scholarly journals KARAKTERISASI DAN KLASIFIKASI TANAH ULTISOL DI KECAMATAN INDRAJAYA KABUPATEN PIDIE

2018 ◽  
Vol 14 (2) ◽  
pp. 52-59
Author(s):  
Sri Handayani ◽  
Karnilawati Karnilawati
Keyword(s):  
Cation Exchange Capacity ◽  
Field Survey ◽  
Secondary Data ◽  
Exchange Capacity ◽  
Soil Sampling ◽  
Soil Reaction ◽  
Organic P ◽  
Climate Data ◽  
Weight Value

This study aims to examine the characteristics of Ultisol soil and produce a system of naming Ultisol soil according to the USDA Land Taxonomy system in Indrajaya District, Pidie District. This research will be carried out in the villages of Gle Gapui, Tuha Suwiek and Masjid Suwiek Indrajaya sub-districts from June to November 2015. This study uses descriptive-quantitative method, which consists of the following stages: (1) Preparation, ie collecting secondary data such as climate data, maps etc. Then prepare the tools and materials for the field survey and establish the ground pedon (2) Field activities, including observation of soil profile, soil sampling, laboratory analysis. Subsequently classified the land based on the USDA Land Taxonomy System Profile Gle Gapui climber determinant (horate Bt) textured clay where there is increasing clay so it is included into the horizontal horizon. Content weight value is inversely proportional to permeability and porosity. The soil reaction is directly proportional to the saturation of base which is equally low. The content of C- organic, P is available and N total is low. Moderate Cation Exchange Capacity, exchangeable acids (H and Al) are high. The classification of Ultisol soil in the location of the Glealing Glean profile is Typic Hapludult, berliat, blend, isohipertermik.

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 Chemical characters of disease suppressive and conducive soil of Moler on shallot in Brebes Central Java

2021 ◽  
Vol 905 (1) ◽  
pp. 012057
Author(s):  
S H Poromarto ◽  
Supyani ◽  
Supriyadi ◽  
Hadiwiyono
Keyword(s):  
Cation Exchange Capacity ◽  
Exchange Capacity ◽  
Organic P ◽  
Suppressive Soil ◽  
Central Java ◽  
Organic Mineral ◽  
Chemical Soil ◽  
Chemical Character ◽  
Chemical Characters ◽  
Conducive Soil

Abstract In the latest years, a disease epidemy of Moler caused by Fusarium oxysporum f.sp. cepae have just occurred in Brebes Central Java. The disease intensity, however, varies between the shallot production lands. Some lands show suppressive with disease intensity lower than 5%, and others are conducive to disease intensity over 50%. It is interesting that in Brebes occur suppressive and conducive soil to moler disease. The suppressiveness may be determined by environmental conditions, including chemical soil characters. This paper reports the chemical character of suppressive and conducive soil to moler disease in Brebes. The evidence shows that the suppressive soil is more fertile than that conducive one. The suppressive soil is chemically characterized by significantly higher organic mineral, C-organic, P-available, K-exchangeable, and Cation Exchange Capacity than that conducive one.

PROPERTIES AND CLASSIFICATION OF FTVE SOILS ON ALLUVIAL LANDFORMS IN CENTRAL NIGERIA

1987 ◽  
Vol 67 (2) ◽  
pp. 249-261 ◽  
Author(s):  
T. A. OKUSAMI ◽  
R. H. RUST ◽  
A. S. R. JUO
Keyword(s):  
Particle Size ◽  
Organic Carbon ◽  
Particle Size Distribution ◽  
Cation Exchange Capacity ◽  
Clay Mineralogy ◽  
Exchange Capacity ◽  
Carbon Distribution ◽  
Parent Materials ◽  
River Niger

