Adsorption of Organic Matter at Mineral/Water Interfaces. 2. Outer-Sphere Adsorption of Maleate and Implications for Dissolution Processes

Langmuir ◽  
2004 ◽  
Vol 20 (12) ◽  
pp. 4996-5006 ◽  
Author(s):  
Stephen B. Johnson ◽  
Tae Hyun Yoon ◽  
Benjamin D. Kocar ◽  
Gordon E. Brown
Langmuir ◽  
2005 ◽  
Vol 21 (14) ◽  
pp. 6356-6365 ◽  
Author(s):  
Stephen B. Johnson ◽  
Gordon E. Brown, ◽  
Thomas W. Healy ◽  
Peter J. Scales

2019 ◽  
Vol 5 (11) ◽  
pp. 1985-1992 ◽  
Author(s):  
Nor Elhouda Chadi ◽  
Slimane Merouani ◽  
Oualid Hamdaoui ◽  
Mohammed Bouhelassa ◽  
Muthupandian Ashokkumar

We have recently reported that the reaction of H2O2/IO4− could be a new advanced oxidation process for water treatment [N. E. Chadi, S. Merouani, O. Hamdaoui, M. Bouhelassa and M. Ashokkumar, Environ. Sci.: Water Res. Technol., 2019, 5, 1113–1123].


Langmuir ◽  
2008 ◽  
Vol 24 (13) ◽  
pp. 6683-6692 ◽  
Author(s):  
Juyoung Ha ◽  
Tae Hyun Yoon ◽  
Yingge Wang ◽  
Charles B. Musgrave ◽  
Gordon E. Brown, Jr.

2019 ◽  
Vol 83 (1) ◽  
pp. 107-117
Author(s):  
Yuzhen Liang ◽  
Yang Ding ◽  
Pei Wang ◽  
Guining Lu ◽  
Zhi Dang ◽  
...  

2017 ◽  
Vol 105 (12) ◽  
Author(s):  
Ping Li ◽  
Hanyu Wu ◽  
Jianjun Liang ◽  
Zhuoxin Yin ◽  
Duoqiang Pan ◽  
...  

AbstractThe sorption of Eu(III) on potassium feldspar (K-feldspar) was studied under various physicochemical conditions such as pH, temperature, counter ions and organic matter. The results showed that the sorption of Eu(III) on K-feldspar significantly increased with the increase of pH, and high Eu(III) concentration can inhibit such immobility to some extent. The presence of humic acid (HA) can increase the sorption of Eu(III) on K-feldspar in low pH range; while inhibit to a large extent under alkaline conditions. It is very interesting that at pH ~6.5, high ionic strength can promote the sorption of Eu(III) on K-feldspar in the presence of HA. In contrast, Eu(III) sorption was restricted obviously by NaCl in the absence of HA. The sorption procedure was involved with ion exchange and/or outer-sphere complexation as well as inner-sphere complexation. The presence of F


2006 ◽  
Vol 6 (6) ◽  
pp. 155-164 ◽  
Author(s):  
X.H. Guan ◽  
D.L. Li ◽  
C. Shang ◽  
G.H. Chen

This paper presented the current state of our understanding of the roles of carboxylic and phenolic groups in NOM adsorption and reviewed the contradictory opinions in the literatures. Previous studies carried out by other researchers indicated that aromatic carboxylates were adsorbed onto metal (hydr)oxides via outer-sphere complexes under most conditions and phenolic groups were very crucial for formation of inner-sphere complexes between organic acids and metal (hydr)oxides. Adsorption test with in-situ ATR-FTIR spectroscopic investigation were carried out to verify the role of aromatic carboxylic and phenolic groups in the NOM adsorption onto aluminium hydroxide surfaces by using a series of aromatic carboxylic acids and dihydroxybenzoic acids as the surrogate of NOM. Our studies suggested that the formation of outer-sphere complexes dominated the adsorption of most of the aromatic carboxylates over the pH range of 5–9; inner-sphere complexes were only detected at some pH levels for some aromatic carboxylates adsorption; and the aromatic carboxylates were most likely to be adsorbed to the first surface layer of hydroxyl groups and water molecules without forming coordinative bonds with the aluminium hydroxide surfaces but strong hydrogen bonds were formed in this process. Our study also revealed that (1) the presence of phenolic groups can increase the interaction strength of carboxylate groups with aluminium hydroxide; (2) chelate formation involving a carboxylate oxygen atom and ortho-phenolic-oxygen is important for the adsorption of organic matter on aluminium hydroxide at acidic pH; and 3) the phenolic groups adjacent to each other are more important than the carboxylic groups at alkaline pH for organic matter adsorption.


2009 ◽  
Vol 89 (5) ◽  
pp. 603-610 ◽  
Author(s):  
H Sun ◽  
M Nelson ◽  
F Chen ◽  
J Husch

Water loss from soil minerals has been known to cause errors in the determination of soil organic matter when the loss on ignition (LOI) method is used. Unfortunately, no known published studies reliably quantify the range of structural water in the soil. To do this, 15 common reference minerals were analyzed by LOI to obtain their individual water loss. In addition, 14 upland, loamy soil samples and 3 wetland/hydric soil samples with varied mineral contents were analyzed to collect their X-ray powder diffraction spectra. Based upon X-ray spectra peak intensities, the modal abundance of minerals in each soil sample was determined using the RockJock computer program. The resultant modal weight percentages of all identified minerals in each soil sample were then multiplied by the LOI value for each mineral to obtain the mineral structural water loss (SWL) of that soil sample. For the 17 soil samples analyzed, the range of mineral water loss is 0.56 to 2.45%. Depending on the LOI values of the soil samples, the SWL:LOI ratios range from 0.04 to around 1.00. The SWL:LOI ratios are particularly low for top wetland soil when the LOI value is higher. The ratios are lower for surface soil samples than for subsurface soil samples because of the high LOI values in surface soil samples. Understanding soil mineral water loss and its relation to the LOI patterns from various environments is important for the accurate evaluation of soil organic matter when the LOI method is used. Key words: Mineral, structural water, loss on ignition


2018 ◽  
Vol 15 (30) ◽  
pp. 201-209
Author(s):  
A. C. C. SILVA ◽  
G. L. G. SOUZA ◽  
J. R. C. ROCHA

Nitrogen is an important chemical element due to biological reactions, including nutrient cycling. This process transforms organic matter into food for plants and other organisms. Some species can absorb the ammonium ion, but this one presents high toxicity. The portion that is most absorbed is nitrate due to its low toxicity, which is generally found in soils, industrial flows and fertilizers. However, the ion presents a danger to human health when present in concentrations higher than 10mg L-1 of N-NO3-, as determined by Resolution 357/2005 of CONAMA in meat, mineral water and aquatic environments. In the present study conducted in rivers of the cities of Paranaguá and Pontal do Paraná, the ion was determined spectrophotometrically at 545nm by the Griess method, with pre-reduction of the nitrate in nitrite, using the metallic zinc as a reducing agent. All the samples evaluated presented values below the limit recommended by CONAMA. These values ranged from 0.03 to 0.69mg L-1 in the low season (September 2016) and 0.00 to 0.07mg L-1 in the high season (March / 2017). The obtained results were compared to others published and that present characteristics similar to the evaluated rivers. It was observed that NO3- concentrations have been increasing continuously, even in small proportions, confirming the occurrence of the eutrophying process.


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