scholarly journals Soil Morphology, Physico-chemical Properties, Classification and Potential of Selected Soils in Kenya

2019 ◽  
pp. 1-12
Author(s):  
Anne N. Karuma
Keyword(s):  
Chemical Properties ◽  
Soil Classification ◽  
Classification Systems ◽  
Soil Profiles ◽  
Soil Morphology ◽  
Alkaline Ph ◽  
Soil Taxonomy ◽  
Physico Chemical ◽  
Physical And Chemical ◽  
Very High

Four soil profiles (Yala, Galana, Baringo and Bondo) that represent different ecology, physiography and pedological variability were described to study their morphology, soil physico-chemical characteristics and to classify them using two internationally known soil classification systems. Soil samples were taken from designated pedogenic horizons for physical and chemical analysis in the laboratory. These soils are deep to very deep (> 110 cm) and well-drained except in Galana which was imperfectly drained, with varying textures. In Bondo, the soils are moderately acid (pH 5.6 – 6). In Baringo, the soil profile is acidic (< 5.0) while in Galana moderately alkaline (pH 7.3 - 8.3) and Yala soils are moderate to strongly acid (5.1 - 5.7). The organic carbon (< 0.6%) and organic matter levels (1 – 2%) were low and decreased down the profiles in all. The soils have low to moderate fertility. The base saturation of the studied soils is rated as very high (> 80%) in Galana and Baringo and low (< 50%) in Yala and Bondo pedons. The soils are non-saline as indicated by the low values of electrical conductivity (< 1.7dS/m) in the pedons. The soils are non-sodic (ESP < 6%) in Bondo and Yala, however moderately sodic (ESP 11-15%) in Galana and Baringo. Ochric horizon was the main diagnostic epipedon while ferralic, argillic and cambic horizons were the diagnostic B horizons. According to USDA Soil Taxonomy, the soils were classified as Typic Haplustox (Yala), Typic Haplocalcids (Galana), Typic Eutrudepts (Baringo) and Plinthic Haplustults (Bondo) corresponding to Haplic Ferralsols, Luvic Calcisols, Haplic Cambisol and Cutanic Plinthic Acrisols in the WRB for Soil Resources. The general fertility of the soils of the areas is discussed highlighting their potentials and constraints.

scholarly journals Classificação dos solos da Planície do Delta do Parnaíba, PI (Soil classification of the Parnaíba Delta Plain, PI (1))

2019 ◽  
Vol 12 (4) ◽  
pp. 1466
Author(s):  
Léya Rodrigues Cabral ◽  
Gustavo Souza Valladares ◽  
Marcos Gervasio Pereira ◽  
Carlos Roberto Pinheiro Júnior ◽  
Andréa Maciel Lima ◽  
...  
Keyword(s):  
Rio De Janeiro ◽  
Chemical Properties ◽  
Morphological Characteristics ◽  
Soil Classification ◽  
Soil Profiles ◽  
Delta Plain ◽  
The North ◽  
Methodological Procedures ◽  
Physical And Chemical ◽  
Pedogenetic Processes