Five soils formed in alluvium in central Nigeria are described, characterized and classified. One soil is on the present floodplain of the River Benue, while the others are on terraces of both the River Niger and the River Benue and their tributaries. Soils have a preponderance of mottles, sesquioxidic nodules and/or concretions and grayer colors of low chromas. Particle size distribution on a clay-free basis was used in addition to morphology and organic carbon distribution to determine the homogeneity of parent materials. The soil on the floodplain and two others on terraces are all formed in two different parent materials. Two other soils on terraces are formed in homogeneous parent materials. Most soils have a generally low effective cation exchange capacity, but higher values are found in neutral to moderately alkaline profiles containing smectite. The clay fractions are a mixture of kaolinite, smectite and some hydrous mica. Two soils are classified as Ustifluvents. The others are Tropaquepts, Plinthaquults and Argiaquolls. Equivalent FAO/UNESCO classifications are Dystric Fluvisols, Dystric Gleysols, Eutric Planosols, Plinthic Gleysols and Mollic Gleysols. Key words: Alluvium, hydromorphic, Nigeria, mixed clay mineralogy, classification

scholarly journals Influence of a planting hole application of dolomitic limestone powder and basalt grit on the growth of Carpathian birch (Betula carpatica W. et K.) and soil chemistry in the air-polluted Jizerské hory Mts.

2008 ◽  
Vol 53 (No. 11) ◽  
pp. 505-515 ◽  
Author(s):  
I. Kuneš ◽  
V. Balcar ◽  
D. Zahradník
Keyword(s):  
Cation Exchange ◽  
Soil Chemistry ◽  
Cation Exchange Capacity ◽  
Exchange Capacity ◽  
Base Saturation ◽  
Soil Reaction ◽  
Dolomitic Limestone ◽  
Soil N ◽  
Exchangeable Bases ◽  
Exchangeable P

The objective of the study was to evaluate the growth potential of Carpathian birch (<I>Betula carpatica</I> W. et K.) at an environmentally harsh mountain site and a response of this species to altered soil chemistry after dolomitic limestone and basalt grit applications. The Carpathian birch proved to be a suitable species for the replanting of extreme acidic mountain sites. This birch shows a low mortality rate, grows well in the clear-felled patches and soon forms a cover which is necessary for the reintroducing of more sensitive tree species. The application of dolomitic limestone and basalt grit resulted in the slower growth of Carpathian birch plantations. Liming raised soil reaction, sum of exchangeable bases, base saturation, cation exchange capacity and reduced exchangeable Al content. On the other hand, liming decreased an amount of oxidizable soil organic matter and negatively affected soil N, exchangeable P and K. Basalt grit increased exchangeable P and K contents and raised soil reaction, however only slightly. The influence of basalt grit on the sum of exchangeable bases, base saturation and cation exchange capacity was also less pronounced compared to liming. Basalt grit elevated the proportion of exchangeable aluminium and reduced the content of soil N.

scholarly journals The place of the Zheltozem-Gley Soils of Azerbaijan in the International System WRB

2020 ◽  
Vol 3 (1) ◽  
Author(s):  
Maharram P. Babayev ◽  
Amin I. Ismayilov ◽  
Sultan M. Huseynova
Keyword(s):  
Cation Exchange ◽  
Cation Exchange Capacity ◽  
Field Experiments ◽  
Exchange Capacity ◽  
Soil Samples ◽  
International Classification ◽  
Current Status ◽  
Soil Resources ◽  
Reference Base

The aim of the study. The aim of the research was obtaining new information about the genesis, current status, diagnostic features and properties of the Zheltozem-Gley Soils of the Lankaran region of Azerbaijan and to perform the taxonomic attribution of those soils in accordance with the International Classification of Soils in compliance with the Reference Base for soil resources (IUSS Working Group WRB, 2014). Location and time of the study. Zheltozem-Gley Soils of the Lankaran region of Azerbaijan were the objects of the study. Methodology. Field experiments (relief, vegetation, laying of soil profiles, their description, selection of soil samples and establishment of a preliminary classification name of the soils) and physico-chemical analyzes of soil samples (humus and total nitrogen content, ratio of C:N in soil organic matter, soil pH, cation exchange capacity, grain-size analysis, water extract composition) were carried out by standard methods. Results. It was established that the most characteristic features of the irrigated zheltozem-gley soils were as following: blocky angular-subangular structure of the upper horizon, clayiness of the entire soil profile, the presence of iron-manganese concretions and ferruginous mottles. A gradual decrease in the content of humus (from 2.15-3.28 to 0.18-1.24%), nitrogen (from 0.17-0.24 to 0.05-0.24%), the ratio of C:N (from 6.64-7.18 to 1.89-5.91) was found. The cation exchange capacity increased down the profile (from 33.37-37.13 to 34.31-40.89 cmol (eq)/kg). The reaction of the soil environment was weakly acidic, and varied within 5.8-6.0. Under the influence of irrigation, the removal of the silt fraction from the upper horizons and its accumulation in the middle horizons of the soil were observed (42-96 cm – 42.4%, 48-87 cm – 28.8%). According to the granulometric composition, these soils were medium-light-heavy loamy. The soils were not saline. Conclusion. For the first time, an attempt was made to carry out the taxonomic attribution of Zheltozem-Gley soils (irrigated Zheltozem-Gley merged, ordinary Zheltozem-Gleyic, irrigated Zheltozem-Gley, irrigated residual calcareous Zheltozem-Gley) according to the international classification of soils based on the Reference Base for soil resources (WRB). With the different principal and supplementary qualifiers, all soils were classified as Lixisols.

