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Tillage, Manure and Gypsum Use in Reclamation of Saline-Sodic Soils

机译:盐碱土壤开垦中的耕作,肥料和石膏用途

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Soil degradation resulting from soil salinity and sodicityis a major problem under arid and semiaridclimates. Nearly 831 million hectares of land are salt-affected worldwide. Thehigh salt concentration negatively affects soil physical and chemicalproperties as well as soil microbial activity, thus causing a decline in soilproductivity. It has led to the depletion of soil organic carbon, decline inbiomass production, contamination of water resources, and emission ofgreenhouse gases such as CO2 at an accelerated rate. The initialhydration of sodic clays leads to slaking and swelling while continuoushydration results in dispersion of clay particles. Saline and sodic soilsusually suffer from poor physical properties, including high bulk density, lowmacroporosity and aggregate stability. Therefore, management of such soils ischallenging. The fundamental issue of soil quality improvement may in along-term have a aim to restore an earlier state for the required cropproduction purposes or to limit and/or slowing down the further deterioration,in order to reservations the original values and features of the soilproperties. Appropriate tillage is key factor for mitigation of negativeeffect, while application of organic matter through various sources is anotheramelioration strategy for salt-affected soils. These procedures affect soilphysical, chemical and biological properties. Tillage improves aeration andalleviates compaction while organic matter promotes binding soil particles intoaggregates. Present paper present positive aspect of tillage and amendmentaddition (gypsum, farmyard manure, sulfur) on properties of saline-sodic soilsusing available literature.
机译:在干旱和半干旱气候条件下,土壤盐分和碱度导致的土壤退化是一个主要问题。全世界有近8.31亿公顷的土地受盐害影响。高盐浓度对土壤的物理和化学性质以及土壤微生物活性产生负面影响,从而导致土壤生产力下降。它导致了土壤有机碳的消耗,生物量生产的下降,水资源的污染以及温室气体(如二氧化碳)的加速排放。钠粘土的初始水合会导致崩解和溶胀,而连续水合会导致粘土颗粒分散。盐水和钠盐土壤通常会遭受不良的物理特性,包括高堆积密度,低巨无石度和骨料稳定性。因此,这种土壤的管理具有挑战性。土壤质量改善的根本问题可能是为了恢复所需作物生产的早期状态或限制和/或减缓进一步恶化的目的,以便保留土壤特性的原始值和特征。适当的耕作是减轻负面影响的关键因素,而通过各种途径施用有机物是缓解盐碱土的另一种策略。这些程序会影响土壤的物理,化学和生物学特性。耕作改善了通气并减轻了压实,而有机物则促进了将土壤颗粒结合成团聚物。本文利用现有文献介绍了耕作和改良添加物(石膏,农家肥,硫磺)对盐碱土壤性质的积极影响。

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