A diversidade natural dos solos reflete na paisagem a sua própria evolução, sendo estes resultados das interações entre os fatores de formação: material de origem, relevo, clima, organismos e tempo. Tais fatores, adjuntos aos processos pedogenéticos na evolução dos solos, definirão suas propriedades físicas e químicas, fundamentais para a caracterização dos solos. Nesse sentido, este estudo tem com o objetivo geral caracterizar e classificar os tipos de solos da planície do Delta do Parnaíba, localizada na região do Norte Piauiense, tendo como limite natural os rios Parnaíba e Igaraçu e o oceano Atlântico. Para a identificação e caracterização dos perfis de solos, foram realizadas atividades de campo, a fim de descrever e coletar os solos mais representativos na área de estudo. Foram descritos e coletados quinze perfis de solo por meio de trincheiras e tradagens, com extensões profundamente suficientes para avaliação das características morfológicas. Os critérios e procedimentos metodológicos seguiram a padronização adotada no Brasil. As análises físicas e químicas foram realizadas no Laboratório de Gênese e Classificação dos Solos da Universidade Federal Rural do Rio de Janeiro. Através dos resultados analisados foi possível classificar os solos de acordo com os níveis categóricos do Sistema Brasileiro de Classificação dos solos. As principais ordens de solos encontradas na área de estudo foram os Neossolos, Planossolos, Gleissolos, Espodossolos, Cambissolos e os Vertissolos. Novas classificações foram sugeridas, devido a características significativas encontradas nos perfis de solos que não se enquadrarem no Sistema Brasileiro de Classificação de Solos.  A B S T R A C TThe natural diversity of the soils reflects in the landscape its own evolution, being these results of the interactions between the factors of formation: material of origin, relief, climate, organisms and time. These factors, coupled with pedogenetic processes in soil evolution, will define their physical and chemical properties, fundamental for soil characterization. In this sense, this study has the general objective of characterizing and classifying the soil types of the Parnaíba Delta plains, located in the North Piauiense region, with the Parnaíba and Igaraçu rivers and the Atlantic Ocean as their natural limit. For the identification and characterization of soil profiles, field activities were carried out in order to describe and collect the most representative soils in the study area. Fifteen soil profiles were described and collected through trenches and traditions, with extensions deep enough to evaluate the morphological characteristics. The criteria and methodological procedures followed the standardization adopted in Brazil. Physical and chemical analyzes were performed at the Genesis and Soil Classification Laboratory of the Federal Rural University of Rio de Janeiro. Through the analyzed results it was possible to classify the soils according to the categorical levels of the Brazilian Soil Classification System. The main orders of soils found in the study area were the Neosols, Planosols, Gleysols, Spodosols, Cambisols and Vertisols. New classifications were suggested, due to significant characteristics found in soil profiles that do not fit into the Brazilian Soil Classification System.Keywords: Soil classification; Parnaíba Delta: pedogenetic processes.

scholarly journals Influence of fire on selected physico-chemical properties of forest soil

2019 ◽  
Vol 70 (1) ◽  
pp. 39-43
Author(s):  
Małgorzata Majder-łopatka ◽  
Wiesław Szulc ◽  
Beata Rutkowska ◽  
Dominik Ptasiński ◽  
Witold Kazberuk
Keyword(s):  
Organic Carbon ◽  
Chemical Properties ◽  
Test Material ◽  
Soil Profiles ◽  
Exchangeable Acidity ◽  
Physico Chemical ◽  
Negative Effect ◽  
Physical And Chemical ◽  
Nitrogen Contents ◽  
And Chemical Properties

Abstract The aim of the research was to determine whether, and to what extent, a surface fire of forest areas determines changes in physical and chemical properties of the soil. The test material consisted of soil samples taken from soil profiles exposed in a burnt-out area and in an area unaffected by fire. The samples were analyzed for total organic carbon and total nitrogen contents, and also selected indicators of soil acidification. As a result of the tests, it was found that there was a decrease in the levels of organic carbon (by over 75%) and nitrogen (by 50%). A negative effect of the changes was the narrowing of the C/N ratio, a positive one – an increase in soil pH (from 3.14 to 4.67), and a several-times reduction in hydrolytic and exchangeable acidity.

scholarly journals Identifikasi Sifat, Ciri, dan Jenis Tanah Utama di Pulau Lombok

2019 ◽  
Vol 5 (1) ◽  
pp. 19
Author(s):  
Joko Priyono ◽  
Ismail Yasin ◽  
Muhammad Dahlan ◽  
Bustan Bustan
Keyword(s):  
Chemical Properties ◽  
Soil Classification ◽  
Organic Content ◽  
X Ray Diffraction ◽  
Soil Taxonomy ◽  
Soil System ◽  
Descriptive Research ◽  
Fertile Soil ◽  
Physical And Chemical ◽  
Lombok Island

