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首页> 外文期刊>Journal of the Indian Society of Soil Science >Effect of Horticultural Land uses on Soil Properties and Organic Carbon Distribution in a Reclaimed Sodic Soil
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Effect of Horticultural Land uses on Soil Properties and Organic Carbon Distribution in a Reclaimed Sodic Soil

机译:复垦苏打土壤中园艺用地对土壤性质和有机碳分布的影响

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摘要

Information on soil properties and organic carbon distribution in reclaimed sodic soils under different horticultural fruit trees as well as how organic carbon stock varies depth-wise under these land uses is very limited. Therefore, four horticultural land uses namely, guava (Psidium guajava), litchi (Litchi chinensis), mango (Mangifera indica), and jamun (Syzygium cumini) were selected to study their effect on soil properties and distribution of soil organic carbon (SOC) onto different pools of their oxidizability in a reclaimed sodic soil. Soil samples were collected up to a depth of 60 cm i.e. 0-20, 20-40 and 40-60 cm from the above land uses. Results showed that soil pHw (soil: water ratio: 1:2) and bulk density (BD) increased with depth in allthe land uses. Minimum and maximum pHw was associated with litchi (6.81) at 0-20 cm and jamun (7.73) at 40-60 cm depth of soil, respectively. Guava recorded minimum BD (1.45 Mg m~3) at 0-20 cm soil depth whereas, a maximum BD of 1.66 Mg m~3 was associated with litchi plantation at lower soil depths. Among the land uses, highest clay content (19.2%) at 0-20 cm was observed under litchi plantation followed by mango (17.3%), jamun (14.4%) and guava (13.9%). Litchi (1.49%) and mango (1.4%) recorded highestCaC03 content at 0-20 cm soil depth. The amount of oxidizable organic C (OC) varied among the land uses, on an average, its amount was highest with guava (25.9 Mg C ha~(-1)) followed by jamun (25.1 Mg C ha') = litchi (25.0 Mg C ha~(-1)) > mango (16.5 MgC ha~(-1)) in surface soil. Total organic carbon (TOC) stock at surface soil in descending order was guava (28.8 Mg C ha~(-1)) > jamun (27.3 Mg C ha~(-1)) > litchi (25.7 Mg C ha~(-1)) > mango (19.2 Mg C ha~(-1)). In all the land uses, with depth increment passive pool carbon content was increased due to more physical, chemical and biochemical stabilization of organic carbon in lower depths of soil. Soils under guava plantation recorded highest SOC storage (61.0 Mg C ha~(-1)) as well as maximum passivepool C (25.3 Mg C ha~(-1)) up to 60 cm soil depth. Therefore, guava plants can be recommended in reclaimed sodic soils or otherwise barren degraded salt affected land for income generation to the farmers as well as environmental benefit to the mankind.
机译:在不同园艺果树下的复垦苏打土壤中的土壤特性和有机碳分布以及在这些土地利用下有机碳储量如何沿深度变化的信息非常有限。因此,选择了四种园艺土地用途,即番石榴(Psidium guajava),荔枝(Litchi chinensis),芒果(Mangifera indica)和贾蒙(Syzygium cumini),以研究其对土壤特性和土壤有机碳(SOC)分布的影响。在复垦的苏打土壤中,它们在不同氧化池中的氧化能力不同。在距上述土地用途60 cm的深度(即0-20、20-40和40-60 cm)的深度收集土壤样品。结果表明,在所有土地利用中,土壤的pHw(土水比:1:2)和容重(BD)均随深度增加。最小和最大pHw分别与0-20厘米土壤深度的荔枝(6.81)和40-60厘米深度的果酱(7.73)有关。番石榴在0-20厘米土壤深度下记录的最小BD(1.45 Mg m〜3),而在较低土壤深度下的荔枝种植最大BD(1.66 Mg m〜3)。在土地利用中,荔枝人工林在0-20厘米处的黏土含量最高(19.2%),其次是芒果(17.3%),果酱(14.4%)和番石榴(13.9%)。荔枝(1.49%)和芒果(1.4%)在0-20厘米土壤深度处记录到最高的CaCO3含量。可氧化有机碳(OC)的量随土地利用而变化,平均而言,其含量最高的是番石榴(25.9 Mg C ha〜(-1)),其次是果酱(25.1 Mg C ha')=荔枝(25.0)地表土壤中的Mg C ha〜(-1))>芒果(16.5 MgC ha〜(-1))。表层土壤有机碳总量以降序排列为番石榴(28.8 Mg C ha〜(-1))>果酱(27.3 Mg C ha〜(-1))>荔枝(25.7 Mg C ha〜(-1) ))>芒果(19.2 Mg C ha〜(-1))。在所有土地利用中,由于深度较小的土壤中有机碳的更多物理,化学和生化稳定作用,被动池碳含量随深度增加而增加。番石榴种植下的土壤记录了最高的SOC储量(61.0 Mg C ha〜(-1))和最大被动池C(25.3 Mg C ha〜(-1)),最高土壤深度为60 cm。因此,可建议在复垦的苏打土壤或贫瘠的盐分退化的土地上种植番石榴植物,以为农民创造收入并为人类带来环境效益。

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