scholarly journals Characterization and Taxonomy Classification of Soils of Hill Slope Land and Stream Terrace Land Located at North-Eastern Ghat Agro-Climatic Zone of Odisha, India

2021 ◽  
pp. 203-209
Author(s):  
Tupaki Lokya ◽  
Antaryami Mishra ◽  
Subhashis Saren
Keyword(s):  
Exchange Capacity ◽  
Taxonomic Classification ◽  
Climatic Zone ◽  
Organic Carbon Content ◽  
Eastern Ghat ◽  
Hill Slope ◽  
North Eastern ◽  
Topographic Positions ◽  
The Hill

The present investigation was carried out to study the characterization, fertility status and taxonomic classification of some soils of North-Eastern Ghat Agro-Climatic zone of Odisha. Hill slope (pedon 1) and stream terrace land (pedon 2) two representative pedons of the Nayagarh district located in different topographic positions were studied for their physico-chemical characteristics and taxonomic classification. Results show that in pedon 1, percentage of sand, silt and clay range between 78.4 to 86.4, 3.2 to 3.4 and 10.4 to 17.4 respectively and in pedon 2, sand, silt and clay percentages range between 72 to 84, 3.2 to 7.2 and 10.8 to 18.8 respectively in different horizons. In pedons 1 and 2, pH increases along with depth from 4.80 to 5.82 and 5.80 to 7.60 respectively. Organic carbon content in pedons 1 and 2, ranges from 3.4 to 5.1 and 1.6 to 6.3 g kg-1 respectively. Cation exchange capacity decreases in pedon 1 from 13.25 to 8.66 c mol (p+) kg-1 and in pedon 2, range 7.66 to 16.65 c mol (p+) kg-1. The exchangeable sodium percentage in pedon 1 and 2, ranges from 4.53 to 9.23, and 2.56 to 6.53 per cent in different horizons respectively. The base saturation percentage in pedon 1, range from 58.11 to 98.15 per cent and in pedon 2, from 59.54 to 97.91 percent. The Hill slope (pedon 1) and stream terrace land (pedon 2) have little or no evidence of development of pedogenic horizons except ochric epipedon, therefore these soil are classified under the order Entisols. These soils have A-C profile with no distinct horizonation. Pedon 1, are classified under sub order Orthents, great group Ustorthents and sub group Typic Ustorthents. In case of pedon 2 the soils are put under the sub order Aquents, great group Fluvaquents and sub group Aeric Fluvaquents.

ETUDE SUR LA VALEUR DES CRITERES CHIMIQUES PROPOSES PAR LA COMMISSION PEDOLOGIQUE DU CANADA POUR LA CLASSIFICATION TAXONOMIQUE DES SOLS DU QUEBEC

1977 ◽  
Vol 57 (3) ◽  
pp. 233-247 ◽  
Author(s):  
ROGER W. BARIL ◽  
THI SEN TRAN
Keyword(s):  
Cation Exchange ◽  
Soil Ph ◽  
Classification System ◽  
Cation Exchange Capacity ◽  
Exchange Capacity ◽  
Taxonomic Classification ◽  
Single Test ◽  
Ph Dependent ◽  
Extractable Al

Correlations were made among chemical criteria used for taxonomic soil classificaton. The compared tests were: oxalate Δ (Fe + Al), pyrophosphate-extractable (Fe + Al), oxalate-extractable Al, pH-dependent cation exchange capacity (ΔCEC), ratios of pyrophosphate-extractable (Fe + Al) over clay or over dithionite-extractable (Fe + Al), and finally soil pH measured in 1 M NaF. Significant correlations were found among various measured parameters. However, no single test was found to be reliable as a single criterion when applied to the taxonomic classification of Quebec soils. The two chemical tests, pyrophosphate-extractable (Fe + Al) and its ratio over clay, combined with morphologic criteria appeared useful for classifying Quebec Podzols. A few soils, which presented discrepancies from chemical criteria were found difficult to classify, thus suggesting the possibility of establishing new sub-groups in the Canadain soil taxonomic classification system.

scholarly journals Characterization and classification of soils of Northern hills Zone of Chhattisgarh, Madhya Pradesh

