2016
DOI: 10.1590/18069657rbcs20150150
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Development of Alternative Methods for Determining Soil Organic Matter

Abstract: Soil organic matter (SOM) is important to fertility, since it performs several functions such as cycling, water and nutrient retention and soil aggregation, in addition to being an energy requirement for biological activity. This study proposes new trends to the Embrapa, Walkley-Black, and Mebius methods that allowed the determination of SOM by spectrophotometry, increasing functionality. The mass of 500 mg was reduced to 200 mg, generating a mean of 60 % saving of reagents and a decrease of 91 % in the volume… Show more

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Cited by 15 publications
(22 citation statements)
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“…However, the quantification of reduced chromium is made through ultraviolet-visible light absorbance using a spectrophotometer. The present study followed the procedure of Souza et al, (2016) with a minor increase in soil volume as SOC tends to be low in soils of south central Idaho. A brief description of the method follows.…”
Section: Walkley-black Spectrophotometric Methodsmentioning
confidence: 99%
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“…However, the quantification of reduced chromium is made through ultraviolet-visible light absorbance using a spectrophotometer. The present study followed the procedure of Souza et al, (2016) with a minor increase in soil volume as SOC tends to be low in soils of south central Idaho. A brief description of the method follows.…”
Section: Walkley-black Spectrophotometric Methodsmentioning
confidence: 99%
“…The color of each sample is related to organic C through a standard curve generated by adding increasing amounts of ferrous ammonium sulfate to reduce dichromate in standard flasks treated otherwise identically to unknowns (S2). This method of SOC determination is also subject to incomplete oxidation of SOC (Souza et al, 2016); therefore, the standard correction factor of 1.33 was applied.…”
Section: Walkley-black Spectrophotometric Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…Soil organic carbon was determined by oxidation using potassium dichromate and concentrated sulphuric acid. Considering that the average content of carbon in soil organic matter is equal to 58 % the conversion factor 1.724 was used to calculate the percentage of organic matter from the content of organic carbon [8,9]. Nitrogen content of the soil was determined using method describe by Kjeldahl [10] while the phosphorus content using molybdate reagent by means of spectrophotometer set at wavelength of 660 nm then the cation exchange capacity was estimated using the Bray and Kurtz Hydrometer method [7,11].…”
Section: Determination Of Soil Physiochemical Parametersmentioning
confidence: 99%
“…In clay rich soils it enables the formation of aggregates with large pores and improves therefore water and air availability. Besides being essential in soil studies, the soil organic matter parameter is the most important one in several soil properties such as structure, coloring, water retention, and cation exchange capacity; as a result it becomes important in guiding soil fertilizing and irrigation (Souza et al, 2016).…”
Section: Introductionmentioning
confidence: 99%