Spectroscopic and Kinetic Study of Sucrose Oxidation by Cr(VI) and Its Application in the Quantitative Analysis of Soil Organic Carbon
International Research Journal of Pure and Applied Chemistry,
Page 1-15
DOI:
10.9734/irjpac/2022/v23i430467
Abstract
The percent organic carbon (%OC) is an important soil fertility measure that has important implications in agricultural productivity and food security. In this study, a UV-visible spectrophotometric technique was investigated and applied to quantify %OC from selected soil samples along a river basin that traverses agricultural farmlands, a forest and sewage treatment lagoons for a comparative survey purposes. The study was based on the measurement of absorbance of Cr(III) species that arise from oxidation of sucrose (which is 42.11% carbon) by dichromate ions which contain Cr(VI) species. The uv-visible spectrophotometric double beam wavelength scan measurements elucidated the conversion of Cr(VI) to Cr(III) ions and a calibration plot was developed with r2= 0.99. The analyte peak was identified in the region from 750 nm to 550 nm (the absorbing Cr(iii) species) with a turning point maximum at 576 nm. The kinetic profile of sucrose oxidation by the dichromate ions was studied via absorbance of Cr(III) and Cr(VI) as a function of the reaction time and was used to characterize the reaction model. The absorbance of Cr(III) as a function of reaction time fitted best into the non-linear Belehradek power function equation y=a(x-b)c,, where y = absorbance; x = time(s); a, b, c = are constants (r2 of 0.91). Kinetic analysis revealed that the reaction that leads to the formation of Cr(III) during sucrose oxidation proceeds via pseudo first-order kinetics (r2= 0.83). A comparative quantitative analysis indicated that the sewage treatment lagoons had the highest %OC content at about 5.5-6.6%OC. The soils sampled from the forest regions had about 4.6-5.8%OC whereas the river bank soils had the lowest levels at about 2.0-2.5%OC. A statistical t-test analysis showed that the %OC levels in sub-soils were significantly higher than those of the top-soils (p > 0.05 at 95% CI).
Keywords:
- UV-Vis spectroscopy
- kinetics
- sucrose oxidation
- organic carbon
- chromium(VI)
How to Cite
References
Lauterbach F, Abetz V. Continuous Kinetic Sampling of Flow Polymerizations via Inline UV–Vis Spectroscopy. Macromol. Rapid Commun. 2020;41(9):2000029.
Begum R, Farooqi ZH, Naseem K, Ali F. Applications of UV / Vis Spectroscopy in Characterization and Catalytic Activity of Noble Metal Nanoparticles Fabricated in Responsive Polymer Microgels : A Review. Crit. Reviwes Anal. Chem. 2018;48(6): 503–516.
Ben Salah M, Aouadhi C, Khadhri A. Green Roccella Phycopsis Ach. Mediated Silver Nanoparticles: Synthesis, Characterization, Phenolic Content, Antioxidant, Antibacterial and Anti-Acetylcholinesterase Capacities. Bioprocess Biosyst. Eng. 2021;44(11): 2257–2268.
Angheluta A, Guizani S, Saunier J, Rönnback R. Application of Chemometric Modelling to UV-Vis Spectroscopy: Development of Simultaneous API and Critical Excipient Assay in a Liquid Solution Continuous Flow. Pharm. Dev. Technol. 2020;25(8):919–929.
Perkampus H-H. UV–VIS Spectroscopy, 1st ed.; H. Charlotte Grinter and Dr. T. L. Threlfall, Ed.; Springer -Verlag: Berlin; 1992.
Pluczyk S, Vasylieva M, Data, P. Using Cyclic Voltammetry, UV-Vis-NIR, and EPR Spectroelectrochemistry to Analyze Organic Compounds. J. Vis. Exp. 2018; 140:56656.
Blanco-Canqui H, Shapiro CA, Wortmann CS, Drijber RA, Mamo M, Shaver TM, Ferguson RB. Soil Organic Carbon: The Value to Soil Properties. J. Soil Water Conserv. 2013;68(5):2–3.
Obalum SE; Chibuike GU, Peth S, Ouyang Y. Soil Organic Matter as Sole Indicator of Soil Degradation. Environ. Monit. Assess. 2017;189(4):176.
Ondrasek G, Bakić Begić H, Zovko M, Filipović L, Meriño-Gergichevich C, Savić R, Rengel, Z. Biogeochemistry of Soil Organic Matter in Agroecosystems & Environmental Implications. Sci. Total Environ. 2019;658:1559–1573.
Baveye PC, Schnee LS, Boivin P, Laba M, Radulovich R. Soil Organic Matter Research and Climate Change: Merely Re-Storing Carbon Versus Restoring Soil Functions. Front. Environ. Sci. 2020;8 (September):1–8.
Van Meter RJ, Glinski DA, Henderson WM, Purucker ST. Soil Organic Matter Content Effects on Dermal Pesticide Bioconcentration in American Toads (Bufo Americanus). Environ. Toxicol. Chem. 2016; 35(11):2734–2741.
De Souza DM, Morais PA. de O, Matsushige I, Rosa LA. Development of Alternative Methods for Determining Soil Organic Matter. Rev. Bras. Cienc. do Solo 2016;40:1–17.
Escalona Y, Petrov D, Oostenbrink C. Vienna Soil Organic Matter Modeler 2 (VSOMM2). J. Mol. Graph. Model. 2021; 103:107817.
Jollymore A, Johnson MS, Hawthorne I. Submersible UV-Vis Spectroscopy for Quantifying Streamwater Organic Carbon Dynamics: Implementation and Challenges before and after Forest Harvest in a Headwater Stream. Sensors 2012;12(4): 3798–3813.
Available:https://doi.org/10.3390/s120403798.
Hamada YZ, Bayakly N, Shafi M, Painter S, Taylor V, Greene J, Rosli K. Reactions of Cr(3+) with Aspartic Acid within a Wide PH Range. Complex Met. 2014;1(1):46–51.
Soares R, Carneiro MC, Monteiroa MIC, Henriquae S. de S, Pontes FVM, Dias da Silva LI, Neto AA, Santelli RE. Simultaneous Speciation of Chromium by Spectrophotometry and Multicomponent Analysis. Chem. Speciat. Bioavailab. 2009; 21(3):153–160.
Scientist F. Florida Academy of Sciences , Inc . Reaction of chromium (VI) wastes with sugars Author (s): Chuhua Wang , Dean F . Martin and Barbara B . Martin Published by : Florida Academy of Sciences , Inc . 2021;62(1):48–57.
Available:https://Www.Jstor.Org/Stable/24320961.
Ravikumar P, Somashekar RK. Evaluation of Nutrient Index Using Organic Carbon, Available P and Available K Concentrations as a Measure of Soil Fertility in Varahi River Basin , India. 2013; 3(4):330–343.
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