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  1. 1 Ιαν 2019 · Leaching of excess soluble Cl − from the root zone to deeper soil levels by ponding/irrigation with Cl −-free water. This amelioration strategy might be an effective means to decrease the amount of soluble Cl − in the root zones for two reasons.

  2. 1 Δεκ 2001 · Natural inputs of chlorine (Cl) to soils come mainly from rainwater, sea spray, dust and air pollution. In addition, human practices, such as irrigation and fertilization, contribute significantly to Cl deposition. In the soil solution, Cl occurs predominantly as the chloride anion (Cl −).

  3. High pH, above 8.5, with high concentrations of HCO3 -and CO3 2-, causes precipitation of calcium and magnesium ions, leaving excess sodium in the soil solution. Small amounts of chloride are...

  4. 25 Μαΐ 2024 · Conventional remediation methods, including ex-situ thermal desorption (ESTD) and in-situ thermal desorption (ISTD), are highly effective in removing chlorinated organic contaminants (COCs) from soils. This paper summarizes the current status of thermal desorption techniques for the removal of COCs, with a focus on their energy efficiency.

  5. 5 Απρ 2018 · In salt-contaminated soils, the Cl − concentration in the soil solution can be so high that Cl − influx into root cortical cells is passive, favoring a rapid accumulation in the aerial tissues.

  6. 30 Μαΐ 2023 · The higher chlorine treatment significantly increased the exchangeable Al3+ content in the 0–20, 20–40, and 40–60 cm soil layers by 2.79, 1.64, and 0.94 mg kg−1, respectively, significantly increasing the risk of aluminum toxicity.

  7. 11 Οκτ 2021 · There was a low content of Cl in the plant during 2016 and 2019, which appeared to result from the higher rainfall (1,849.5 and 1,742.1 mm) and the lower content of Cl in the soil. The highest Cl accumulation was observed in the treatment of 900 mg Cl ha −1 with the value of 1,205 mg kg −1 in the leaves (Figure 3A), 1,113 mg Cl ha −1 in ...

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