CLASSIFICATION OF SOILS DEVELOPED ON BASIC PARENT MATERIALS IN THE CANADIAN AND FRENCH SYSTEMS OF SOIL CLASSIFICATION

1986 ◽  
Vol 66 (1) ◽  
pp. 177-181 ◽  
Author(s):  
C. R. DE KIMPE ◽  
J. DEJOU
Keyword(s):  
Organic Matter ◽  
Key Words ◽  
Bulk Density ◽  
Amorphous Material ◽  
Soil Classification ◽  
Parent Materials

Six profiles of soils developed on parent materials poor in SiO2 but rich in total Fe (> 10% Fe2O3), were sampled in Canada and France. In the French system of soil classification, the soils were classified as Andosols or Andic and Andic Brown soils because of their large amounts of < 50 μm particles and amorphous material, and their low bulk density related to large percentages of organic matter. All profiles contained one or more horizons that met the criteria of a Podzolic B horizon in the Canadian system of soil classification. The absence of a class for Andosols makes an appropriate classification of these soils difficult in the Canadian system. Key words: Andosols, Andic soils, Andic brown soils, podzols, soil classification

scholarly journals Soils with vertic properties in Kamennaya Steppe

2013 ◽  
pp. 3-25 ◽  
Author(s):  
N. B. Khitrov ◽  
Yu. I. Cheverdin ◽  
N. P. Chizhikova ◽  
L. V. Rogovneva
Keyword(s):  
Soil Classification ◽  
Humus Formation ◽  
Calcium Carbonates ◽  
Parent Materials ◽  
Kamennaya Steppe ◽  
Relief Elements ◽  
Heavy Loam ◽  
Voronezh Region ◽  
Carbonate Leaching

The most spread are soils with vertic properties at the territory of Kamennaya Steppe (Voronezh region, Talovsky district) being confined to four landscape positions within 11 different soil combinations derived from clayey or two-layered heavy loam-clayey parent materials. These soils have developed: (A) on bottoms of deep and closed depressions covered by spotted soil combinations in flat watersheds; (B) on some depression bottoms in spotted combinations without solonetzic soils; (C) in different relief elements occupied by chernozemic hydromorphic solonetz complexes and (D) in concave (in long and cross directions) relief elements in the topolithomosaic composition confined to exposed re-deposition products of Dnieper moraine on the slope of Talovaya narrow. Occupying only 0.2% from the total area of agro-forest landscapes, the vertic soils can account for 0.7% to 15% within a separate soil combination and reveal a great diversity. The latter is associated with vertic properties developed together with features of gleying and quasi-gleying, accumulation of calcium carbonates and, on the contrary, clay illuviation against the background of calcium carbonate leaching, solonetz process, salinization, humus formation and the topsoil eluviations. Such a diversity may be adequately reflected both in the soil classification of Russia and in WRB.

scholarly journals COMPARATIVE ASSESSMENT OF SOME PHYSICAL PROPERTIES AND ORGANIC MATTER CONTENT OF SOILS DERIVED FROM DIFFERENT PARENT MATERIALS IN AKWA IBOM STATE, NIGERIA

2019 ◽  
Vol 18 (1) ◽  
pp. 107-125
Author(s):  
P. C. OGUIKE ◽  
U. E. UTIN
Keyword(s):  
Organic Matter ◽  
Bulk Density ◽  
Crop Production ◽  
Alluvial Soil ◽  
Organic Matter Content ◽  
Field Capacity ◽  
Matter Content ◽  
Comparative Assessment ◽  
Parent Materials ◽  
Cumulative Infiltration

