COMPARATIVE STUDY OF FOUR TILLS IN WEST-CENTRAL ALBERTA

1974 ◽  
Vol 54 (1) ◽  
pp. 69-80
Author(s):  
A. G. TWARDY ◽  
S. PAWLUK ◽  
J. D. LINDSAY
Keyword(s):  
Clay Fraction ◽  
Coarse Sand ◽  
Parent Material ◽  
The Other ◽  
High Grade ◽  
Soil Series ◽  
Physical Chemical ◽  
West Central ◽  
Two Samples ◽  
Range Test

Twenty-two samples of till representing Ck horizons of soils with very similar morphologies were investigated in west-central Alberta in order to determine the validity for their separation into four separate soil series on the basis of parent material characteristics. Physical, chemical and mineralogical analyses were conducted in order to characterize the tills and determine differences in their lithology, texture and geochemistry. The data were statistically evaluated using Duncan's new multiple range test. The data indicate that the four tills investigated are statistically separable on the basis of their analytical differences. The Lobley till is characterized by a higher limestone content and higher calcium carbonate equivalent than the other three tills. Amphibole minerals and high grade metamorphic and igneous pebbles were absent in the Lobley till. A greater quantity of total sand, coarse sand and amphiboles permits the separation of the Cooking Lake till from the other three tills. The Hubalta and Breton tills were found to be somewhat similar in many of their characteristics. However, the Breton till is coarser in texture and contains a greater montmorillonitic component in the clay fraction.

INFLUENCE OF PARENT MATERIAL AND MOISTURE REGIME ON SOIL GENESIS IN THE APPALACHIAN HIGHLANDS, QUEBEC

1976 ◽  
Vol 56 (3) ◽  
pp. 271-283 ◽  
Author(s):  
C. R. DE KIMPE
Keyword(s):  
Clay Fraction ◽  
Parent Material ◽  
Glacial Till ◽  
Soil Reaction ◽  
Moisture Regime ◽  
Material Base ◽  
Soil Series ◽  
Mineralogical Analysis ◽  
The North ◽  
Aluminous Cement

Ten pedons representing the Saint Onésime, Manie, Mont Carmel and Ixworth soil series were studied to respectively characterize the well to very poorly drained members of a toposequence formed on glacial till deposits along the north flank of the Appalachian Highlands. The parent material was generally homogeneous in the occurrence area except in the western part where glacial lakes along the Chaudière Valley controlled the deposition of a coarser till material. Soil reaction was extremely acid in the solum and pH reached approximately 6.0 in the parent material. Base saturation was low, which was related to the large amounts of aluminum hydroxypolymers present in the clay fraction. Mineralogical analysis of the clay fraction indicated an extensive transformation of illite not only to the swelling minerals, vermiculite and montmorillonite, but also to kaolinite. Chlorite was absent in the A horizons of the well drained profiles. The soils were underlain by fragic horizons. This fragipan had a moderately developed gray streak network, as these soils are not very prone to alternate humidification and desiccation cycles. Cohesion and brittleness were related to the illitic clay bridges and to an amorphous aluminous cement. The content of kaolinite in the Ae horizon of the well drained profiles and the presence of large amounts of Al hydroxypolymers in the clay fraction corresponded to more intense weathering conditions than those existing in the soils of the south flank of the Appalachian Mountains.

scholarly journals Soil-landscape relationship in sandstone-gneiss topolithosequence in Amazonas, Brazil

2019 ◽  
Author(s):  
Julimar da Silva Fonseca ◽  
Milton César Costa Campos ◽  
Elilson Gomes de Brito Filho ◽  
Bruno Campos Mantovanelli ◽  
Laércio Santos Silva ◽  
...  
Keyword(s):  
Three Dimensional ◽  
Clay Fraction ◽  
Parent Material ◽  
Sand Fraction ◽  
Physical Chemical ◽  
Soil Landscape ◽  
History Of ◽  
Geomorphic Surfaces ◽  
Upper Third ◽  
History Of Formation

Abstract. Soil position in the landscape reveals its history of formation and genesis. Therefore, the landscape is the combination of features of the surface of the earth with subsurface components (parent material), while the soil is a three-dimensional, dynamic natural body inserted in the landscape. This research aimed to study the soil-landscape relationship in a sandstone-gneiss topolithosequence in Amazonas, Brazil. The study was carried out along a 9.253-meter transect from the top downwards the softer slope. Soil profiles were selected in five landscape compartments (top, upper third, lower third, transport foothill, and deposition foothill). Morphological, mineralogical, physical, chemical, and ray diffraction characterizations were performed. Soils had different morphological, physical, chemical, and mineralogical attributes due to the variations of the geological substrate and landscape position. The mineralogy of the clay fraction is composed of kaolinite, goethite, hematite, and gibbsite, with goethite being the predominant iron oxide. A sand fraction dominance was observed in relation to the other fractions in all the profiles, being related to the alluvial nature of the parent material, with the highest values occurring in the lower third. The separation of the landscape into geomorphic surfaces and identification of the parent material were effective for understanding the variation of soil attributes along the landscape.

