CARBON BONDED SULPHUR IN SELECTED QUEBEC SOILS

1963 ◽  
Vol 43 (1) ◽  
pp. 151-155 ◽  
Author(s):  
L. E. Lowe ◽  
W. A. DeLong
Keyword(s):  
Organic Soils ◽  
Mineral Surface ◽  
Surface Soils ◽  
Total Sulphur ◽  
Mineral Soils

Details are given of a procedure for the determination of carbon bonded sulphur in soils and soil extracts.Significant amounts of carbon bonded sulphur were found in a few selected Quebec soils. Organic soils contained substantially more carbon bonded sulphur than mineral soils, and also a higher proportion of the total sulphur was in a carbon bonded form in the organic (47–58 per cent) than in the mineral soils (12–35 per cent).The distribution of carbon bonded sulphur between acid-extractable, alkali-extractable and non-extractable fractions was determined on the same samples. The recovery of carbon bonded sulphur in these fractions was high in the organic soils, but 16–48 per cent was not accounted for in three mineral surface soils. For all samples, very little carbon bonded sulphur was non-extractable and, in all samples, except a podzol B21 horizon, more of this sulphur fraction was extracted by alkaline than by acid extraction.The importance of this fraction as a source of sulphur for plants cannot yet be assessed.

scholarly journals Sulphur status in Finnish cultivated soils

1973 ◽  
Vol 45 (2) ◽  
pp. 121-215
Author(s):  
Johan Korkman
Keyword(s):  
Ammonium Acetate ◽  
Induction Furnace ◽  
Soil Samples ◽  
Total Sulphur ◽  
Sulphate Sulphur ◽  
Close Relationship ◽  
Mineral Soils ◽  
Sulphur Uptake ◽  
Cultivated Soils

A method for determining total sulphur in plant material and soil samples using the induction furnace technique and subsequent turbidimetric determination of sulphate sulphur was discussed. A procedure for extracting sulphur from soil samples with ammonium acetate (pH 4.65), the interference of the organic matter being reduced by oxidation of the extract with H2O2, was proposed. Sulphur balance in Finnish cultivated soils was estimated by taking into account the average amounts of emitted (8 kg S/ha/yr.), precipitated (8 kg S/ha/yr.) and leached (8 kg S/ha/yr.) sulphur. The actual situation in the cultivated soils seems thus to be depending, on an average, on the uptake by plants and the sulphur applied (12 kg S/ha/yr. in the early 1970s). In 104 samples of cultivated soil, the content of total sulphur showed a slight correlation with the content of organic carbon. The amounts of sulphur extracted in various ways were not predictable by means of the soil characteristics used (pHCaCl2, org. C and texture). Extracted sulphur did not correlate sufficiently with the development and sulphur uptake of plants. Under field conditions in northern Finland, sulphur application produced a relatively distinct result in respect both to the ley yields on Carex peat, and their sulphur content. On mineral soils in southern Finland the yields were unaffected by supplementary fertilization with sulphur. In the pot experiments performed a fairly close relationship between sulphur and nitrogen was demonstrated.

scholarly journals Príspevok k problematike určovania špecifickej hmotnosti subhorizontov opadu lesných pôd

2013 ◽  
Vol 59 (1) ◽  
pp. 38-43
Author(s):  
Jana Bútorová
Keyword(s):  
Mineral Soil ◽  
Soil Aggregate ◽  
Soil Samples ◽  
Organic Soils ◽  
Laboratory Methods ◽  
Elementary Unit ◽  
Final Density ◽  
International Laboratory ◽  
Mineral Soils

Abstract According to national and international laboratory methods, the density of soil samples is determined by pycnometer in heated samples crushed by ultrasound. In mineral soils, the elementary unit of density is represented by a mineral grain of quartz, granite, andesite, etc. On the other hand, in organic soils, the elementary unit is represented by a leaf (or just a part of it), needles, stems and roots. Heating of the mineral grain causes its release from the soil aggregate. Organic parts of the soil are losing air vacuoles by heat treatment while in the same time, carbohydrates, proteins, oils and resins create new chemicals which are heavier than water. That is a reason why density determination of litter subhorizons in forest soils needs to have different rules in comparison with mineral soil samples. Samples with more than 50 volume per cent of organic matter are not treated by heat and do not decompose. In case of high mineral soil content, mineral parts are removed from the sample and their density is determined. The final density is based on mathematically processed data.

