Adsorption-desorption of maleic hydrazide on mineral soil components

1991 ◽  
Vol 26 (2) ◽  
pp. 165-183 ◽  
Author(s):  
M. C. Hermosin ◽  
I. Roldan ◽  
J. Cornejo
2020 ◽  
Vol 85 (6) ◽  
pp. 809-819
Author(s):  
Rada Djurovic-Pejcev ◽  
Svjetlana Radmanovic ◽  
Zorica Tomic ◽  
Lazar Kaludjerovic ◽  
Vojislava Bursic ◽  
...  

Studies of adsorption and desorption of pesticides by soils are important for understanding and predicting their fate and transmission in the environment. Considering the agricultural and environmental relevance of clomazone, its sorption?desorption behaviour was studied in two widespread Serbian agricultural soil types named Regosol and Chernozem. Both phenomena are well-described by the Freundlich equation, which shows that clomazone is generally sorbed more to organic matter than to the mineral soil fractions. Chernozem, a soil containing more of both organic matter and clay, was found to bind more, and desorb less herbicide, than Regosol. Higher desorption hysteresis obtained for Chernozem could be attributed to its larger number of high- -energy sorption sites, compared to Regosol. In both soils, the hysteresis effect increases with the rise of initial clomazone concentration in the soil-water system, while the percentage of desorbed amount during successive desorption cycles decreases. The presented adsorption?desorption study shows that soil composition plays an important role in clomazone behaviour and fate in the environment, and a significantly reduced probability of contamination of both the deeper soil layers and groundwater may be expected when this herbicide is found in humus-rich soils


HortScience ◽  
1993 ◽  
Vol 28 (2) ◽  
pp. 126-128 ◽  
Author(s):  
Glenn R. Wehtje ◽  
Charles H. Gilliam ◽  
Ben F. Hajek

Adsorption of 14C-labeled oxadiazon was evaluated in three soilless media and a mineral soil at concentrations between 0.1 and 100 mg·kg-1. Adsorption, which was at least 96%, was not influenced by absorbent type (medium vs. soil) or by oxadiazon concentration. However, desorption was greater in the media than in the soil. After five water extractions, 5.4% of the applied oxadiazon was recovered from media, but only 0.4% was recovered from the soil. In the soil and in two of the media, leaching with water failed to displace oxadiazon 2 cm below the surface to which it had been applied. No oxadiazon was detected below 4 cm in the third medium. Oxadiazon is sufficiently adsorbed to resist leaching-based displacement. Oxadiazon is not likely to enter the environment by escaping from treated containers. Chemical name used: 3-[2,4-dichloro-5-(1-methylethoxy)phenyl]-5-(1,1-di-methylethyl)-1,3,4-oxadiazol-2-(3H)-one (oxadiazon).


2006 ◽  
Vol 39 (11) ◽  
pp. 1198-1207 ◽  
Author(s):  
A. A. Shinkarev ◽  
M. K. Latypov ◽  
K. G. Giniyatullin ◽  
M. G. Khramchenkov

Author(s):  
Jerzy Weber ◽  
Elżbieta Jamroz ◽  
Andrzej Kocowicz ◽  
Magdalena Debicka ◽  
Jakub Bekier ◽  
...  

AbstractHumic substances, including humin fraction, play a key role in the fate of organic and inorganic xenobiotics contaminating the environment. Humin is an important fraction of humic substances, which has been the least studied to date. This is due to the difficulties connected with its isolation that pose a number of methodological problems. Methods of humin fraction isolation can be divided into following main groups: (1) digestion of mineral soil components with HF/HCl followed by alkali extraction of HA and FA; (2) alkali extraction of HA and FA followed by extraction of humin by different organic solvents; and (3) alkali extraction of HA and FA followed by HF/HCl digestion of mineral soil components. Nevertheless, each of these methods has different limitations. We described in detail a useful procedure of humin isolation, in which this fraction was not extracted, but isolated from the soil by removing its soluble organic and mineral components. A modified method of HA and FA extraction with 0.1 M NaOH, according to the International Humic Substances Society, was used in the first step. Then, the mineral components in the residue were digested with the 10% HF/HCl. Unlike the procedures oriented to increase the concentration of organic matter, samples were treated several times with the HF/HCl mixture until the mineral fraction was almost completely digested. The main assumption of the method modification was to obtain the highest yield with the lowest possible ash content, but without affecting humin chemical structure. The results showed that the proposed procedure is characterized by a high efficiency and recovery and, therefore, it can be used to isolate high amounts of humin from soil.


1971 ◽  
Vol 68 ◽  
pp. 29-33 ◽  
Author(s):  
Bernard Weber ◽  
Albert Cassuto

1977 ◽  
Vol 27 (5) ◽  
pp. 611-617
Author(s):  
Walter T. Smith ◽  
Charles F. Mayer ◽  
Chyung S. Kook ◽  
John M. Patterson
Keyword(s):  

1983 ◽  
Vol 139 (4) ◽  
pp. 736
Author(s):  
V.N. Ageev ◽  
E.Ya. Zandberg ◽  
N.I. Ionov ◽  
A.Ya. Tontegode

2015 ◽  
Vol 14 (1) ◽  
pp. 66-72 ◽  
Author(s):  
Seo-Hyun Pak ◽  
◽  
Myung-Seop Shin ◽  
Hyun-Jung Kim ◽  
Yong-Woo Jeon

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