CARACTERISTIQUES MINERALOGIQUES ET CHIMIQUES DE QUELQUES SOLS SABLEUX DU QUEBEC EN REGARD DE LEUR EVOLUTION PEDOLOGIQUE

1981 ◽  
Vol 61 (2) ◽  
pp. 273-283 ◽  
Author(s):  
M. R. LAVERDIERE ◽  
C. R. DE KIMPE ◽  
A. D’AVIGNON
Keyword(s):  
Organic Matter ◽  
Sandy Soil ◽  
Cation Exchange Capacity ◽  
Clay Fraction ◽  
Sandy Soils ◽  
Exchange Capacity ◽  
Parent Material ◽  
Regression Equations ◽  
Soil Series ◽  
Podzolic Soils

A, B and C horizons of 13 sandy soil series were sampled in the lowlands of southern Quebec. From the amounts of pyrophosphate-extractable Fe and Al and clay contents, nine of these profiles were classified as Podzolic soils while the others were Brunisols. Formation of montmorillonite and dissolution of chlorite in Ae horizons indicate intense weathering of the minerals at this level. In the B horizons, vermiculite that was present in the parent material or resulted from the alteration of illite was often chloritized. Values of pH measured in 1 M NaF were generally higher than 10.2 for the B horizons. The amounts of phosphorus retained by the samples varied in the following ranges: 23–397 μg P/g of soil for A horizons, 301–1578 μg P/g of soil for B horizons and 71–296 μg P/g of soil for C horizons. Cation exchange capacity of the soils was lower than 10 meq/100 g of soil, except in those horizons that contained high amounts of organic matter and where values up to 27.6 meq/100 g were measured. Using regression equations, values were obtained for the CEC of the organic matter and the clay fraction of these sandy soils.

ETUDE COMPARATIVE DE SOLS DES LAURENTIDES, QUEBEC

1975 ◽  
Vol 55 (3) ◽  
pp. 363-379 ◽  
Author(s):  
B. MUTWEWINGABO ◽  
C. R. DE KIMPE ◽  
G. A. BOURBEAU ◽  
R. W. BARIL ◽  
P. LAJOIE
Keyword(s):  
Particle Size ◽  
Clay Fraction ◽  
Parent Material ◽  
The Other ◽  
Quebec City ◽  
X Ray Diffraction ◽  
X Ray ◽  
High Bulk Density ◽  
Diffraction Patterns ◽  
High Bulk

Five profiles were sampled in the till deposits of the Laurentides Hills. Two were obtained at Duchesnay, near Quebec City and three north of Montreal, including two profiles of the Gatineau and one of the Sainte-Agathe series of soils. Results of the particle-size distribution, morphological and mineralogical analyses suggested that the parent material was similar in all profiles. A high bulk density, about 2.00 g/cm3, was observed in the fragic horizon. Maximum weathering was found in the A horizons resulting in the formation of montmorillonite and kaolinite. The X-ray diffraction patterns obtained for the samples from Duchesnay were better defined than those obtained from the other profiles. In addition to illite, chlorite and vermiculite, two types of interstratified minerals were observed: illite–montmorillonite in the Podzolic-B and illite–vermiculite in the fragic horizons. High values, up to about 700 meq/100 g were obtained for the Al interlayers in the clay fraction. These profiles were classified as fragic ferro-humic Podzols (Sainte-Agathe and the profiles from Duchesnay) and fragic humo-ferric Podzols (Gatineau). The concept of fragic horizon in the soils from the Laurentides is discussed.