scholarly journals A New Approach to the Determination of Mineral and Organic Soil Types Based on Dilatometer Tests (DMT)

2018 ◽  
Vol 8 (11) ◽  
pp. 2249 ◽  
Author(s):  
Simon Rabarijoely
Keyword(s):  
Pore Water Pressure ◽  
Water Pressure ◽  
Organic Soil ◽  
Soil Types ◽  
Organic Soils ◽  
New Classification ◽  
New Approach ◽  
Mineral Soils ◽  
Material Index

In order to identify the soil type in the ground, Marchetti’s nomogram chart is commonly used on the basis of dilatometer tests (DMT). In this chart, the material index values (ID) and the dilatometer modulus (ED) are used to determine the state and type of soils predominant in mineral soils. Unfortunately, this classification is not accurate enough for the identification of organic soils. This article proposes a new classification based on a nomogram chart for both mineral soils and organic soils using (p0), (p1) readings and pore water pressure (uo).

Determination of total sulphur in naphthas

The Analyst ◽  
1977 ◽  
Vol 102 (1215) ◽  
pp. 414 ◽  
Author(s):  
T. Fernández ◽  
J. M. Rocha ◽  
N. Rufino ◽  
A. García Luis
Keyword(s):  
Total Sulphur

scholarly journals Calcium, magnesium and potassium in mineral soils from the southern half of Finland

1973 ◽  
Vol 45 (3) ◽  
pp. 254-261
Author(s):  
Armi Kaila
Keyword(s):  
Clay Content ◽  
Total Content ◽  
Fine Sand ◽  
Clay Soils ◽  
Surface Layers ◽  
Surface Soils ◽  
Exchangeable Ca ◽  
Heavy Clay ◽  
Southern Half ◽  
Mineral Soils

210 samples of mineral soils from the southern half of Finland with mainly an acid precambrian bedrock, were analysed for the total contents of Ca, Mg and K, and for the portion of these nutrients which could be exchanged by N NH4OAc (pH 7), dissolved by 0.1 N HCI at room temperature, or released by N HCI at 50° C. The total content of Ca was lowest in samples of heavy clay, 0.78±0.14 % in the surface soils and 0.92±0.10 % in the deeper layers. The mean content in the groups of other soils was at least about 1.1 %. The total content of Mg increased with an increase in the clay content (r = 0.81***). It ranged from 0.6±0.1 % in the sand and fine sand samples to 1.53±0.19 % in the heavy clay soils of the surface layers and to 1.89±0.12 % in those of the deeper layers. Also in the groups of loam and silt soils and of the coarser clay soils, respectively, the Mg content was in the deeper layers higher than in the surface soils. The total content of K also increased with the clay content (r=0.73***) from 1.7±0.1 % in the sand and fine sand soils to 2.74±0.21 % in the heavy clay soils of the surface layers and to 3.10±0.07 % in those of the deeper layers. The portion of exchangeable Ca was relatively high: in the groups of surface soils from more than one tenth to one third of the total amount. The corresponding average amounts released by even the more drastic treatment with acid were not markedly higher. Only a few per cents of total Mg were exchangeable and slightly higher amounts were dissolved by 0.1 N HCI, whereas the treatment with N HCI at 50° C released about half of the total Mg. Exchangeable K and K dissolved by 0,1 N HCI did not exceed 1 % of the total K, except slightly in the heavy clay soils; the average amounts released by N HCI ranged from 5 to 18 % of the total K. The plant availability of these nutrients was discussed.

scholarly journals The determination of total sulphur in India rubber

1912 ◽  
Vol 8 (3) ◽  
pp. 445 ◽  
Author(s):  
C.E. Waters ◽  
J.B. Tuttle
Keyword(s):  
Total Sulphur
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