scholarly journals Soil-Landscape Relationship in the Northern Volcanic Mountain of Leyte, Philippines

2017 ◽  
pp. 87-104
Author(s):  
Roland Rallos ◽  
Victor Asio ◽  
Faustino Villamayor
Keyword(s):  
Sustainable Management ◽  
Crop Production ◽  
Chemical Properties ◽  
Parent Material ◽  
Landscape Position ◽  
Soil Landscape ◽  
Physical And Chemical ◽  
The Relationship ◽  
Unstable Position ◽  
And Chemical Properties

Studies on soil-landscape relationships are necessary to improve our understanding of the spatial distribution and variation of soils for their sustainable management. This study evaluated the relationship between soil properties and landscape position in the northern volcanic mountain of Leyte, Philippines. Five soil profiles located on summit, shoulder, backslope and footslope positions were evaluated. Findings revealed that the degree of soil development as well as the soil morphophysical and chemical properties varied with landscape position. The soil in the most stable position (summit) had thicker solum and slightly more developed soil profile than the soils in other landscape positions. On the other hand, soils in the unstable position (backslope) generally had thinner solum. All the five soils also revealed the influence of the andesitic volcanic parent material on their properties. They all showed some properties typical of Andisols such as low bulk density and high pH in NaF although they were classified as Andic Dystrudept. The soils all possessed physical and chemical constraints for crop production.

scholarly journals Impact of Bush Burning on Chemical Properties of Some Soil in Igboora, Oyo State, Nigeria

2021 ◽  
Vol 7 (2) ◽  
Author(s):  
M. A. Adejumobi
Keyword(s):  
Crop Production ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Rooting Depth ◽  
Physical And Chemical Properties ◽  
Land Clearing ◽  
Two Samples ◽  
Burnt Soil ◽  
Physical And Chemical ◽  
And Chemical Properties

Soil is used in agriculture as an anchor and primary nutrient base for plants, and the types of soil and available moisture determine the species of plants that can be cultivated. Bush burning, whether as result of a wildfire or a controlled burning, affects not only the appearance of the landscape, but the quality of the soil. Bush burning method of land clearing is a traditional farming system used as a means of land clearing for crop production. This method of land clearing has both beneficial and detrimental effects on soil physical and chemical properties. Therefore, this study investigated the effects of bush burning on soil chemical properties at different soil depth of 0-30 cm and 30-60 cm respectively base on the rooting depth of crop planted. The experiment was carried out in six selected farms in Igboora, Ibarapa central Local Governmental, Oyo State. The soil sampled were collected from burnt and unburnt experimental soil and analyzed using USDA standard methods for soil analysis for the selected chemical characteristics (pH, Ca2+, Mg2+ Na+. TN and P). Two samples were taken from each burnt and un-burnt locations at depth of 0-30 and 30-60 cm. Paired t-test was used to compare means value of soil chemical properties determined from burnt and un-burnt soil. ANOVA was used for significance difference between soil from burnt and un-burnt soil. pH increased from moderately acidic to slightly acidic, phosphorus content of the soil increased greatly from un-burnt soil to burnt soil at 0-30 cm and 30-60 cm depths from 6.64 to 22.21 ppm and 3.53 to 24.95 ppm, respectively. Similarly, potassium increased from 0.27 to 0.40ppm at 0-30cm depth but decreased from 0.23 to 0.17 ppm at 30-60 cm depth. Nitrogen reduced at both depths from 0.80 to 0.76% and 0.72 to 0.68% respectively. Magnesium also increased from 1.3 cmol/kg to 2.00 cmol/kg and 1.65 to 1.75 cmol/kg at both 0-30 cm and 30-60 cm depth respectively. Whereas calcium showed a reduction from 3.17 to 2.85 cmol/kg and 1.65 to 1.45 cmol/kg at both depths. The variations observed between burnt and un-burnt soil for Ca, Mg, exchangeable acidity, pH, Nitrogen, potassium was significant at p<0.05 probability level. This indicates that bush burning has an impact on soil physical and chemical properties which may affect the suitability of the soil for crop production. Based on this, there is need for environmental education for farmers in the area in order to know the implications of bush burning on soil properties for soil sustainability which will boost food production.