scholarly journals Analisis Kesesuaian Lahan untuk Padi di Distrik Semangga, Kabupaten Merauke

2017 ◽  
Vol 1 (1) ◽  
pp. 87
Author(s):  
ARDIANSYAH ARDIANSYAH ◽  
SIDHARTA SAHIRMAN ◽  
M. RIF'AN ◽  
EDY H.P. MELMAMBESSY
Keyword(s):  
Cation Exchange Capacity ◽  
Drainage System ◽  
Nutrient Content ◽  
Exchange Capacity ◽  
Land Suitability ◽  
Limiting Factor ◽  
Overlay Analysis ◽  
Climate Data ◽  
Optimal Production ◽  
Land Preparation

This study aimed to determine the land suitability for paddy plantation in Semangga subdistrict, Merauke Regency, Papua Province and to identify any treatments that needs to be taken to promote the land suitability classes. The information on land suitability is important to determine the treatment required in land preparation in order to achieve optimal production. Survey was conducted to collect necessary data which includes climate data, nutrient content (N, P, K available), Cation Exchange Capacity (CEC), pH, and toxicity. These data are interpolated within the area of Semangga subdistrict and classified based on the criteria developed by Indonesian Soil Research Institute - Ministry of Agriculture and FAO. Overlay analysis is performed in order to determine land suitability classes and the dominant limiting factor. Criteria for determining the suitability classes was taken from the lowest class of land unit. The results showed that the area of 1% (360.09 hectare) is classified as class of S2wfn, 55.8% (19,495.83 hectare) as class of S3n, 7% (2,431.83 hectare) as class of S3np, 35.3% (12,349.74 hectare) as class N1n, and 0.9% (306.6 hectare) as class of N2f. The finding of land suitability classes and its dominant inhibitory factor can be used then to determine the proper land treatment planning such as fertilization, liming, and drainage system design.

scholarly journals KESESUAIAN LAHAN TANAMAN JAGUNG DI KABUPATEN MINAHASA SELATAN

EUGENIA ◽  
2007 ◽  
Vol 13 (3) ◽  
Author(s):  
J. E.X. Rogi ◽  
Johan A. Rombang ◽  
Josephus I. Kalangi ◽  
Malsupri Taher
Keyword(s):  
Cation Exchange ◽  
Air Temperature ◽  
Spatial Data ◽  
Cation Exchange Capacity ◽  
Geographic Information ◽  
Exchange Capacity ◽  
Climate Data ◽  
The South ◽  
Suitability Map ◽  
Suitable Area

ABSTRACT   Rogi, J.E.X. et. al. 2007. The Suistability Land for Corn in the South Minahasa District. Eugenia 13 (3) : 320-326. Based on agri-climate and market prospective, corn is a potential comodity in the South-Minahasa District. From 215.000 ha of South-Minahasa District area, it has 18.437 ha harvest-area and in 2006 produced 52.747 tonnes corn. The above data showed that this district has a possibility to extend the corn planting area in suitable area. To find this suistability area for corn, a spatial data was composed based on soil and climate data using Geographic Information Systemm (GIS). Soil data consisted of texture, pH, C-organic, and cation exchange capacity (CEC), whereas climate data consisted of rainfall and air temperature. Spatial data in the form of land suitability map for corn in the South-Minahasa District was analysed using ArcViewer 3.2. software.   Keywords: Harvest area, soil and climate, spatial data, GIS, ArcViewer 3.2

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