2021 ◽  
Vol 17 (AAEBSSD) ◽  
pp. 147-149
Author(s):  
P.N. Tripathi ◽  
U.S. Mishra ◽  
Pawan Sirothia ◽  
R.P. Singh
Keyword(s):  
Cation Exchange Capacity ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Organic Carbon Content ◽  
Physical And Chemical Properties ◽  
Clay Loam ◽  
Physical And Chemical ◽  
And Chemical Properties

Three representative soil pedonsof northern hills of Chhattisgarh, M.P were morphologically studied, characterized and classified. The soils are very deep, colour ranges from brown (10YR5/3) to dark brown (10YR3/3) and very dark greyish brown (10YR3/2) in different horizons. Fe and calcretes are observed in sub surface horizons. The texture in surface soils varied from clay loam to clay while in pedon 2, the texture was observed sandy clay loam throughout the profile. The soils are calcareous and pH ranged from 7.0 to 7.5. The organic carbon content in these soils were (4.4 g kg-1), low to medium (6.1 g kg-1) in surface and decreased with depth. Cation exchange capacity (CEC) were found high in horizons where clay content was more. Based on morphological, physical and chemical properties P1 and P3 were classified as VerticHaplustalfs and pedon (P2) was placed under Typic Haplustepts.

scholarly journals Characterization and Classification of soils on different Geomorphic Units of North-Eastern Haryana, India

Agropedology ◽  
2019 ◽  
Vol 27 (2) ◽  
Author(s):  
◽  
Mohammad Amin Bhat ◽  
K.S. Grewal ◽  
◽  
Keyword(s):  
Water Retention ◽  
Particle Density ◽  
Total Porosity ◽  
Exchange Capacity ◽  
Flood Plains ◽  
North Eastern ◽  
Retention Characteristics ◽  
Geomorphic Units ◽  
Physical And Chemical

Twelve pedons occurring on different landforms of North-Eastern Haryana were characterized for morphological, physical and chemical characteristics and classified. The soil colour of pedons varied from yellowish brown to reddish/ dark brown in the hues of 10YR, 5YR and 2.5YR. The soils of Shiwalik hills, upper piedmont plains and flood plains, lower piedmont plains and old alluvial plains were medium to moderately heavy in texture, relatively lighter and light to moderately heavy in texture, respectively. The soils have weak to medium subangular blocky structure. The sub surface horizons in old alluvial plains showed the translocation and accumulation of clay. The soils of the area were moderately alkaline to strongly alkaline (pH 7.5-9.4). The organic carbon was less than 1 per cent except surface horizons of forest areas. The water retention characteristics of soils were strongly associated to texture with the finer soil showing higher retention and vice-versa. The particle density, bulk density and total porosity varied from 2.20 to 2.84, 1.16 to 1.45 Mg m−3 and 40.43 to 56.78 per cent, respectively and did not show regular pattern down the profile. The cation exchange capacity varied from 5.21 to 17.00 cmol (p+) kg−1.

scholarly journals A Consensus Framework Unifies Multi-Drug Synergy Metrics

2019 ◽  
Author(s):  
David J. Wooten ◽  
Christian T. Meyer ◽  
Vito Quaranta ◽  
Carlos Lopez
Keyword(s):  
Drug Combination ◽  
Mass Action ◽  
Maximal Effect ◽  
Drug Synergy ◽  
Synergistic Interactions ◽  
Broad Applicability ◽  
Hill Slope ◽  
The Hill ◽  
The Relationship

AbstractDrug combination discovery depends on reliable synergy metrics; however, no consensus exists on the appropriate synergy model to prioritize lead candidates. The fragmented state of the field confounds analysis, reproducibility, and clinical translation of combinations. Here we present a mass-action based formalism to accurately measure the synergy of drug combinations. In this work, we clarify the relationship between the dominant drug synergy principles and show how biases emerge due to intrinsic assumptions which hinder their broad applicability. We further present a mapping of commonly used frameworks onto a unified synergy landscape, which identifies fundamental issues impacting the interpretation of synergy in discovery efforts. Specifically, we infer how traditional metrics mask consequential synergistic interactions, and contain biases dependent on the Hill-slope and maximal effect of single-drugs. We show how these biases systematically impact the classification of synergy in large combination screens misleading discovery efforts. The proposed approach has potential to accelerate the translatability and reproducibility of drug-synergy studies, by bridging the gap between the curative potential of drug mixtures and the complexity in their study.

