scholarly journals Komposisi Fraksi Pasir dan Sifat Kimia Tanah Pada Areal Revegetasi Lahan Bekas Tambang Batubara

2020 ◽  
Vol 8 (2) ◽  
pp. 46
Author(s):  
Ria Rachel Paranoan
Keyword(s):  
Cation Exchange Capacity ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Rock Fragment ◽  
Sand Fraction ◽  
Exchangeable Ca ◽  
P Content ◽  
Mineralogical Compositions ◽  
Very High ◽  
And Chemical Properties

The purpose of this research were to determine the composition of sand fraction and chemical properties at revegetation area. The research was conducted from April to October 2019 . The mineralogical Compositions of sand fraction were analyzed using a Polarizing Microscope (PM) at the laboratory of Mineral BB Litbang SDLP, Bogor. The results showed that the composition of sand fractionof soil at revegetation area was dominatd by quartz,with small amounts of opaque, zircon,weathered mineral, rock fragment, and tourmaline.Chemical properties indicated that the soil at revegetation area showed pH from 6,05 to 6,49, had low content of cation exchange capacity in the whole layers, very high content of base saturation, very low to low organic carbon. Exchangeable K and Na are low in the whole layers, the moderate content of potential potassium. Both exchangeable Ca and Mg were lot to moderate. Potentioal P content in soil varies from moderate to high.Soil management in revegetation area should be focused on Maintaining soil fertility through application of liming, and fertilizers

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 STRONTIUM CONTENT IN SANDY SOILS IN AGRICULTURE FIELDS (CASE STUDY: MOUNDOU, CHAD)

AGROFOR ◽  
2018 ◽  
Vol 3 (2) ◽  
Author(s):  
Kamssou KOI ◽  
Victor NAGORNY ◽  
Otilija MISECKAITE ◽  
Yuri MAZHAYSKY
Keyword(s):  
Soil Depth ◽  
Chemical Properties ◽  
Sandy Soils ◽  
Total Content ◽  
Exchange Capacity ◽  
Strontium Content ◽  
Physical And Chemical ◽  
Very High ◽  
And Chemical Properties

During evaluation of physical and chemical properties of sandy soils and theirfertility in Southern part of Republic of Chad it has been revealed that some soilshave very high content of strontium. Its content varies from 10 to 270 mg/kg ofsoil depending on type of soil, depth of soil layers, clay and organic content.Strontium content negatively correlates with total content of calcium andphosphorus in layers of soil. Low CEC (CEC - Cation-exchange capacity) of soilmay be a reason of possible translocation of strontium from higher to lower layersof soils. Strontium content in soils do not relates with level of radioactivity of soilmeasured. The highest content of strontium has been found in soils developed onsome eolian and colluvio-alluvium deposits. Some researchers hypothesize thatsome endemic and chronic diseases such as Kashin-Beck disease, `Dysostosisenchondralis endemic`, endemic hoiter, osteoarthritis might be caused by highcontent of strontium in water and plant foods contaminated with it. Absence ofconsensus on etiological factors of these diseases confirms that it is worthconsidering necessity of further studies of different affects of high content ofstrontium in water and foods on human health directly or indirectly throughcausing misbalance in mineral nutrition.

scholarly journals CHANGES IN THE PHYSICAL AND CHEMICAL PROPERTIES OF SOIL UNDER THE INFLUENCE OF MANURE, GREEN MANURE AND THE STOVER BIODESTRUCTOR

2020 ◽  
Author(s):  
А.В. Сафонов ◽  
Е.Н. Кузин ◽  
А.Н. Арефьев ◽  
Е.Е. Кузина
Keyword(s):  
Cation Exchange ◽  
Green Manure ◽  
Cation Exchange Capacity ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Physical And Chemical Properties ◽  
Physical And Chemical ◽  
Compound Action ◽  
And Chemical Properties ◽  
Hydrolytic Acidity