The study of soils derived from different parent materials is useful in formulating appropriate management schemes for soil health and agricultural production. A comparative assessment of some physical properties and organic matter content of soils formed from coastal plain sands (CPS), sandstone (SST) and river alluvium (ALV) was conducted in Akwa Ibom State, Nigeria. Topsoil samples (0 – 30 cm) were collected from ten points in soils of each of the three parent materials for laboratory analyses. The soil samples were analyzed for texture, macro and micro aggregate stability indices, soil water characteristics, bulk density and organic matter. Data generated were subjected to Analysis of Variance to compare properties of soils of the different parent materials. Significantly different means were separated using the Least Significant Difference at 5% probability level. Results showed that soils of SST and CPS parent materials both had loamy sand texture while that of ALV soil was clay. Bulk density of ALV soil (1.20 Mg m-3) was significantly lower (p≤0.05) than those of CPS (1.55 Mg m-3) and SST (1.39 Mg m-3).  Significantly higher (p≤0.05) mean weight diameter (MWD) (2.01 mm), aggregated silt+clay (51.96%) and clay flocculation index (89.00%) were observed in ALV soils than in CPS and SST soils while the dispersion ratio and clay dispersion index were significantly higher (p≤0.05) in CPS and SST soils than in the ALV soil. Alluvial soil had significantly higher (p≤0.05) saturation water content (SWC), field capacity (FC), permanent wilting point (PWP) and available water content (AWC) of 0.61, 0.45, 0.25 and 0.20 m3 m-3, respectively, than those of CPS and SST. Alluvial soil also had the lowest cumulative infiltration (3.05 cm) and saturated hydraulic conductivity (0.40 cm hr-1) relative to those of CPS and SST. The CPS soil had significantly lower (p≤0.05) organic matter content (2.07%) than SST (3.06%) and ALV (3.34%) soils. Cumulative infiltration (I) significantly and positively correlated with total sand (TS) (r = 0.710*) in the CPS soil, and Ksat (r = 0.681*), MWD (r = 0.829**) and CFI (r = 0.655*) in the SST soil. In the ALV soil, cumulative infiltration positively correlated with total porosity (r = 0.770**) and negatively with bulk density (r = - 0.770**). Saturated hydraulic conductivity (Ksat) had a positive correlation with SWC (r = 0.745*) and TP (r = 0.833**), but a significant and negative correlation with BD (r = - 0.833**) in SST soil. Field capacity (FC) positively and significantly correlated with TP (r = 0.638*) in CPS soil, and with MWD (r = 0.713*), CFI (r = 0.647*) and OM (r = 0.651*) in SST soil and with TP (r = 0.790**) and OM (r = 0.672*) in ALV soil. The correlations of FC with BD (r = - 0.638*) in CPS soil, with CDI (r = -0.647*) in SST soil and with BD (r = -0.790**) in ALV soil were significant and negative. MWD positively and significantly correlated with organic matter (r = 0.699*).  The clayey ALV soil will be suitable for paddy rice production and dry season crops due to its higher water retention capacity than the CPS and SST soils which will be better utilized for vegetable crop production under irrigation. The CPS and SST soils can also be applied to intensive crop production under rain fed condition and supplemented with irrigation.  

CHEMICAL PROPERTIES AND CLASSIFICATION OF ORGANIC HORIZONS FROM SELECTED SOILS IN BRITISH COLUMBIA

1987 ◽  
Vol 67 (2) ◽  
pp. 383-394 ◽  
Author(s):  
L. E. LOWE ◽  
A. M. SCAGEL ◽  
K. KLINKA
Keyword(s):  
British Columbia ◽  
Correlation Analysis ◽  
Key Words ◽  
Chemical Properties ◽  
Morphological Characteristics ◽  
Soil Classification ◽  
Canonical Variates Analysis ◽  
Organic Horizons ◽  
Canonical Variates

In order to assess the extent to which chemical properties of organic horizons support their differentiation on the basis of morphological characteristics, as used in the Canadian System of Soil Classification (CSSC), a total of 265 samples of organic horizons (including L, F, H, Of, Om and Oh) were analyzed for 26 chemical properties (organic and inorganic). One-way analysis of variance, correlation analysis and tests of normality were used to select variables for canonical variates analysis (CVA). The results of CVA indicated that the six types of horizon could be distinguished by a combination of chemical properties, and that the grouped upland (L-F-H) horizons could be distinguished from the grouped wetland (Of-Om-Oh) horizons. The results provided support for the present usage in the CSSC, based on field morphology. It was concluded that there remained a need to improve definitions, to review designations, and to develop quantitative diagnostic criteria for organic horizons. Some problems in the classification of organic horizons are discussed, particularly in relation to a hierarchical system. Key words: Organic horizons, horizon classification, British Columbia, chemical properties

THE ORIGIN OF BANDS IN SANDY SOILS OF THE STONY PLAIN AREA

1966 ◽  
Vol 46 (3) ◽  
pp. 245-254 ◽  
Author(s):  
G. M. Coen ◽  
S. Pawluk ◽  
W. Odynsky
Keyword(s):  
Organic Matter ◽  
Sandy Soils ◽  
Total Thickness ◽  
Free Iron ◽  
Parent Materials ◽  
Plain Area ◽  
Mineralogical Characteristics ◽  
Bt Horizon