TA descriptive research aimed to identify the characteristics and name of main soils in Lombok Island was carried out through field observation for soil profiles and landform and laboratory analyses for soil physical and chemical properties. The type or name of soil was defined by using The National (Indonesian) Soil Classification System (2014), Soil Taxonomy (SSS-USDA, 2014), and World Soil Reference (FAO, 2014). There were 4 main types of soil in Lombok Island, which were Litosol, Aluvial, Kambisol, and Vertisol; and a fairly developed soil in limited spots was Mediteran. Based on the soil taxonomy system, those soils were respectively equivalent to Orthents, Fluvents, Undepts, Underts, and Udalfs; whereas based on the soil system of FAO, were Leptisols, Fluvisols, Cambisols, Vertisols, and Luvisols. The main characteristics of Litosol/Orthents/Leptosols Lombok were shallow solum (< 25 cm on the rocks or lithic contacts), coarse textured (sandy), nutritionally deficient, very low CEC (< 5 cmolc.kg-) and C-organic content (< 1 %). Aluvial or Fluvents, were mainly utilized as paddy soil, consisting of several layers which it clay and C-organic content were changed irregularly with depth, CEC of top soil (Ap) was medium (5–10 cmolc.kg-), and it was relatively fertile. Kambisols or Undepts was fairly deep (consisting of 40 – 60 cm of A and B horizons,), loamy textured, fairly fertile, CEC was medium, and C-organic content was low – medium (1–2 %). Vertisol or Uderts was characterized by a significant swell-shrinking properties, clay textured, extremely hard to be cultivated, high CEC, Ca, and Mg, and relatively fertile soil. Mediteran or Udalf was a further developed soil (solum > 100 cm), clay translocation has been occurred from upper (E) to lower horizons (Bt), CEC was fair, and it was relatively fertile soil. In conclusion, the pedologic development of soils in Lombok Island was relatively slow due mainly to the low–moderate rainfall, and the soil types were dominated by Litosols, Aluvials, Kambisols, and Vertisols, and Mediteran in small area. In order to provide a complete reference for the characteristics of main soils in Lombok Island, it necessaries to define mineralogy composition through X-ray diffraction analysis (XRD) and thermogravimetry analysis (TGA) of the clay fractions of the soils

scholarly journals Selected Chemical Properties of Necrosols from the Abandoned Cemeteries Słabowo and Szymonka (Great Mazurian Lakes District)

2012 ◽  
Vol 5 (1) ◽  
pp. 43-55 ◽  
Author(s):  
Leszek Majgier ◽  
Oimahmad Rahmonov
Keyword(s):  
Chemical Properties ◽  
Soil Horizon ◽  
Morphological Description ◽  
Soil Profiles ◽  
Anthropogenic Soils ◽  
Physico Chemical ◽  
Physical And Chemical ◽  
Burial Grounds ◽  
Cemetery Soils ◽  
And Chemical Properties

Abstract The paper shows the occurrences of cemetery soils and the physico-chemical features of soils in the cemeteries Słabowo and Szymonka (Great Mazurian Lakes District). Necrosols are anthropogenic soils and belong to Urbanosols. They form only in the area of cemeteries. Four soil profiles (Necrosols) were investigated in terms of morphological description and chemical properties especially phosphorus (Pt), organic carbon (OC) and nitrogen (Nt). These profiles were compared with the reference profile (Rusty soil, according to WRB 2007 Brunic Arenosol) made outside the cemetery. On the basis of research Necrosol has been defined as a soil formed by special human activity in cemeteries and burial grounds with specific soil horizon sequence, and also physical and chemical properties.

Ionic Liquids in Analytical Chemistry: Applications and Recent Trends

2021 ◽  
Vol 17 ◽  
Author(s):  
Giuseppe Maria Merone ◽  
Angela Tartaglia ◽  
Enrica Rosato ◽  
Cristian D’Ovidio ◽  
Abuzar Kabir ◽  
...  
Keyword(s):  
Analytical Chemistry ◽  
Ionic Liquids ◽  
Stationary Phases ◽  
Extraction Procedure ◽  
Chemical Properties ◽  
Electrochemical Analysis ◽  
Physico Chemical ◽  
Recent Trends ◽  
Number Of Publications ◽  
Physical And Chemical

Background: Ionic liquids (ILs) are a unique class of compounds consisting exclusively of cations and anions that possess distinctive properties such as low volatility, high thermal stability, miscibility with water and organic solvents, electrolytic conductivity and non-flammability. Ionic liquids have been defined as "design solvents", because it is possible to modify their physical and chemical properties by appropriately choosing cations and anions, in order to meet the specific characteristics based on their potential application. Introduction: Due of their tunable nature and properties, ILs are considered as the perfect candidates for numerous applications in analytical chemistry including sample preparation, stationary phases in liquid or gas chromatography, additives in capillary electrophoresis, or in mass spectrometry for spectral and electrochemical analysis. In the last years, the number of publications regarding ILs has rapidly increased, highlighting the broad applications of these compounds in various fields of analytical chemistry. Results: This review first described the main physico-chemical characteristics of ionic liquids, and subsequently reported the various applications in different subdisciplines of analytical chemistry, including the extraction procedure and separation techniques. Furthermore, in each paragraph the most recent applications of ionic liquids in the food, environmental, biological, etc. fields have been described. Conclusion: Overall, the topic discussed highlights the key role of ionic liquids in analytical chemistry, giving hints for their future applications in chemistry but also in biology and medicine.

