Relationships between three measures of organic matter or carbon in soils of eucalypt plantations in Tasmania

Soil Research ◽  
1996 ◽  
Vol 34 (4) ◽  
pp. 545 ◽  
Author(s):  
XJ Wang ◽  
PJ Smethurst ◽  
AM Herbert
Keyword(s):  
Organic Matter ◽  
Complete Recovery ◽  
Parent Material ◽  
Wet Oxidation ◽  
Loss On Ignition ◽  
Structural Water ◽  
Parent Materials ◽  
Eucalypt Plantations ◽  
Highly Correlated ◽  
Dry Combustion

Organic carbon or organic matter in acidic Tasmanian soils supporting eucalypt plantations was measured by dry combustion using a LECO CHIN-1000 Analyzer (CT), wet oxidation by the Walkley-Black method (CW&B), and loss-on-ignition (LOI at 375°C). CT and CW&B were highly correlated in 119 surface and subsoil samples, and on average, CW&B provided near complete recovery of CT (97%). Although LOI may have released some structural water from the fine-textured soils, and apart from granite-derived soils which need further study, strong regressions were found between LOI and both CW&B and CT which were specific for either basalt or non-basalt soils. Within the non-basalt soils, parent material had little effect on these relationships, although there were large differences in C concentrations of surface soils between soils of different parent materials. The relationships of CW&B and CT to LOI in the basalt soils were significantly different from those in the non-basalt soils.

EFFECTS OF HISTORICAL LAND CLEARING ON ORGANIC MATTER AND NITROGEN LEVELS IN SOILS OF THE FRASER LOWLAND OF BRITISH COLUMBIA, CANADA AND WASHINGTON, U.S.A.

1990 ◽  
Vol 70 (4) ◽  
pp. 583-592 ◽  
Author(s):  
ALAN GOLDIN ◽  
L. M. LAVKULICH
Keyword(s):  
Organic Matter ◽  
The United States ◽  
Parent Material ◽  
Aerial Photographs ◽  
Parent Materials ◽  
Land Clearing ◽  
Nitrogen Levels ◽  
Glacial Outwash ◽  
International Boundary ◽  
Air Photo

Two soils derived from glacial deposits and one from alluvium were examined for changes in organic matter (OM) and nitrogen levels between 1943 and 1983 across the international boundary in the Fraser Lowland of western North America. Duplicate samples were collected from the upper 0.2 m from 60 randomly selected sites on the five land clearing periods (1943–1955, 1955–1966, 1966–1976, 1976–1983, uncleared) on each of three parent materials: glacial outwash, alluvium, and glacialmarine deposits in the United States and Canada. The land clearing periods were determined from medium scale aerial photographs taken in 1943, 1955, 1966, 1976, and 1983. Cultivation results in a 20% loss of OM after 35 yr on all soils. The largest loss is in the first 15 yr on all soils. Changes in N levels on the three parent materials is irregular. C:N narrows on all soils from about 15:1 to about 12:1. Key words: Organic matter, nitrogen, Fraser Lowland, land clearing, air photo interpretation, parent material

scholarly journals COMPARISON BETWEEN ORGANIC MATTER CONTENT OF MAIN SOIL ORDERS IN KURDISTAN REGION USING TWO DIFFERENT METHODS.

2020 ◽  
Vol 51 (Special) ◽  
Author(s):  
Khoshnaw & Esmail
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Linear Equation ◽  
Organic Matter Content ◽  
Combustion Method ◽  
Matter Content ◽  
Soil Samples ◽  
Kurdistan Region ◽  
Loss On Ignition ◽  
Dry Combustion

This study was conducted to compare between two methods of soil organic matter determination for main soil orders in Kurdistan region/Iraq, for this purpose forty-five soil samples were taken then the organic matter was determined using chemical (Walkley-Black (wet) method and loss-on-ignition method (dry) combustion method. The results indicated the significant correlation (r = 0.88**) between the studied methods It means there is good adjustment to convert organic matter by loss-on-ignition method (dry) to Walkley-Black (wet) method organic matter by this linear equation (organic matter by loss-on-ignition =1.651* Walkley-Black method organic matter +2.1877) this equation can be used to convert organic matter by two methods for Mollisols(M), Vertisols(V) and Aridisols(A) in Hawler(H), Sulaimani(S) and Duhok(D) governorates, this equation is very important and economic to determine and convert dry method to wet method, the amount of organic matter for M, V, A was recorded the highest value (49.5, 24.8, 20 gkg-1) respectively for Mollisols, Vertisols, and Aridisols at Hawler (H), Sulaimani (S), and Duhok(D) respectively for (DM5, SV4, DA1) in Duhok Mollisols, Sulaimani Vertisols and Duhok Aridisol respectively for walk- black (wet) method, the highest value for dry method organic matter in Mollisols, Vertisols, Aridisols was recorded (97.6, 77.9, 50.3 g kg-1) for soil orders (MD3, VD4, AD4) respectively.