The presence of bands in the lower sola has presented difficulties in the classification of soils developed from pitted deltaic sandy parent materials west of Edmonton, Alberta. The bands were shown to contain more organic matter, free iron, and clay than the interbands, which resulted in a darker, redder color and finer texture as observed in the field. The bands were often coincidental with stratified layers, but their occasional transgression across geologic stratification and their development in profiles without stratification suggested a pedogenic origin. Micropedological investigations revealed oriented clay around the sand grains in the bands and not the interbands, further indicating that the increase in clay was due, at least in part, to illuviation.The bands in the soils investigated have sufficient total thickness of clay accumulation to meet the requirements for a Bt horizon and together with their chemical, physical, and mineralogical characteristics permit their inclusion in the Eluviated Dark Grey Subgroup of the Chernozemic Order and the Orthic Dark Grey Wooded Subgroup of the Podzolic Order.

RELATIONS ENTRE LA TENEUR EN MATIÈRE ORGANIQUE ET LA MASSE VOLUMIQUE APPARENTE DU SOL

1986 ◽  
Vol 66 (4) ◽  
pp. 743-746 ◽  
Author(s):  
D. A. ANGERS ◽  
R. R. SIMARD
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Key Words ◽  
Bulk Density ◽  
Soil Compaction ◽  
Organic Matter Content ◽  
Soil Bulk Density ◽  
Matter Content ◽  
Soil Organic Matter Content ◽  
Masse Volumique

As a part of a study on soil compaction, measurements of soil bulk density were taken three times during the season at five sites and three depths. Strong negative correlations were obtained between soil organic matter content and (1) soil bulk density and, (2) the increase in bulk density during the season. Key words: Bulk density, compaction, organic matter

DISSOLUTION DES COMPOSÉS FERRUGINEUX ET ALUMINEUX DES HORIZONS B PODZOLIQUES DE SOLS DU QUÉBEC PAR LE DITHIONITE-CITRATE-BICARBONATE, L'OXALATE, LE PYROPHOSPHATE ET LE TÉTRABORATE

1989 ◽  
Vol 69 (3) ◽  
pp. 451-459 ◽  
Author(s):  
F. PAGÉ ◽  
C. R. DE KIMPE
Keyword(s):  
Organic Matter ◽  
Key Words ◽  
Acid Content ◽  
Inorganic Compounds ◽  
Soil Classification ◽  
Classification Criteria ◽  
Organic C ◽  
Inorganic Oxides ◽  
Iron Aluminum ◽  
Total Organic C

Organic matter, Fe and Al were determined in dithionite-citrate-bicarbonate (d), oxalate (o), pyrophosphate (p) and tetraborate (t) extracts from Quebec Podzolic B horizons in order to evaluate the ability of these reagents to extract the organo-metallic complexes as well as inorganic oxides and hydroxides, and to verify the appropriateness of soil classification criteria. Dithionite solubilized most of the Fe whereas oxalate extracted most of the Al compounds; the ability of the same reagents to extract Al and Fe, respectively, was directly related to the amount of organo-metallic complexes. Pyrophosphate extracted not only complexes but also inorganic compounds while tetraborate extracted mainly complexes. Organic matter extraction by dithionite, oxalate and tetraborate was enhanced by a high fulvic acid content; it was highest in the Bh and lowest in the Bf horizons. Organic matter, Fe and Al extraction by tetraborate was reduced in the presence of a large Fe-inorganic compounds content. These results indicated that extracting ability of the reagents depends on the nature of the B horizons, except for Fe extraction by dithionite and Al extraction by oxalate. Consequently, Fe and Al extraction by pyrophosphate or tetraborate is not appropriate for classification purposes. Differentiation of Bh horizons from other Podzolic B horizons was possible by using the total organic C to Fed + Alo ratio, because the ratio was > 3 for Bh horizons and < 3 for Bf and Bhf horizons. Key words: Organic matter, iron, aluminum, Podzolic B horizons, extraction reagents

scholarly journals PEDOGENESIS AND SOIL CLASSIFICATION OF AN EXPERIMENTAL FARM IN MOSSORÓ, STATE OF RIO GRANDE DO NORTE, BRAZIL

2016 ◽  
Vol 29 (4) ◽  
pp. 1036-1042 ◽  
Author(s):  
LUNARA GLEIKA DA SILVA RÊGO ◽  
CAROLINA MALALA MARTINS ◽  
EULENE FRANCISCO DA SILVA ◽  
JÉSSIA JULIANA ALVES DA SILVA ◽  
REBECA NAIRONY DA SILVA LIMA
Keyword(s):  
Rio Grande ◽  
Soil Classification ◽  
Soil Types ◽  
Soil Profiles ◽  
Mineralogical Analysis ◽  
Parent Materials ◽  
Physical Chemical ◽  
Determining Factors ◽  
Pedogenic Processes