scholarly journals Effect of Slice Weight and Soaking Time on the Physico-Chemical Properties of Cassava Flour (Manihotesculentus) used for Bakery Products

2021 ◽  
pp. 10-24
Author(s):  
C. R. Abah ◽  
C. N. Ishiwu ◽  
J. E. Obiegbuna ◽  
E. F. Okpalanma ◽  
C. S. Anarado
Keyword(s):  
Chemical Properties ◽  
Process Variables ◽  
Soaking Time ◽  
Cassava Flour ◽  
Baked Goods ◽  
Cassava Root ◽  
Physico Chemical ◽  
Physical And Chemical ◽  
And Chemical Properties

Quality cassava(Manihotesculentus, Crantz) flour is often influenced by process variables such as slice weight and soaking time which may affect its nutritional quality. In this study, the effect of process variables (slice weight and soaking time) on quality of cassava flour was carried out. Cassava root was peeled, washed and cut into varied sizes (25.86 - 54.14 g) and soaked at varied time (7.03 - 40.97 h). The proximate composition, physical and chemical properties of the flour were carried out using standard methods. The result in our findings showed that slice weight and soaking time had significant increase (p<0.05) on the proximate and physico-chemical properties of the flour.The amylose and amylopectin content of the flour increased with increasing soaking time while the hydrogen cyanide content decreased with increase in soaking time. Overall, the quality cassava flour displayed desirable properties for its incorporation into baked goods.

scholarly journals Classification and assessment of agricultural potential of the lower Niger floodplain soils of Atani, Southeastern Nigeria

Agro-Science ◽  
2020 ◽  
Vol 19 (3) ◽  
pp. 51-61
Author(s):  
F.C. Okenmuo ◽  
C.O. Anochie ◽  
M.E. Ukabiala ◽  
C.L.A. Asadu ◽  
P.K. Kefas ◽  
...  
Keyword(s):  
Chemical Properties ◽  
Soil Classification ◽  
Exchange Capacity ◽  
Available Phosphorus ◽  
Soil Taxonomy ◽  
Southeastern Nigeria ◽  
Reference Base ◽  
Anambra State ◽  
Agricultural Potential ◽  
Capability Evaluation

The soils of Atani floodplain in Anambra State of Nigeria contribute significantly to the food production of the State, hence the need to understand their behavior in order to enhance their management and productivity. Profile pits were sited along three physiographic units viz: levee crest, levee  slope and flood basin. Soil samples were collected from the profile horizons and subjected to standard laboratory procedures. Characterization of the soils was based on their morphological, physical and chemical properties. Soil classification was carried out using the USDA Soil Taxonomy and correlated with FAO/IUSS World Reference Base. Its agricultural potential was assessed using the fertility capability classification. The soils were deep. Topsoil colour was dominantly blackish black (10YR 3/2). Mottles were pervasive; an indication of impeded drainage conditions. The soils were predominantly fine textured. Soil pH values ranged from 4.8 to 6.2. Exchangeable Calcium was low to moderate (2.6-8.2 cmol kg−1); Magnesium was moderate to high (1.6-6.8 cmol kg−1); Sodium was high to very high (1.0-2.5 cmol kg−1), while potassium was high (1.2-4.2 cmol kg−1). Cation  exchange capacity values ranged from 11.6 to 42.6 cmol kg−1. Total nitrogen was very low to low (0.14-1.12 g kg−1), while organic carbon was low to moderate (0.4-15.2 g kg−1). Available phosphorus was very low to high ranging from 0.93 to 31.71 mg kg−1 while base saturation ranged from 64 to 93%. The soils were classified as Typic Fluvaquents (Typic Fluvisols), Fluvaquentic Endoaquepts (Endostagnic Cambisols) and Fluventic Endoaquepts (Endostagnic Cambisols) according to the USDA and FAO/IUSS. The fertility capability evaluation of the soils revealed that the pedons were Lgn in classification due to limitations in drainage. Key words: alluvium, cambic horizon, Inceptisols, lithologic discontinuity

scholarly journals Free-standing spider silk webs of the thomisid Saccodomus formivorus are made of composites comprising micro- and submicron fibers