scholarly journals Characterization and Classification of Soils from Different Topographic Positions under Sugarcane Plantation in South Sulawesi, Indonesia

2019 ◽  
Vol 24 (2) ◽  
pp. 93
Author(s):  
Risma Neswati ◽  
Christianto Lopulisa ◽  
Ahmad Faudzan Adzima
Keyword(s):  
Soil Formation ◽  
Soil Classification ◽  
Exchange Capacity ◽  
Soil Taxonomy ◽  
South Sulawesi ◽  
Topographic Positions ◽  
Pore Types ◽  
Void Pores ◽  
Basic Cations

The varied topography will influence the soil formation. This study aims to characterize and classify the soil selected on different topography positions of the sugarcane plantation area. The research was conducted in sugarcane plantation area of Camming, District of Bone, South Sulawesi, which was carried out from November 2017 to March 2018. This study used a descriptive method, observation and description of the nine soil profiles at three transects. Each transect consisted of three profiles points located in different positions, consisting of summit, backslope, and valleys. Each horizon soil samples were analyzed for their physical, chemical and micromorphology characteristics in the laboratory. Soil classification system was done by using soil taxonomy to the level of subgroups. The results showed that an average rainfall annual on the research location was 2.200 mm per year. Soil characteristics such as soil solum, cation exchange capacity, and sum of basic cations tended to increase in parts of the valley than in the back and summit. The primary mineral from the sand fraction included quartz, calcite, biotite, opaque, and orthoclase found especially in the position of the back and valley. The pore types consisted of vugh and packing void pores. Pedofeature type of soil was generally in the form of concretions and nodules that showed the process of oxidation and reduction. The soil type in the study area was classified into Typic Haplustepts and Typic Haplustalf.

The Preliminary Study on Definition of Slope Debris Flow

2014 ◽  
Vol 955-959 ◽  
pp. 3630-3634
Author(s):  
Shi Yue Fang ◽  
Jun Yang
Keyword(s):  
Debris Flow ◽  
Hill Slope ◽  
Formation Conditions ◽  
Preliminary Study ◽  
Definition Of ◽  
The Hill ◽  
Slope Debris Flow ◽  
Flow Study

So far, the definitions of slope debris flow are cinders and divergent, even, some scholars equate it with the hill slope debris flow/landslide-induced debris flow and other similar terms. This article summarizes research on the slope debris flow, from the definition and classification of debris flow, study on the classification of slope debris flow , analyzes the formation conditions, properties and characteristics of slope debris flow, at last, use the definition method of attribute and kind, tentatively give the preliminary definition of the slope debris flow .

Wind tunnel tests and dynamic analysis of wind-induced response of a transmission tower on a hill

2021 ◽  
pp. 136943322110339
Author(s):  
Jian Guo ◽  
Changliang Xiao ◽  
Jiantao Li
Keyword(s):  
Wind Tunnel ◽  
Wind Field ◽  
Dynamic Responses ◽  
Interactive Effects ◽  
Induced Response ◽  
Transmission Tower ◽  
Structural Dynamic ◽  
Wind Tunnel Tests ◽  
Hill Slope ◽  
The Hill

A hill with a lattice transmission tower presents complex wind field characteristics. The commonly used computational fluid dynamics (CFD) simulations are difficult to analyze the wind resistance and dynamic responses of the transmission tower due to structural complexity. In this study, wind tunnel tests and numerical simulations are conducted to analyze the wind field of the hill and the dynamic responses of the transmission tower built on it. The hill models with different slopes are investigated by wind tunnel tests to measure the wind field characteristics, such as mean speed and turbulence intensity. The study shows that the existence of a transmission tower reduces the wind speed on the leeward slope significantly but has little effect on the windward slope. To study the dynamic behavior of the transmission tower, a hybrid analysis procedure is used by introducing the measured experimental wind information to the finite element tower model established using ANSYS. The effects of hill slope on the maximum displacement response of the tower are studied. The results show that the maximum value of the response is the largest when the hill slope is 25° compared to those when hill slope is 15° and 35°. The results extend the knowledge concerning wind tunnel tests on hills of different terrain and provide a comprehensive understanding of the interactive effects between the hill and existing transmission tower regarding to the wind field characteristics and structural dynamic responses.

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