Adsorption and Desorption of Mercury(II) in Three Forest Soils in Shandong Province, China
References (29)
- et al.
Binding and mobility of mercury in soils contaminated by emissions from chlor-alkali plants
Sci. Total. Environ.
(2002) - et al.
Mercury storage in surface soils in a central Washington forest and estimated release during the 2001 Rex Creek Fire
Sci. Total. Environ.
(2008) - et al.
Adsorption and desorption of iodine by various Chinese soils: II. Iodide and iodate
Geoderma.
(2009) - et al.
Comparison of the composition of forest soil litter derived from three different sites at various decompositional stages using FTIR spectroscopy
Geoderma.
(1998) - et al.
Drift and transmission FT-IR spectroscopy of forest soils: an approach to determine decomposition processes of forest litter
Vib. Spectrosc.
(1999) - et al.
Effects of pH, organic acids, and competitive cations on mercury desorption in soils
Chemosphere.
(2007) - et al.
The chemistry of atmospheric mercury: a review
Atmos. Environ.
(1999) - et al.
Sorption of mercury (II) in Amazon soils from column studies
Chemosphere.
(2005) - et al.
Extractability and mobility of mercury from agricultural soils surrounding industrial and mining contaminated areas
Chemosphere.
(2010) - et al.
Fourier transform infrared study of mercury interaction with carboxyl groups in humic acids
J. Photoch. Photobio. A.
(2008)
Adsorption of mercury on laterite from Guizhou Province, China
J. Environ. Sci.
Adsorption behavior of herbicide butachlor on typical soils in China and humic acids from the soil samples
J. Colloid. Interf. Sci.
Structural characterization of humic acids isolated from typical soils in China and their adsorption characteristics to phenanthrene
Colloid. Surface. A.
Competitive sorption behavior of copper(II) and herbicide propisochlor on humic acids
J. Colloid. Interf. Sci.
Cited by (19)
The interplay between atmospheric deposition and soil dynamics of mercury in Swiss and Chinese boreal forests: A comparison study
2022, Environmental PollutionCitation Excerpt :However, our calculation indicated an annual release (2 μg Hg m−2 yr−1) of only 0.008% of total Hg in the Bs horizon (100 mg Hg m−3, 25 cm thick). Similar low desorption rates were found in batch experiments with 3 forest soils in China with Hg concentrations of 338–477 μg kg−1, showing averagely desorption of 0.24–0.58% of adsorbed Hg (Xue et al., 2013). Based on the current mass balance, the net release of Hg from the Bs horizon via seepage water (2.07 μg m−2) may account for approximately 5.9% of the readily mobilisable pool (35 μg m−2, 15–50 cm depths).
Mercury fractionation in tropical soils: A critical point of view
2020, ChemospherePretreatment with Ochrobactrum immobilizes chromium and copper during sludge pyrolysis
2020, Ecotoxicology and Environmental SafetyCitation Excerpt :The FTIR peak adjacent to the wavenumber of 1541.73 cm−1 corresponds to amino N–H/C–N (Zhou et al., 2014); the FTIR peak of this functional group in the samples supplemented with the bacterial solution was sharply increased. The FTIR peak adjacent to the wavenumber of 779.05 cm−1 and 536.70 cm−1 belongs to Si–O (Xue et al., 2013); these peaks were shifted after the addition of the bacterial solution or culture medium suggesting that silicon may act as a “bridge”. The FTIR peak adjacent to the wavenumber of 694.26 cm−1 belongs to O–Si–O (Huang et al., 2016); this peak had a large displacement after pyrolysis emerging only in the samples supplemented with the bacterial solution.
Determination of (Bio)-available mercury in soils: A review
2020, Environmental PollutionCitation Excerpt :For example, Tipping et al. (2011) reported that the emissions of Hg0 from the UK soils to the global atmosphere is almost 50% greater than its emissions from all primary anthropogenic sources. In addition, a considerable fraction of soil Hg can potentially accumulate in plants and crops e.g. rice (Zhang et al., 2010a) or migrate to ground and surface waters (Xue et al., 2013). Estimating the total concentrations of metal(loid)s in soil is often a poor indicator of their health and ecological risks.
Establishing soil adsorption testing methods for gaseous mercury and evaluating the distribution coefficients of silica sand, decomposed granite soil, mordenite, and calcium bentonite
2020, Soils and FoundationsCitation Excerpt :For example, the soil adsorption abilities of decomposed granite soils, incineration ashes, and activated carbons were investigated using aqueous mercuric chloride liquids in Japan. In other countries, the abilities for forest soils, humic acids, marine sediments, and bentonites, have been investigated (Liang et al., 2012; Reis et al., 2016; Xue et al. 2013; Yang et al., 2008; Yin et al., 1997; Zhang, et al. 2009). According to these reports, the distribution coefficients of soils against aqueous mercuric chloride liquids were on the order of hundreds of mL/g for sandy soils, several thousand mL/g for clay soils and humic acids, and tens of thousands of mL/g for activated carbons.
Supported by the National Natural Science Foundation of China (Nos. 30970166 and 40801088), the Science and Technology Program for Environmental Protection of Shandong Province, China (No. 2006007), and the Research Award Fund for Outstanding Young Scientists of Shandong Province, China (No. 2007BS08001).