Интенсификация земледелия в лесостепной зоне Среднего Поволжья требует решения проблемы сохранения почвенного покрова и его потенциального и эффективного плодородия с целью повышения урожайности сельскохозяйственных культур и качества растениеводческой продукции. В связи с этим разработка и внедрение в земледельческую практику агробиологических приемов предотвращения антропогенной деградации в агроландшафтах является актуальным направлением современной аграрной науки. Цель исследований заключалась в сравнительной оценке влияния навоза, сидератов и их сочетаний с биодеструктором стерни на физико-химические свойства лугово-черноземной почвы. Для достижения поставленной цели были проведены исследования в период с 2017 по 2019 гг. в первом агропочвенном районе Пензенской области. Исследованиями установлено, что действие и последействие навоза, сидератов и их комплексное действие и последействие с биодеструктором стерни оказало положительное влияние на физико-химические свойства лугово-черноземной почвы. Сидеральные пары по эффективности влияния на емкость катионного обмена, сумму обменных оснований, величину обменной и гидролитической кислотности не уступали унавоженным парам. Более существенное влияние на изменение физико-химических свойств почвы оказало комплексное действие и последействие навоза, редьки масличной и бобовых сидератов с биодеструктором стерни. Емкость катионного обмена на их фоне увеличилась на 1,40-1,51 мг-экв./100 г почвы, сумма обменных оснований на 1,6-1,7 мг-экв./100 г почвы, величина рНсолна 0,22-0,24 ед., величина гидролитической кислотности снизилась на 0,17-0,19 мг-экв./100 г почвы. Intensification of agriculture in the forest-steppe zone of the Middle Volga region requires solving the problem of preserving the soil and its potential and effective fertility in order to increase crop productivity and quality of crop production. In this regard, the development and implementation in agricultural practice of agrobiological techniques to prevent anthropogenic degradation in agricultural landscapes is an urgent direction of modern agricultural science. The purpose of the research was to compare the effect of the implementation of manure, green manure and their combinations with the stover biodestructor on the physical and chemical properties of meadow-chernozemic soil. To reach this purpose, research was conducted in the period from 2017 to 2019 in the first agro-soil district of the Penza region. Research has shown that the effect and after-effect of manure, green manure and their compound action and after-action with the stover biodestructor had a positive effect on the physical and chemical properties of meadow-chernozemic soil. Green manure fallows were not inferior to manured fallows in terms of their effect on the cation-exchange capacity, the sum of exchange bases, and the amount of exchange and hydrolytic acidity. A compound action and after-action of manure, the oil radish and green manure of legumes with the stover biodestructor had a more significant influence on the change in the physical and chemical properties of the soil. In their background, the cation-exchange capacity increased by 1.40-1.51 mg equivalent/100 g of soil, the sum of exchange bases by 1.6-1.7 mg equivalent/100 g of soil, the value of рНКСl 0.22-0.24 units, the value of hydrolytic acidity decreased by 0.17-0.19 mg equivalent/100 g of soil.

scholarly journals Nutrient and Chemical Properties of Aging Golf Course Putting Greens as Impacted by Soil Depth and Mat Development

HortScience ◽  
2009 ◽  
Vol 44 (2) ◽  
pp. 452-458 ◽  
Author(s):  
Ty A. McClellan ◽  
Roch E. Gaussoin ◽  
Robert C. Shearman ◽  
Charles S. Wortmann ◽  
Martha Mamo ◽  
...  
Keyword(s):  
Cation Exchange ◽  
Cation Exchange Capacity ◽  
Root Zone ◽  
Soil Depth ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Soil Samples ◽  
Putting Greens ◽  
Putting Green ◽  
And Chemical Properties