Pronamide Phytotoxicity in Ten Wisconsin Soils

Weed Science ◽  
1980 ◽  
Vol 28 (4) ◽  
pp. 429-432 ◽  
Author(s):  
T. E. Dutt ◽  
R. G. Harvey
Keyword(s):  
Organic Matter ◽  
Chemical Properties ◽  
Clay Content ◽  
Exchange Capacity ◽  
Fresh Weight ◽  
Relationship Of ◽  
Physical And Chemical ◽  
Mg Content ◽  
The Relationship ◽  
And Chemical Properties

Pronamide [3,5-dichloro-(N-1, 1-dimethyl-2-propynyl) benzamide] phytotoxicity was compared in 10 Wisconsin soils and the relationship of activity to soil physical and chemical properties appraised. Twelve soil properties were measured and correlated with pronamide I50(50% fresh weight inhibition) values using oats (Avena sativaL. ‘Portal’) as the indicator plant in bioassays conducted under greenhouse conditions. Organic matter was the soil variable most inversely correlated with pronamide phytotoxicity. Cation exchange capacity, field moisture capacity, and Mg content were also inversely correlated with pronamide phytotoxicity, but probably reflect changes in soil organic matter levels. Clay content did not significantly affect pronamide phytotoxicity.

A soil toposequence on bunya phyllite in Brisbane

Soil Research ◽  
1981 ◽  
Vol 19 (1) ◽  
pp. 1
Author(s):  
AJ Koppi
Keyword(s):  
Chemical Properties ◽  
Parent Material ◽  
Physical And Chemical Properties ◽  
Genetic Unit ◽  
Dioctahedral Mica ◽  
Physical And Chemical ◽  
In Situ Weathering ◽  
And Chemical Properties

A common toposequence on Bunya Phyllite in south-east Queensland was studied in detail at a representative site. Four sample profiles on the slope are described, and some physical and chemical properties are given. The clay minerals, derived from the weathering of the quartz-sericite-chlorite phyllite, comprise dioctahedral mica, dioctahedral vermiculite, an interstratification of these minerals, and kaolin. Properties are related to the slope; and the clay-rich horizon of the middle and lower slopes is considered to be formed mostly by in situ weathering. The classification of the genetic unit given by the slope and parent material is discussed.

PHOTO-OXIDATION OF CRUDE OILS

1977 ◽  
Vol 1977 (1) ◽  
pp. 617-620 ◽  
Author(s):  
Shinichi Nagata ◽  
Goro Kondo
Keyword(s):  
Chemical Properties ◽  
Physical And Chemical Properties ◽  
Photo Oxidation ◽  
Elapsed Time ◽  
Boiling Points ◽  
Ca 50 ◽  
Physical And Chemical ◽  
The Relationship ◽  
Photo Decomposition ◽  
And Chemical Properties

ABSTRACT Changes with elapsed time are presented for five kinds of oils that were studied through the analyses of GLC method, where particularly we made an attempt to examine the relationship among specific gravity, viscosity, and the amount of water in oils. Furthermore, we tried to evaluate a few processes of various kinds of changes on the physical and chemical properties of oils such as evaporation, biodegradation, and photo-decomposition. The evaporation process was found to affect mainly paraffins with smaller boiling points, below the number of C12-C13, for 21 days, while due to the action of marine bacteria, normal paraffins were effectively degraded (ca. 50%) after 15 days except for branched ones. Moreover, it was also found that the aromatic hydrocarbons with anthracene ring and heteroaromatic ones, which were not easily decomposed by the processes mentioned above, were fairly decomposed by photo-irradiation for 10 hours.

Effect of Basicity on Continuous Casting Mold Flux Properties

2012 ◽  
Vol 567 ◽  
pp. 62-65 ◽  
Author(s):  
Xin Hua Zhu ◽  
Li Guang Zhu ◽  
Yu Liu ◽  
Peng Fei Wang
Keyword(s):  
Continuous Casting ◽  
Mold Flux ◽  
Chemical Properties ◽  
Physical And Chemical Properties ◽  
Continuous Casting Mold ◽  
Casting Mold ◽  
Flux Function ◽  
Physical And Chemical ◽  
The Relationship ◽  
And Chemical Properties

Basicity is an important parameter which can determine the performance of continuous casting fluxes, and it have different effects on flux of various physical and chemical properties. This paper discusses the relationship and impact between basicity and the physical and chemical properties of flux, Which proved how changes of basicity affect physical and chemical properties of flux, and then how it affects the flux function .

scholarly journals Pemberian Kirinyuh (Cromolaena odorata L.) sebagai Mulsa Organik pada Tanaman Kedelai (Glycine max L.) serta Pengaruhnya terhadap Sifat Fisika dan Kimia Tanah

2020 ◽  
Vol 3 (2) ◽  
pp. 43-50
Author(s):  
Nasrullah Nasrullah ◽  
Syakur Syakur ◽  
Hasanuddin Hasanuddin
Keyword(s):  
Organic Matter ◽  
Bulk Density ◽  
Crop Production ◽  
Chemical Properties ◽  
Physical And Chemical Properties ◽  
Organic Mulch ◽  
Ground Support ◽  
Glycine Max L ◽  
Physical And Chemical ◽  
And Chemical Properties