Soil mineral structural water loss during loss on ignition analyses

2009 ◽  
Vol 89 (5) ◽  
pp. 603-610 ◽  
Author(s):  
H Sun ◽  
M Nelson ◽  
F Chen ◽  
J Husch
Keyword(s):  
Organic Matter ◽  
Soil Sample ◽  
Water Loss ◽  
Mineral Water ◽  
Surface Soil ◽  
Soil Samples ◽  
Loss On Ignition ◽  
Soil Mineral ◽  
Structural Water ◽  
X Ray

Water loss from soil minerals has been known to cause errors in the determination of soil organic matter when the loss on ignition (LOI) method is used. Unfortunately, no known published studies reliably quantify the range of structural water in the soil. To do this, 15 common reference minerals were analyzed by LOI to obtain their individual water loss. In addition, 14 upland, loamy soil samples and 3 wetland/hydric soil samples with varied mineral contents were analyzed to collect their X-ray powder diffraction spectra. Based upon X-ray spectra peak intensities, the modal abundance of minerals in each soil sample was determined using the RockJock computer program. The resultant modal weight percentages of all identified minerals in each soil sample were then multiplied by the LOI value for each mineral to obtain the mineral structural water loss (SWL) of that soil sample. For the 17 soil samples analyzed, the range of mineral water loss is 0.56 to 2.45%. Depending on the LOI values of the soil samples, the SWL:LOI ratios range from 0.04 to around 1.00. The SWL:LOI ratios are particularly low for top wetland soil when the LOI value is higher. The ratios are lower for surface soil samples than for subsurface soil samples because of the high LOI values in surface soil samples. Understanding soil mineral water loss and its relation to the LOI patterns from various environments is important for the accurate evaluation of soil organic matter when the LOI method is used. Key words: Mineral, structural water, loss on ignition

scholarly journals Soil property variability in a humid natural Mediterranean environment: La Rioja, Spain .

2014 ◽  
Vol 2 ◽  
Author(s):  
José Navarro Pedreño ◽  
Ignacio Gómez Lucas ◽  
Ignacio Meléndez-Pastor
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Soil Property ◽  
Vegetation Type ◽  
Global Climate ◽  
Quantitative Information ◽  
Parent Material ◽  
Mediterranean Environment ◽  
Parent Materials ◽  
La Rioja

Estimating the spatial variability of soil properties is significant for evaluating environmental impacts. For example, many soil properties are directly used in the modelling of environmental processes such as global climate change. These aspects have not previously been studied at this level in La Rioja (a region of Spain with a humid Mediterranean environment). The intention of this study was to provide quantitative information on soil assessment and mapping methods for natural soils in a humid Mediterranean environment. The properties considered included: pH and organic matter, calcium carbonate and clay contents. For testing, samples were selected from several different soil types which, in theory, were only affected by pedogenetic processes and had developed on different parent materials. More than half of the samples did not contain any CaCO<sub>3</sub>, while the rest of the samples presented a variety of CaCO<sub>3</sub>, forms, with high percentages being present in certain cases (up to 65% on the surface). It was possible to establish two different areas: one predominantly acidic and the other principally basic. The predominately basic samples were due to the high percentage of carbonate in the parent materials. The clay content on the surface was similar to that in the subsurface layers. Finally, the organic matter contents in the uppermost layers presented average values of 3.9%,with a range of from 0.3 to 17.5%. The major variations in soils were determined by soil type (therefore by soil forming processes), parent material composition, and vegetation type. This study reveals that these methods are useful to determine the spatial distribution of some soil properties in undisturbed soils. The contour maps of soil property variability could be used to improve future sampling designs and management decisions.

scholarly journals Soil property variability in a humid natural Mediterranean environment: La Rioja, Spain .