Nutrient and chemical changes in turfgrass sand-based root zones are not well understood. This study was conducted to characterize nutrient and chemical properties in putting greens influenced by root zone mixture and establishment treatment, putting green age, and soil depth. Putting greens were constructed and established with Agrostis stolonifera L. in sequential years from 1997 to 2000. Treatments included root zone mixtures of 80:20 (v:v) sand and sphagnum peat and 80:15:5 (v:v:v) sand, sphagnum peat, and soil, and accelerated versus controlled establishment. In the establishment year, the accelerated treatment received 2.6-, 3.0-, and 2.6-fold more nitrogen, phosphorus, and potassium, respectively, than the controlled treatment. Soil samples were taken in Fall 2001, Spring 2004, and Summer 2004 and were analyzed for nutrient and chemical properties such as pH, cation exchange capacity (CEC), organic matter (OM), total soluble salts (TSS), and 12 nutrients. The root zone mixture and establishment treatments had minimal effects on most nutrient and chemical properties with the exception of phosphorus and pH. Cation exchange capacity, OM, TSS, and all nutrients decreased with soil depth, whereas soil pH increased. The putting green age × soil depth interaction was significant for many of the nutrient and chemical properties, but separating soil samples into mat and original root zone instead of predetermined soil sampling depths eliminated most of these interactions. The mat layer had higher CEC and OM values and nutrient concentrations and lower pH values than the original root zone mixture.

scholarly journals Identifying Potential Leakage Zones in an Irrigation Supply Channel by Mapping Soil Properties Using Electromagnetic Induction, Inversion Modelling and a Support Vector Machine

Soil Systems ◽  
2020 ◽  
Vol 4 (2) ◽  
pp. 25
Author(s):  
Ehsan Zare ◽  
Nan Li ◽  
Tibet Khongnawang ◽  
Mohammad Farzamian ◽  
John Triantafilis
Keyword(s):  
Electrical Conductivity ◽  
Support Vector Machine ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Future Research ◽  
Support Vector ◽  
Stream Channels ◽  
Supply Channel ◽  
Physical And Chemical ◽  
And Chemical Properties

The clay alluvial plains of Namoi Valley have been intensively developed for irrigation. A condition of a license is water needs to be stored on the farm. However, the clay plain was developed from prior stream channels characterised by sandy clay loam textures that are permeable. Cheap methods of soil physical and chemical characterisations are required to map the supply channels used to move water on farms. Herein, we collect apparent electrical conductivity (ECa) from a DUALEM-421 along a 4-km section of a supply channel. We invert ECa to generate electromagnetic conductivity images (EMCI) using EM4Soil software and evaluate two-dimensional models of estimates of true electrical conductivity (σ—mS m−1) against physical (i.e., clay and sand—%) and chemical properties (i.e., electrical conductivity of saturated soil paste extract (ECe—dS m−1) and the cation exchange capacity (CEC, cmol(+) kg−1). Using a support vector machine (SVM), we predict these properties from the σ and depth. Leave-one-site-out cross-validation shows strong 1:1 agreement (Lin’s) between the σ and clay (0.85), sand (0.81), ECe (0.86) and CEC (0.83). Our interpretation of predicted properties suggests the approach can identify leakage areas (i.e., prior stream channels). We suggest that, with this calibration, the approach can be used to predict soil physical and chemical properties beneath supply channels across the rest of the valley. Future research should also explore whether similar calibrations can be developed to enable characterisations in other cotton-growing areas of Australia.

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.

Relationship between certain physical and chemical properties and subsoil friability in Lemnos loam

1974 ◽  
Vol 14 (70) ◽  
pp. 694 ◽  
Author(s):  
EH Mikhail ◽  
WI Walbran
Keyword(s):  
Chemical Properties ◽  
Aggregate Stability ◽  
Strong Relationship ◽  
Fruit Production ◽  
Multiple Regression Equation ◽  
Exchangeable Ca ◽  
Field Assessment ◽  
Physical And Chemical ◽  
Significant Factors ◽  
And Chemical Properties

Lemnos loam, a red-brown earth used for fruit production in the Goulburn Valley, Victoria, has degrees of friability in the subsoil as assessed in the field. Forty-one samples from three subsoil depths were obtained from 25 sites near Kyabram. Aggregate stability, as measured in the laboratory was found to be related to field assessments of friability. Exchangeable cations, pH, silt, clay and clay minerals were determined on the samples. By relating some of these measurements to aggregate stability it has been shown that exchangeable Ca++ contributes to a strongly aggregated soil (friable) ; and silt, exchangeable Na+ and exchangeable Mg++ to a weakly aggregated soil (less friable). The effect of silt and exchangeable Na+ is greater than that of exchangeable Ca++ and exchangeable Mg++. A multiple regression equation describing the effect of these four significant factors on stability percentage is presented. This equation accounts for 85.5 per cent of the variation in stability percentage. There is a strong relationship between field assessment of friability and exchangeable Ca++/Mg++ ratio; the higher the ratio, the more friable is the soil.