Abstrak :Gulma kirinyuh sangat berpotensi untuk dijadikan pupuk organik karena kandungan unsur  hara dalam jaringannya yang tinggi. Biomassa kirinyuh memiliki kandungan hara N 2,65%, P 0,53% dan K 1,9% sehingga dapat dimanfaatkan sebagai sumber hara yang potensial dalam upaya peningkatan produksi kedelai dan perbaikan kesuburan tanah. Penelitian ini bertujuan untuk mengetahui tanah yang sesuai dalam menunjang produksi tanaman kedelai akibat dari penambahan bahan organik kirinyuh. Penelitian ini bertujuan untuk mengetahui tanah yang sesuai dalam menunjang produksi tanaman kedelai akibat dari penambahan bahan organik kirinyuh. Penelitian ini dilakukan dengan menggunakan Rancangan Acak Kelompok (RAK) Faktorial yang terdiri atas 2 (dua) faktor dengan pola 4 x 3 sehingga diperoleh 12 kombinasi perlakuan. Faktor pertama adalah dosis mulsa organik kirinyuh (D), terdiri atas 4 (empat) taraf yaitu: D0 = 0 ton ha-1, D1 = 6 ton ha-1, D2 = 12 ton ha-1, D3 = 18 ton ha-1. Faktor kedua adalah waktu aplikasi mulsa organik kirinyuh (W) terdiri atas 3 (tiga) taraf yaitu saat tanam (W1), 1 minggu setelah tanam (W2), 2 minggu setelah tanam (W3). Peubah fisika dan kimia tanah yang diamati meliputi bulk density, stabilitas agregat tanah, kapasitas tukar kation dan kejenuhan basa.Hasil penelitian menunjukkan bahwa dosis mulsa organik kirinyuh berpengaruh sangat nyata  terhadap sifat fisika tanah yaitu bulk density. Dosis mulsa organik kirinyuh 6 - 18 ton ha-1 menurunkan nilai bulk density namun tidak meningkatkan stabilitas agregat tanah. Waktu aplikasi mulsa organik kirinyuh yang awal tidak menunjukkan pengaruhnya terhadap sifat fisika dan kimia tanah yang diamati. Tidak terdapat interaksi antara dosis dan waktu aplikasi mulsa organik kirinyuh terhadap semua peubah yang diamati.   Granting Kirinyuh (Cromolaena odorata L.) As Organic Mulch In Soybean Plants (Glycine max L.) As Well As Its Effects On The Physical And Chemical Properties Of SoilAbstract. Weed kirinyuh potential to be used as organic fertilizer because the content of nutrient elements in its high. Biomass kirinyuh contain nutrient N 2.65%, 0.53% P and K 1.9% so that it can be utilized as a source of potential nutrient in an attempt to increase the production of soybean and improvement of soil fertility. This research aims to know the appropriate ground support the soybean crop production resulting from the addition of organic matter kirinyuh. This research aims to know the appropriate ground support the soybean crop production resulting from the addition of organic matter kirinyuh. This research was performed using Random Design Group (RAK) Factorial of 2 (two) factors with the 4 x 3 pattern so obtained 12 combination treatment. The first factor is a dose of organic mulch kirinyuh (D), consisting of four (4) levels, namely: a D0 = 0 ton ha-1, D1 = 6 ton ha-1, D2 = 12 ton ha-1, D3 = 18 ton ha-1. The second factor is the time of organic mulch application kirinyuh (W) consists of 3 (three) level that is when planting (W1), 2 weeks after planting (W2), 2 weeks after planting (W3). Soil physical and chemical variables were observed include bulk density, soil aggregate stability, cation exchange capacity and saturation of the base. The results showed that a dose of organic mulch kirinyuh very real effect against soil physical properties namely bulk density. A dose of organic mulch kirinyuh 6-18 ton ha-1 lowers the values of bulk density but does not increase the stability of soil aggregates. Organic mulch application time kirinyuh the beginning does not show its effects on the physical and chemical properties of the soil is observed. There is no interaction between the dose and time of application of organic mulch kirinyuh against all variables were observed. 

