2017
DOI: 10.1016/j.chemgeo.2017.06.017
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Quantification of dissolved organic matter in pore water of the vadose zone using a new ex-situ positive displacement extraction

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Cited by 4 publications
(4 citation statements)
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“…According to the JMPR report on ethiprole, ethiprole sulfone residue in brown rice and rice husks was from the metabolism of ethiprole in rice and transportation from soils, while ethiprole amide was mainly from uptake and translocation from roots 9 . The uptake and translocation of compounds by plants are affected by their physiochemical properties and soil characteristics 41,42 . Compounds (log K ow < 3) are readily taken by rice roots but finitely translocated into rice leaves 41 .…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…According to the JMPR report on ethiprole, ethiprole sulfone residue in brown rice and rice husks was from the metabolism of ethiprole in rice and transportation from soils, while ethiprole amide was mainly from uptake and translocation from roots 9 . The uptake and translocation of compounds by plants are affected by their physiochemical properties and soil characteristics 41,42 . Compounds (log K ow < 3) are readily taken by rice roots but finitely translocated into rice leaves 41 .…”
Section: Resultsmentioning
confidence: 99%
“…9 The uptake and translocation of compounds by plants are affected by their physiochemical properties and soil characteristics. 41,42 Compounds (log K ow < 3) are readily taken by rice roots but finitely translocated into rice leaves. 41 The ethiprole and its metabolites have log K ow < 3.…”
Section: Dissipation Of Ethiprole and Its Metabolites In Rice Husks A...mentioning
confidence: 99%
“…The evaluation and the nature of the compacted layer could be related to different factors such as leaching and accumulation of organic and inorganic colloidal material in the soil pores, compaction processes under the recharged water weight, soil erosion processes, and the routine operations in the ponds [18]. In fact, the results from the soil profile measurements and from other research studies in the Shafdan (e.g., [4,7,21]) indicate that each of these factors can be relevant, or even dominant, in different areas of the recharge ponds. Regardless of these factors, it can be assumed that the development of this layer was enhanced with the utilization of improper tillage tools (e.g., narrow plow) and due to the improper tillage regime (e.g., working over too wet soil).…”
Section: Soil Compactionmentioning
confidence: 99%
“…The recharge and the SAT process take place in the coastal Quaternary sandstone aquifer, which also provides vast storage capacity that cannot be replaced by surface reservoirs. During the flow process of secondary effluent through the vadose zone and the aquifer, most of the biodegradable organic matter, suspended solids, bacteria, viruses, phosphorus, heavy metals, and other elements are removed from the effluents by a combination of geochemical, physical, and biological processes [1][2][3][4][5][6][7][8][9][10][11][12][13]. The recovered effluents, after SAT treatment, are characterized by excellent quality for most of the measured parameters, which comply with the levels allowed by the Israeli Health Ministry for unrestricted irrigation of any crop [1,10,11].…”
Section: Introductionmentioning
confidence: 99%