scholarly journals Eosin Removal by Cetyl Trimethylammonium-Cloisites: Influence of the Surfactant Solution Type and Regeneration Properties

Molecules ◽  
2019 ◽  
Vol 24 (16) ◽  
pp. 3015
Author(s):  
Fethi Kooli ◽  
Souad Rakass ◽  
Yan Liu ◽  
Mostafa Abboudi ◽  
Hicham Oudghiri Hassani ◽  
...  
Keyword(s):  
Cation Exchange ◽  
Clay Mineral ◽  
Salt Solution ◽  
Cation Exchange Capacity ◽  
Chemical Properties ◽  
Surfactant Solution ◽  
Exchange Capacity ◽  
Maximum Temperature ◽  
Basal Spacing ◽  
Xrd Techniques

The effect of the counteranion of hexadecyltrimethylammonium salts on the physico-chemical properties of organoclays was investigated, using a selected natural clay mineral with a cation exchange capacity of 95 meq/100 g. The uptake amount of C16 cations was dependent on the hexadecyltrimethylammonium (C16) salt solution used, the organoclay prepared from C16Br salt solution exhibited a value of 1. 05 mmole/g higher than those prepared from C16Cl and C16OH salt solutions. The basal spacing of these organoclays was in the range of 1.81 nm to 2.10 nm, indicating a similar orientation of the intercalated surfactants, and could indicated that the excess amount of surfactants, above the cation exchange capacity of 0.95 meq/g could be adsorbed on the external surface of the clay mineral sheets. These organoclays were found to be stable in neutral, acidic, and basic media. The thermal stability of these organoclays was carried out using thermogravimetric analysis and in-situ X-ray diffraction (XRD) techniques. The decomposition of the surfactant occurred at a maximum temperature of 240 °C, accompanied with a decrease of the basal spacing value close to 1.42 nm. The application of these organoclays was investigated to remove an acidic dye, eosin. The removal amount was related to the initial used concentrations, the amount of the surfactants contents, and to the preheated temperatures of the organoclays. The removal was found to be endothermic process with a maximum amount of 55 mg of eosin/g of organoclay. The value decreased to 25 mg/g, when the intercalated surfactants were decomposed. The reuse of these organoclays was limited to four regeneration recycles with a reduction of 20 to 30%. However, noticeable reduction between 35% to 50% of the initial efficiency, was achieved after the fifth cycle, depending of the used organoclays.

The ameliorative effects of low-grade palygorskite on acidic soil

Soil Research ◽  
2020 ◽  
Vol 58 (4) ◽  
pp. 411
Author(s):  
Jin-Hua Yuan ◽  
Sheng-Zhe E ◽  
Zong-Xian Che
Keyword(s):  
Soil Ph ◽  
Cation Exchange Capacity ◽  
Soil Amendment ◽  
Acid Soil ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Acidic Soil ◽  
Low Grade ◽  
Incubation Experiments ◽  
Acid Neutralisation

Mineral composition and alkaline properties of palygorskite (Pal), and its ameliorative effects on chemical properties of acid soil were investigated. Dolomite was the main form of alkali in Pal and the acid neutralisation capacity of Pal was 215 cmol kg–1. Incubation experiments indicated that Pal incorporation increased soil pH, cation exchange capacity, base saturation and exchangeable K+, Na+, Ca2+ and Mg2+ contents, and decreased the levels of exchangeable H+, Al3+ and acidity, over a 1-year period. The ameliorative mechanisms were the dissolution of major alkaline matter in Pal (i.e. dolomite), and the exchange between released Ca2+ and Mg2+ with H+ in acidic soil. Hence, Pal can be used as a moderate acidic soil amendment.

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