Communication of integrated dielectric permitivity and NMR–characteristics of oil with its physical and chemical properties

2020 ◽  
Author(s):  
Andrey A. Mezin ◽  
◽  
Mariya Y. Shumskayte ◽  
Olga V. Rodionova ◽  
Aleksandra I. Buruhina ◽  
...  
Keyword(s):  
Group Composition ◽  
Experimental Studies ◽  
Chemical Properties ◽  
Complex Dielectric Constant ◽  
Physical And Chemical Properties ◽  
Nmr Parameters ◽  
Dielectric Permitivity ◽  
Physical And Chemical ◽  
The Relationship ◽  
And Chemical Properties

The paper presents the results of experimental studies on the dielectric and NMR characteristics of oil samples. The relationship between the complex dielectric constant and the NMR parameters of oil with its density, viscosity and group composition has been established. It was found that the results of these methods directly depend on the content of resinous–asphaltenic compounds in the composition of the studied oil sample.

scholarly journals Variability of morphological, physical and chemical properties of soils derived from carbonate-rich parent material in the Pieniny Mountains (south Poland)

2017 ◽  
Vol 68 (1) ◽  
pp. 27-38 ◽  
Author(s):  
Joanna Kowalska ◽  
Bartłomiej Kajdas ◽  
Tomasz Zaleski
Keyword(s):  
Chemical Properties ◽  
Parent Material ◽  
Rock Material ◽  
Base Saturation ◽  
Soil Profiles ◽  
Physical And Chemical Properties ◽  
Calcite Veins ◽  
High Base ◽  
Physical And Chemical ◽  
And Chemical Properties

Abstract Carbonate-rich soils are characterized by great diversity in content of carbonate and non-carbonate mineral substances in soil substrate which largely influences soil properties. The study presents the analysis results of four soil profiles located at the area of Pieniny National Park. The aim of this study was to characterize and classify the soils developed from the mixture of carbonate and carbonate-rich rock material, formerly classified as pararendzinas. It was achieved by determination of morphological, physical, and chemical properties, as well as mineralogical composition of selected carbonate-rich soils occurring in the Polish part of the Pieniny Mts. Soils were classified as typical chernozemic rendzina (P1), typical eutrophic brown soils (P2, P4), as well as typical pararendzina (P3) according to Polish Soil Classification (2011). The parent material of studied soils P1, P2 and P4 were slope covers, with a dominant share of sandstone and minor share of limestone, whereas soil P3 was formed from variegated shale cut with multiple calcite veins. Soils were characterized by stable aggregate structure: crumby, angular blocky and subangular blocky. They were medium or strong skeletal, mostly with loam texture with great share of silt fraction. CaCO3 content in genetic horizons ranged from 0.0 to 703.0 g·kg-1. The reaction of studied soils was from weakly acidic to alkaline. Analysed soils were characterized by very high base saturation. Among determined exchangeable cations, Ca2+ ions had the biggest share in all analysed profile. High base saturation, as well as high content of calcium carbonate was accompanied by content of organic matter and percentage content of clay fraction. Taking into consideration determined chemical and physical properties, it can be found that investigated soils were influenced by not only the in-situ weathering material but also by rock material which have been transported and deposited as a result of slope processes. Furthermore, the lack or lower content of CaCO3 in surface and middle part of analysed soil profiles was most likely a result of the impoverishment of rock material during the transport on the slope.

Properties and mineralogy of topsoil in the town of Longyearbyen (Spitsbergen, Norway)

Polar Record ◽  
2019 ◽  
Vol 55 (2) ◽  
pp. 102-114
Author(s):  
Wojciech Szymański ◽  
Janusz Siwek ◽  
Michał Skiba ◽  
Bronisław Wojtuń ◽  
Aleksandra Samecka-Cymerman ◽  
...  
Keyword(s):  
Trace Elements ◽  
Urban Soils ◽  
Chemical Properties ◽  
Parent Material ◽  
Physical And Chemical Properties ◽  
Natural Properties ◽  
Local Parent ◽  
Physical And Chemical ◽  
The Town ◽  
And Chemical Properties

AbstractSoil is one of the most important constituents of an ecosystem, playing a crucial role in many environmental reactions and processes. Despite the fact that many environmental studies were conducted in the vicinity of Longyearbyen, very little is known about the physical and chemical properties as well as mineralogy of soils occurring in this town. Thus, the main aims of this study were: (1) to determine the texture, chemical properties and mineralogy of the topsoil horizons of urban soils occurring in the Longyearbyen area (Spitsbergen, Norway); and (2) to determine and explain their spatial distribution within the area of Longyearbyen. In general, the topsoils are characterised by loamy texture; acidic reaction; quite high content of total organic carbon (TOC); high content of Si, Al and Fe; and low content of K, Na, Ca, Mg and P. Quartz, K-feldspar, plagioclase, mica and chlorite are the prevailing minerals. Differences in the concentration of TOC, total nitrogen and elements in the topsoils are mainly related to the diversity of texture and mineralogy of the local parent material and the development of vegetation cover. The results indicate that topsoils in Longyearbyen are characterised by the natural properties and are not strongly transformed by human activity. However, pollution of soil with trace elements related to coal mining should be checked.

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