ABSTRACT The Rafael Fernandes experimental farm is located in the Alagoinha district, northwest of Mossoró, State of Rio Grande do Norte, Brazil, over two pedogenic formations of different edaphic characteristics, thus needing a more detailed description of its soil types, since this area hosts several experimental fields for researches on agriculture. The objective of this work was to characterize the morphological, physical, chemical and mineralogical features of the most representative soils of this farm, in order to understand its pedogenesis and define its classifications. The whole area was surveyed in order to assess its more representative pedogenic formations. Three soil profiles were classified and described, from which samples were collected in all horizons for physical, chemical and mineralogical analysis. The parent materials and the relief were the determining factors for pedogenic processes of desilication, podzolization and laterization, generating the three main soil types of the area, which were classified up to the 4th categorical level and described as: Typic Rhodustults (P1), Rhodic Haplustox (P2) and Typic Plinthustalfs (P3).

Micromorphological evidence of pedogenetic pathway of a Podzolic Gray Luvisol (Falmouth series) in Nova Scotia

1995 ◽  
Vol 75 (4) ◽  
pp. 491-496 ◽  
Author(s):  
C. Wang ◽  
G. R. Brewster ◽  
K. T. Webb
Keyword(s):  
Organic Matter ◽  
Nova Scotia ◽  
Key Words ◽  
Thin Sections ◽  
Parent Materials ◽  
Acidic Nature ◽  
Gray Luvisol ◽  
Bt Horizon

A catena of Podzolic Gray Luvisols (Falmouth series) – Gleyed Gray Luvisols (Queens series) – Orthic Gleysols (Kingsville series) is commonly found on fine loamy, weakly calcareous parent materials in Nova Scotia, with Podzolic Gray Luvisols occupying the best drained landscape positions. The hypothesis that podzolic B horizons of Podzolic Gray Luvisols were developed on degraded Bt horizons was investigated by micromorphological characterization of one Podzolic Gray Luvisol pedon. Although not visible in field examinations, argillans were common in thin sections of the Bf and Bm horizons. These argillans were not associated with the walls of voids or the surface of grains. Argillans of the Bt horizons, however, were associated with features such as cracks, vughs, and channels. The upper Bt horizon (i.e., Bt1gj) showed signs of degradation. The pale brown matrix color was more like the Bm horizon above than the dark brown Bt2gj horizon below. The strongly acidic nature of the Bt1gj horizon may have triggered degradation. It is concluded that the Bf and Bm horizons were developed on degraded Bt horizons through the translocation of amorphous Fe and Al and organic matter. Key words: Pedogenesis, micromorphology, Luvisols, bisequal soils

CHEMICAL AND PHYSICAL PROPERTIES OF SOME SOILS DERIVED FROM REDDISH BROWN MATERIALS IN THE ATLANTIC PROVINCES

1969 ◽  
Vol 49 (1) ◽  
pp. 65-78 ◽  
Author(s):  
J. A. McKeague ◽  
D. B. Cann
Keyword(s):  
Particle Size ◽  
Organic Matter ◽  
Nova Scotia ◽  
Physical Properties ◽  
New Brunswick ◽  
Bulk Density ◽  
Parent Materials ◽  
High Bulk ◽  
Obvious Feature ◽  
Bt Horizon

Nearly all of the 16 soils from Nova Scotia and New Brunswick that were studied had Ae horizons, acid sola and dense, reddish brown parent materials, but they differed widely in the kind and the degree of B horizon development. Particle-size analyses supported the micromorphological observations in indicating that marked illuviation of clay had occurred in some soils, and weak illuviation in others. In a few soils it was difficult to estimate the extent of Bt horizon development as there were obvious discontinuities in the materials. Horizons having the chemical requirements of Podzol B horizons (Bf), significant accumulations of amorphous Al and Fe associated with organic matter, were found in only three of the soils. None of the soils had a Bft horizon; hence, the subgroup, Textural Podzol, should be eliminated. Bisequa development was evident in several of the soils and one was a Bisequa Podzol. Prominently mottled Bg horizons were the most obvious feature of the Gleysolic soils and some of them had Btg horizons. The bulk density of the fragipan in one of the soils was about 2.0, and many of the parent materials had equally high bulk densities. Free carbonates occurred at depths ranging from 60 to 180 cm in 12 of the 16 soils studied.

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