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Chloride retention in forest soil by microbial uptake and by natural chlorination of organic matter
Inorganic chlorine (i.e. chloride; Cl-in) is generally considered inert in soil and is often used as a tracer of soil and ground water movements. However, recent studies indicate that substantial rExpand
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The Role of Organic-matter-bound Chlorine in the Chlorine Cycle: A Case Study of the Stubbetorp Catchment, Sweden
Abstract.The objective of this study is to construct a balanced chlorine budget for a small forested catchment, focusing on the interaction between chloride (Clinorg) and organic-matter-boundExpand
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Differentiation of human mesenchymal stem cells and articular chondrocytes: Analysis of chondrogenic potential and expression pattern of differentiation‐related transcription factors
Mesenchymal stem cells (MSCs) are a candidate for replacing chondrocytes in cell‐based repair of cartilage lesions. However, it has not been clarified if these cells can acquire the hyalineExpand
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Temperature sensitivity indicates that chlorination of organic matter in forest soil is primarily biotic.
Old assumptions that chloride is inert and that most chlorinated organic matter in soils is anthropogenic have been challenged by findings of naturally formed organochlorines. Such naturalExpand
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Chloride retention and release in a boreal forest soil: effects of soil water residence time and nitrogen and chloride loads.
The common assumption that chloride (Cl-) is conservative in soils and can be used as a groundwater tracer is currently being questioned, and an increasing number of studies indicate that Cl- can beExpand
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Is chloride a conservative ion in forest ecosystems?
Chloride (Cl−) has often been assumed to be relatively unreactive in forest ecosystems, and is frequently used as a conservative tracer to calculate fluxes of water and other ions. Recently, however,Expand
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Organic and inorganic chlorine in Swedish spruce forest soil: influence of nitrogen
Concentrations of organic and inorganic chlorine were estimated in samples collected in forest soils in the southern part of Sweden, and changes were observed after the addition of nitrogen in incuExpand
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Chlorine transport in a small catchment in southeast Sweden during two years
Previous studies have revealed that chlorine participates in a complex biogeochemical cycle in soil, which suggests that the transport of chloride through catchments may also be influenced. TheExpand
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Release of reactive organic halogens by the brown macroalga Saccharina latissima after exposure to ultraviolet radiation
The brown macroalga Saccharina latissima (Linnaeus) C.E. Lane, C. Mayes, Druehl & G.W. Saunders (formerly Laminaria saccharina [L.] Lamouroux) was exposed to ultraviolet radiation (UVR) in the mWExpand
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Chlorine cycling and fates of 36Cl in terrestrial environments
Chlorine-36 (36Cl), a radioisotope of chlorine (Cl) with a half-life of 301,000 years, is present in some types of nuclear waste and is disposed in repositories for radioactive waste. As the releasExpand
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