[Characteristics of DNA adsorption on different sizes red soil colloidal particles].

Ying Yong Sheng Tai Xue Bao

College of Environmental and Resource Science, Zhejiang University, Hangzhou, China.

Published: March 2013

By using balance reaction method, this paper studied the adsorption characteristics and thermodynamic properties of DNA on four kinds of red soil colloids (organic matter-contained coarse clay, organic matter-removed coarse clay, organic matter-contained fine clay, and organic matter-removed fine clay). The DNA adsorption on the four red soil colloids was a process of fast reaction, and the adsorption isotherms were conformed to the Langmuir equation, with the corresponding correlation coefficient (r2) being 0.974, 0. 991, 0. 958, and 0. 975, respectively. The maximum adsorption amount of DNA on the colloidal particles followed the order of organic matter-contained fine clay > organic matter-removed fine clay > organic matter-contained coarse clay > organic matter-removed coarse clay, implying that the size and organic matter content of colloidal particles played an important role in DNA adsorption. Electrolyte concentration and type and adsorption system pH were the main factors affecting the DNA adsorption on the four soil colloids. Within a definite electrolyte concentration range (NaCl < 60 mmol . L-1 and CaCl2 <10 mmol L-1) , the adsorption amount of DNA on the red soil colloids increased significantly with the increase of electrolyte concentration. As compared with sodium ion, calcium ion had a greater promotion effect on the DNA adsorption, but the effect decreased significantly with the increase of adsorption system pH. The DNA adsorption on the organic matter-contained red soil colloids was an endothermic reaction, while the DNA adsorption on the organic matter-removed red soil colloids was an exothermic reaction. The DNA adsorption on the red soil colloids was a process of entropy increase.

Download full-text PDF

Source

Publication Analysis

Top Keywords

clay organic
24
dna adsorption
16
organic matter-contained
16
coarse clay
16
organic matter-removed
16
fine clay
16
red soil
12
soil colloids
12
organic
9
adsorption
8

Similar Publications

Relaxation process of photoexcited berberine via aggregation and dissociation state-dependent intramolecular electron transfer.

Photochem Photobiol Sci

December 2024

Department of Applied Chemistry for Environment, Graduate School of Urban Environmental Sciences, Tokyo Metropolitan University, 1-1 Minami-Osawa, Hachioji-Shi, Tokyo, 192-0397, Japan.

The fluorescence quantum yield of berberine in aqueous solution is significantly smaller than those of organic solution. The time profile of fluorescence intensity of berberine was analyzed by a bi-exponential function, showing that two kinds of states of berberine exist in the solutions. The observed fluorescence lifetime of shorter lifetime species of berberine in water (0.

View Article and Find Full Text PDF

The incorporation of photoactive organic dyes into layered inorganic materials enhances their optical and chemical properties, making them ideal for sensing applications. In this study, Bisindolyl methane (BIM)-based neutral probes were integrated with bentonite clay to explore their sensing capabilities. Probe 1 (unoxidized BIM) and Probe 2 (oxidized BIM) generally exhibited quenched luminescence in solution due to intramolecular rotations.

View Article and Find Full Text PDF

Land use conversion from natural forests to grassland, plantation forests, mono-cropping coffee and croplands is a significant causes of soil degradation, leading to aggravate soil acidity and nutrient depletion. However, there is limited information regarding comprehensive effect of land use conversion on soil fertility and acidity in western Oromia Region of Ethiopia. Hence, this study aims to assess the surface soil fertility and acidity across different land use types (forest, crop, eucalyptus land, grazing land, and coffee farmland) to provide management options.

View Article and Find Full Text PDF

The retention and mobility of arsenic (As) in soil depend on various physical and chemical factors. The knowledge of the sorption-desorption chemistry of As in soil is necessary for predicting the fate and behavior of As in soil environments. Therefore, this study assessed different organic (sugarcane bagasse and vermicompost) and inorganic amendments (steel slag and fly ash) for their impact on sorption-desorption of As in texturally different contaminated soils (of sandy clay (SC) and sandy clay loam (SCL) texture) to understand the effect of amendments on As retention and mobility.

View Article and Find Full Text PDF

Oxidation states and distribution of arsenic (As) in annually laminated (varved) lacustrine deposits were analyzed with a seasonal resolution. This deposit was formed in the mid-Holocene landslide-dammed paleolake in the upper reaches of the Ane River, central Japan and the paleolake watershed consists of the Jurassic accretionary complexes (Mino-Tamba belt) including sedimentary and igneous rocks. In the outcrop, centimeter-to-decimeter-scale silty clay layers alternating with laminated layers are well developed.

View Article and Find Full Text PDF

Want AI Summaries of new PubMed Abstracts delivered to your In-box?

Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!