2014 ◽  
Vol 2 ◽  
Author(s):  
Raimundo Jiménez-Ballesta ◽  
Marisol S. Andrades ◽  
Álvaro Marín ◽  
Victoria Íñigo ◽  
Juan I. Alonso-Martirena
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Soil Property ◽  
Vegetation Type ◽  
Global Climate ◽  
Quantitative Information ◽  
Parent Material ◽  
Mediterranean Environment ◽  
Parent Materials ◽  
La Rioja

Estimating the spatial variability of soil properties is significant for evaluating environmental impacts. For example, many soil properties are directly used in the modelling of environmental processes such as global climate change. These aspects have not previously been studied at this level in La Rioja (a region of Spain with a humid Mediterranean environment). The intention of this study was to provide quantitative information on soil assessment and mapping methods for natural soils in a humid Mediterranean environment. The properties considered included: pH and organic matter, calcium carbonate and clay contents. For testing, samples were selected from several different soil types which, in theory, were only affected by pedogenetic processes and had developed on different parent materials. More than half of the samples did not contain any CaCO<sub>3</sub>, while the rest of the samples presented a variety of CaCO<sub>3</sub>, forms, with high percentages being present in certain cases (up to 65% on the surface). It was possible to establish two different areas: one predominantly acidic and the other principally basic. The predominately basic samples were due to the high percentage of carbonate in the parent materials. The clay content on the surface was similar to that in the subsurface layers. Finally, the organic matter contents in the uppermost layers presented average values of 3.9%,with a range of from 0.3 to 17.5%. The major variations in soils were determined by soil type (therefore by soil forming processes), parent material composition, and vegetation type. This study reveals that these methods are useful to determine the spatial distribution of some soil properties in undisturbed soils. The contour maps of soil property variability could be used to improve future sampling designs and management decisions.

Organic carbon, organic matter and bulk density relationships in boreal forest soils

2008 ◽  
Vol 88 (3) ◽  
pp. 315-325 ◽  
Author(s):  
Catherine Périé ◽  
Rock Ouimet
Keyword(s):  
Organic Matter ◽  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Bulk Density ◽  
Forest Soils ◽  
Sandy Loam ◽  
Measurement Techniques ◽  
Complete Recovery ◽  
Soil Bulk Density ◽  
Dry Combustion

Relationships between soil organic carbon (SOC), organic matter (SOM), and bulk density (BD) were established in acidic loamy to sandy loam fine fractions of forest soils in Quebec (Canada). The interest of such relationships rests with the possibility of using simple and rapid techniques to estimate SOC and BD. It is also a crucial step in establishing the correspondence among several databases when SOC data are obtained using different measurement techniques. In this study, SOC was measuredby dry combustion (SOCNDC) and wet digestion (SOCWD) methods, and organic matter by loss-on-ignition (LOI). Our results suggest that, in these soils: (1) LOI can be used for estimating SOC (r2 = 0.95, RMSEP = 16%) and SOCDC/SOM significantly decreased with increasing depth from 0.49 to 0.27; (2) SOCDC and SOCWD were highly correlated. Even if SOCWD provided near complete recovery of SOCDC, dry combustion remains the preferred method for SOC analysis since recovery decreased with increasing depth from 100 to 83%. (3) BD was also strongly related to SOM(r2 = 0.81). We recommend using the organic density approach to estimate BD from SOM because it allows BD to be predicted without significant bias and with a degree of accuracy of 14%. Key words: Forest soils, soil organic carbon, soil organic matter, soil bulk density

Correction for particulate organic matter as estimated by loss on ignition in estuarine ecosystems

2003 ◽  
Vol 58 (1) ◽  
pp. 147-153 ◽  
Author(s):  
Anne-Laure Barillé-Boyer ◽  
Laurent Barillé ◽  
Henri Massé ◽  
Daniel Razet ◽  
Maurice Héral
Keyword(s):  
Organic Matter ◽  
Particulate Organic Matter ◽  
Loss On Ignition ◽  
Estuarine Ecosystems

Particle densities of wetland soils in northern Alberta, Canada

2006 ◽  
Vol 86 (1) ◽  
pp. 57-60 ◽  
Author(s):  
T. E. Redding ◽  
K. J. Devito
Keyword(s):  
Organic Matter ◽  
Particle Density ◽  
Physical Property ◽  
Organic Soils ◽  
Wetland Soil ◽  
Loss On Ignition ◽  
Simple Method ◽  
Mean Values ◽  
Northern Alberta ◽  
Wetland Types

Particle density is a fundamental soil physical property, yet values of soil and organic matter particle density (ρs and ρo) vary widely in the literature. We measured particle density of organic soils from five wetland types, and from exposed sediments of drying ponds, in northern Alberta, Canada. Our measured values of organic soil and pond sediment ρs varied widely (1.43–2.39 Mg m-3); however, calculated values of ρo (1.34–1.52 Mg m-3) were relatively constant. The measured and calculated ρs and ρo values were similar to those obtained in published studies using similar methods, but were higher than the values provided in many reference texts. Given the relatively small variability in ρo, the use of mean values of ρo, combined with measurements of organic matter loss-on-ignition, shows promise as a simple method for obtaining reliable estimates of ρs across a range of wetland types. Key words: Particle density, peat, organic matter, wetland soil, loss-on-ignition

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