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Christian Haynl ◽  
Jitraporn Vongsvivut ◽  
Kai R. H. Mayer ◽  
Hendrik Bargel ◽  
Vanessa J. Neubauer ◽  
...  
Keyword(s):  
Spider Silk ◽  
Structural Integrity ◽  
Chemical Properties ◽  
Free Standing ◽  
Physico Chemical ◽  
Physical And Chemical ◽  
Crab Spiders ◽  
Ambush Predators ◽  
The Web ◽  
And Chemical Properties

Abstract Our understanding of the extraordinary mechanical and physico-chemical properties of spider silk is largely confined to the fibers produced by orb-weaving spiders, despite the diversity of foraging webs that occur across numerous spider families. Crab spiders (Thomisidae) are described as ambush predators that do not build webs, but nevertheless use silk for draglines, egg cases and assembling leaf-nests. A little-known exception is the Australian thomisid Saccodomus formivorus, which constructs a basket-like silk web of extraordinary dimensional stability and structural integrity that facilitates the capture of its ant prey. We examined the physical and chemical properties of this unusual web and revealed that the web threads comprise microfibers that are embedded within a biopolymeric matrix containing additionally longitudinally-oriented submicron fibers. We showed that the micro- and submicron fibers differ in their chemical composition and that the web threads show a remarkable lateral resilience compared with that of the major ampullate silk of a well-investigated orb weaver. Our novel analyses of these unusual web and silk characteristics highlight how investigations of non-model species can broaden our understanding of silks and the evolution of foraging webs.

scholarly journals Interferons: Purification and Physicochemical Aspects

1970 ◽  
Vol 56 (1) ◽  
pp. 113-133 ◽  
Author(s):  
K. H. Fantes
Keyword(s):  
Chemical Properties ◽  
Pure Substance ◽  
Physical And Chemical Properties ◽  
High Purification ◽  
Interferon Activity ◽  
Physical And Chemical ◽  
Very High ◽  
And Chemical Properties

Antiviral interferon activity in any one species can be exhibited by a variety of substances that differ in their physical and chemical properties, but the nature of these differences is not understood. Conditions that can lead to the formation of diverse types of interferons have been outlined. Reasons have been adduced why, for certain purposes, purification of interferons is desirable or even necessary, and examples have been presented to show how and to what extent this has been achieved. In spite of some very high purification factors, not a single interferon has been obtained as a pure substance. Therefore, all available knowledge of physical and chemical properties has been obtained by indirect means.

Classification and Mitigation of Soil Salinization

2017 ◽  
Author(s):  
Tibor Tóth
Keyword(s):  
Soil Salinity ◽  
Soil Classification ◽  
Soil Salinization ◽  
Classification Systems ◽  
Salt Accumulation ◽  
Soil Taxonomy ◽  
Sodic Soils ◽  
Water Rates ◽  
Irrigated Lands ◽  
The Right

Soil salinity has been causing problems for agriculturists for millennia, primarily in irrigated lands. The importance of salinity issues is increasing, since large areas are affected by irrigation-induced salt accumulation. A wide knowledge base has been collected to better understand the major processes of salt accumulation and choose the right method of mitigation. There are two major types of soil salinity that are distinguished because of different properties and mitigation requirements. The first is caused mostly by the large salt concentration and is called saline soil, typically corresponding to Solonchak soils. The second is caused mainly by the dominance of sodium in the soil solution or on the soil exchange complex. This latter type is called “sodic” soil, corresponding to Solonetz soils. Saline soils have homogeneous soil profiles with relatively good soil structure, and their appropriate mitigation measure is leaching. Naturally sodic soils have markedly different horizons and unfavorable physical properties, such as low permeability, swelling, plasticity when wet, and hardness when dry, and their limitation for agriculture is mitigated typically by applying gypsum. Salinity and sodicity need to be chemically quantified before deciding on the proper management strategy. The most complex management and mitigation of salinized irrigated lands involves modern engineering including calculations of irrigation water rates and reclamation materials, provisions for drainage, and drainage disposal. Mapping-oriented soil classification was developed for naturally saline and sodic soils and inherited the first soil categories introduced more than a century ago, such as Solonchak and Solonetz in most of the total of 24 soil classification systems used currently. USDA Soil Taxonomy is one exception, which uses names composed of formative elements.

Sign in / Sign up

Export Citation Format

Share Document