepth (32-160 cm), non-saline (EC 0.03-0.45 dS nr'), acidic in nature (pH 5.1-6.6), low to high in organic carbon (OC) (0.03-2.91%) with low to moderate CEC [1.6-19.4 cmol(p+)kg']. Base saturation ranged from 45.9 to 75.1% in which calcium (Ca2*) and magnesium (Mg2f) were the dominant cations on exchangeable sites followed by potassium (K+) and sodium (Na+). The studied soils were dominated by silt fraction followed by clay, except in Dhamas (P4), Dhaili (P5) and Kosi (P10) which showed high sand content. Hill top profiles showed the highest OC. The upper soil layers of hill top and broad valley terrace profiles showed higher availability of soil macronutrients, whereas micronutrients were higher than agronomic critical limits in all profiles. Three soil profiles were classified as Entisols and keyed out as Typic Udifluvents (Kosi), Lithic Udorthents (Dhamas) and Typic Udorthents (Dhaili). Majkhali (P7) soils were placed under Inceptisol soil order and were classified as Dystric Eutrudepts. The remaining soils were placed under Alfisol soil order and keyed out as Hapludalf at great group level. Among the Alfisols, Someshwar (P9) was classified as Oxyaquick Hapludalfs, Sitlakhet (PI) was classified as Ultic Hapludalfs, Salla Routela (P2) and Chaubattia (P3) were classified as Mollic Hapludalfs, while Kausani (P6) and Hawalbagh (P8) soils were keyed out as Typic Hapludalfs. The soils in Almora district of Uttarakhand exhibited wide variations with topographic positions and proper soil management willhelp in maintaining sustainable production of this area.
机译:地形位置是在丘陵地区治理土壤发展的最主领域之一。选择不同地貌单位的十种土壤剖面I.E.Hill顶部,边坡,宽阔的山谷和狭窄的山谷露台,探讨了伊塔拉克省阿尔莫拉区的土壤形态,物理和化学特征及其关系。在研究的轮廓中,土壤性质显着变化。土壤中度浅到极深的暗淡(32-160厘米),非盐水(EC 0.03-0.45 DS NR'),自然酸性(pH5.1-6.6),有机碳(OC)低至高(0.03) -2.91%)低至中等CEC [1.6-19.4 CMOL(P +)kg']。基础饱和度为45.9至75.1%,其中钙(Ca2 *)和镁(Mg2F)是可更换位点上的主要阳离子,然后是钾(k +)和钠(Na +)。研究的土壤由淤泥部分占据主导,然后粘土,除了达米斯(P4),Dhaili(P5)和Kosi(P10),显示出高砂含量。 Hill Top Cuitiles展示了最高的OC。山顶和宽阔的山谷露台型材的上层土壤层显示出较高的土壤Macronrients的可用性,而微量营养素高于所有轮廓中的农艺临界限制。三块土壤型材被归类为奥斯索尔,并关键为典型的Udifluvents(Kosi),岩石Uteortents(Dhamas)和典型的Udortentents(Dhaili)。 Majkhali(P7)土壤被置于1次土壤秩序下,并被归类为染额Eutrudepts。将剩余的土壤置于血清醇土壤秩序下,并在大型群体水平下被关键。在血清醇中,Someshwar(p9)被归类为oxyaquick hapludalfs,Sitlakhet(pi)被归类为Ultic Hapludalfs,Salla Fordela(P2)和Chaubattia(P3)被归类为Mollic Hapludalfs,而Kausani(P6)和Hawalbagh(P8)土壤被关键为典型的Hapludalfs。北方阿尔莫拉区的土壤展出了各种各样的地形职位和适当的土壤管理Willhelp在维持该地区的可持续生产方面。

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