scholarly journals MECHANICAL COMPOSITION OF THE SOILS FORMED ON LIMESTONES AND DOLOMITES IN THE REPUBLIC OF MACEDONIA

2017 ◽  
Vol 36 (1) ◽  
Author(s):  
Mile Markoski ◽  
Tatjana Mitkova ◽  
Kole Vasilevski ◽  
Zorica Tomić ◽  
Marjan Andreevski ◽  
...  
Keyword(s):  
Clay Fraction ◽  
Fine Sand ◽  
Coarse Sand ◽  
Parent Material ◽  
Sand Fraction ◽  
Terra Rossa ◽  
Physical Clay ◽  
Average Value ◽  
Fine Soil ◽  
The Republic

The paper presents results from the research of the influence of the parent material on the mechanical compo-sition of calcomelanosols, calcocambisols and terra rossa. The contents of the fine soil separates in the calcomelano-sols vary depending on the subtype. The physical sand fraction (coarse sand + fine sand) in the Amo horizon amounts 44.81% in the organomineral calcomelanosols, 40.13% in the organogenic and brownised calcomelanosols 36.52%. In the (B)rz horizon in the brownised calcomelanosols it amounts 32.64%. The content of clay + silt or physical clay in the Amo horizon amounts 55.19% in the organomineral calcomelanosols, 59.87% in the organogenic and the high-est content is in the brownised calcomelanosols 63.48%. The average value of this fraction in the horizon (B)rz in the brownised calcomelanosols amounts 67.36%. In the calcocambisols the average content of the fraction physical sand in the Amo horizon amounts 33.43%, and in the cambic horizon (B)rz 22.50%. In the terra rossa the fraction physical clay is represented with a greater percentage related to the physical sand fraction. In the Amo horizon, in the physical clay fraction, the clay fraction is predominant, average 43.08%, and 52.13% in the cambic horizon, and 24.90% in the Amo horizon and 19.37% in the (B)rz horizon for the silt fraction. From a research soils 36% of the soils are formed on massive limestone, 13% are formed on dolomitic limestone and bituminous marbles, 16% on plate (flat) limestone, 10% on dolomitic marbles and 12% on laminated (plate) dolomite and calcite.

Comparative influence of soil and management on barley yield in the Vale of Whitehorse, England

1987 ◽  
Vol 108 (3) ◽  
pp. 555-560 ◽  
Author(s):  
A. O. Ogunkunle ◽  
P. H. T. Beckett
Keyword(s):  
Soil Properties ◽  
Cumulative Effect ◽  
Soil Classification ◽  
Coarse Sand ◽  
Barley Grain ◽  
The Other ◽  
Yield Prediction ◽  
Soil Series ◽  
Undisturbed Soil ◽  
O 15

SummaryThe reliability of the soil series as a basis for crop yield prediction was examined by comparing the influence of soil and management (inter-farmer differences) on the variance of barley grain yield. Yields of barley were measured from farmers' fields for 2 years and in undisturbed soil cores for 5 years. Fields on different soil series within farms and on the same soil series across farms were used. Linear stepwise regressions of yield on a number of soil properties were also examined to assess the relative influence of soil and management on the properties that were significant to yield.The results show that generally, soil classification has a strong influence on yield variance, but there is clear evidence that the influence of management, specifically the cumulative effect of P and K fertilizer applications, is considerable. Thus in an undisturbed core, for the first 3 years when N, P, K and Mg were applied, the influence of soil was stronger than that of management, but this was reversed in the 4th year when P and K were not applied. Similarly in the field, the influence of soil was stronger in the 1st year, but this was reversed in the 2nd year, although on different field-farm combinations. In all cases, the influence of neither soil nor management was significantly stronger than the other.The results of the regression studies also confirmed those of yield variance in that in general, neither soil nor management has exclusive control of the yield variance. The soil was significantly stronger than management in the control of only coarse sand content at 0–15 cm out of the four soil properties (including Mg and pH (0–15 cm) and K (15–30 cm)) which were significant to yield in the cores. On the other hand, management was significantly stronger than soil in the control of only available P at O–15 cm out of the three soil properties (including Cu and Mg both at 0–15 cm) that were significant to field yield.It is concluded that for soil classification to be a reliable basis for yield prediction and/or agrotechnology transfer, the effect of management must be emphasized.

