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Journal ArticleDOI

Sorption of dissolved organic matter in salt-affected soils: effect of salinity, sodicity and texture.

TLDR
The sorption of DOC (derived from mature wheat straw) was more strongly affected by SAR than by EC, andDOC sorption in salt-affected soil is more strongly controlled by CEC and Fe/Al concentration than by clay concentration per se except in sodic soils where DOC sorption is low due to the high sodium saturation of the exchange complex.
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This article is published in Science of The Total Environment.The article was published on 2012-10-01. It has received 74 citations till now. The article focuses on the topics: Sorption & Soil water.

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Citations
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Salt effects on the soil microbial decomposer community and their role in organic carbon cycling: A review

TL;DR: A review of the available research on how salt affects decomposer microbial communities and carbon cycling in soil can be found in this paper, where the authors provide a brief overview and qualification of widely applied methods to assess microorganisms in soil to date.
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Salinity and bacterial diversity: to what extent does the concentration of salt affect the bacterial community in a saline soil?

TL;DR: It emerged that a patchy saline soil can not contain just a single microbial community selected to withstand extreme osmotic phenomena, but many communities that can be variously correlated to one or more environmental parameters.
Journal ArticleDOI

Treated wastewater reuse for irrigation: Pros and cons

TL;DR: This review highlights growing water scarcity, the history of wastewater reuse in agriculture, and the limitations of existing studies, and takes an in-depth look at three broad areas: environmental impacts, public health impacts, and economic impacts.
Journal ArticleDOI

Siderophore-Producing Rhizobacteria as a Promising Tool for Empowering Plants to Cope with Iron Limitation in Saline Soils: A Review

TL;DR: A critical overview of the combined effects of Fe limitation and soil salinization as challenges to modern agriculture is provided and some indirect evidence is summarized that argues in favour of siderophore-producing PGPR as biofertilization agents in salinized soils.
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Adsorption-desorption behavior of dissolved organic carbon by soil clay fractions of varying mineralogy

TL;DR: In this article, a set of batch adsorption-desorption experiments were conducted using pedogenic clays extracted from soils dominated by kaolinite-illite (Kaol-Ill), smectite (Smec), and allophane (Allo).
References
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Journal ArticleDOI

Dissolved organic matter in soil: challenging the paradigm of sorptive preservation

TL;DR: In this article, the authors present a case study where they relate the yearly retention of dissolved organic carbon (DOC) in the mineral soil to the available sorption capacity of seven forest soils and estimate that the saturation of the sorption complex would occur within 4-30 years.
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Degradation processes and nutrient constraints in sodic soils

TL;DR: The principal factor that determines the extent of adverse effects of excess sodium (Na+) on soil properties is the accompanying electrolyte concentration in the soil solution, with low concentration promoting the deleterious effects of exchangeable Na+ even at exchangeable sodium percentage (ESP) levels less than 5 as discussed by the authors.
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Stabilization of dissolved organic matter by sorption to the mineral soil

TL;DR: In this article, the main process by which dissolved organic matter is retained in forest soils is likely to be sorption in the mineral horizons that adds to stabilized organic matter (OM) pools.
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Biodegradation of forest floor organic matter bound to minerals via different binding mechanisms

TL;DR: In this paper, the authors studied the biodegradation of OM bound to goethite (α-FeOOH), pyrophyllite, and vermiculite via specific mechanisms as estimated from OC uptake in different background electrolytes and operationally defined as 'ligand exchange', 'Ca2+ bridging', and 'van der Waals forces'.
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