Suitability of forms of preparing seeds of Dalbergia miscolobium Benth for exposure to the tetrazolium test / Adequação das formas de preparação de sementes de Dalbergia miscolobium Benth para exposição ao teste de tetrazolium

2017 ◽  
Vol 1 (1) ◽  
Author(s):  
Juliana Martins de Mesquita Matos ◽  
Rosana De Carvalho Cristo Martins ◽  
Valéria Regina Bellotto ◽  
Lilian Gomes da Silva Rocha ◽  
Eloiza Aparecida Barbosa ◽  
...  
Keyword(s):  
Endangered Species ◽  
Filter Paper ◽  
Federal District ◽  
Complete Removal ◽  
Sensu Stricto ◽  
The Other ◽  
Distrito Federal ◽  
Viable Seeds ◽  
Range Test ◽  
Tetrazolium Test

Dalbergia miscolobium or Jacarandá do Cerrado is a species of legume in the Fabaceae family. It occurs in the sensu stricto Cerrado and in the dystrophic cerradão. It shows potential for landscaping and for recovering damaged areas. It is an endangered species and therefore is protected by the law that prevents cut in areas of the Federal District (Decree No. 14.783/93). The purpose of this study was to determine the best procedure to prepare seeds of Dalbergia miscolobium to assess viability in the tetrazolium test. We carried out the following treatments: i) hydration on filter paper at 25 ° C, ii) hydration on filter paper at 25 ° C followed by a cut in the tegument and iii) hydration on filter paper at 25 ° C followed bya complete removal of the tegument. The results were analyzed using analysis of variance and the Tukey range test. The analyzes showed that the best procedure to prepare seeds of Dalbergia miscolobium is the treatment in which there is a hydration followed by the complete removal of the integument. Where 78% of the seeds showed uniform staining, indicating that the seeds analyzed are of good quality. The other treatments, hydration and hydration followed by cutting, showed respectively 35% and 41% of viable seeds. RESUMO A Dalbergia miscolobium ou Jacarandá do Cerrado é uma espécie de leguminosa da família Fabaceae. Ocorre no sentido stricto Cerrado e no cerradão distrófico. Possui potencial para paisagismo e para recuperar áreas degradadas. É uma espécie ameaçada de extinção e, portanto, está protegida pela lei que previne o corte em áreas do Distrito Federal (Decreto 14.783 / 93). O objetivo deste estudo foi determinar o melhor procedimento de prepararação das sementes de Dalbergia miscolobium para serem submetidas à análise de viabilidade pelo teste de tetrazólio. Foram realizados os seguintes tratamentos: i) hidratação em papel de filtro a 25 ° C, ii) hidratação em papel de filtro a 25 ° C seguida de um corte no tegumento e iii) hidratação em papel de filtro a 25 ° C seguido de remoção completa do tegumento. Os resultados foram analisados utilizando-se a análise de variância e o teste de médias de Tukey. As análises mostraram que o melhor procedimento para preparar sementes de Dalbergia miscolobium é o tratamento em que há uma hidratação seguida pela remoção completa do tegumento, onde 78% das sementes apresentaram coloração uniforme, indicando que as sementes analisadas são de boa qualidade. Os demais tratamentos, hidratação e hidratação seguida de corte, mostraram respectivamente 35% e 41% de sementes viáveis.

Polymer-Graphene Nanoassemblies and their Applications in Cancer Theranostics

2020 ◽  
Vol 20 (11) ◽  
pp. 1340-1351 ◽  
Author(s):  
Ponnurengam M. Sivakumar ◽  
Matin Islami ◽  
Ali Zarrabi ◽  
Arezoo Khosravi ◽  
Shohreh Peimanfard
Keyword(s):  
Mechanical Stability ◽  
Chemical Properties ◽  
The Other ◽  
Hydrophilic Polymer ◽  
Two Dimensional ◽  
Normal Tissues ◽  
Physical Chemical ◽  
Anti Cancer ◽  
Good Biocompatibility ◽  
Cancer Theranostics

Background and objective: Graphene-based nanomaterials have received increasing attention due to their unique physical-chemical properties including two-dimensional planar structure, large surface area, chemical and mechanical stability, superconductivity and good biocompatibility. On the other hand, graphene-based nanomaterials have been explored as theranostics agents, the combination of therapeutics and diagnostics. In recent years, grafting hydrophilic polymer moieties have been introduced as an efficient approach to improve the properties of graphene-based nanomaterials and obtain new nanoassemblies for cancer therapy. Methods and results: This review would illustrate biodistribution, cellular uptake and toxicity of polymergraphene nanoassemblies and summarize part of successes achieved in cancer treatment using such nanoassemblies. Conclusion: The observations showed successful targeting functionality of the polymer-GO conjugations and demonstrated a reduction of the side effects of anti-cancer drugs for normal tissues.

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