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1

Hamad, Asal Mahmud, and Mahmood Gazey Jassam. "A Comparative Study for the Effect of Some Petroleum Products on the Engineering Properties of Gypseous Soils." Tikrit Journal of Engineering Sciences 29, no. 3 (2022): 69. http://dx.doi.org/10.25130/tjes.29.3.7.

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Gypseous soils are considered problematic soils because the soil cavities happen during receiving the water or this type of soil and solving gypsum materials and contract in a soil volume. In this study, three types of gypseous soils are used; soil1, soil2, and soil3 with gypsum content (28.71%, 43.6%, and 54.88%) respectively, petroleum products (engine oil, fuel oil, and kerosene) are added to the soils with percentages (3%, 6%, 9%, and 12%) for each product. The result showed that specific gravity, liquid limit, optimum moisture content (O.M.C), and maximum dry density decreased with an inc
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Neethu, John, Nihal N. Mohamed, KS Niveditha, Das Renil, and Prakash J. Ridhick. "Alkali Interaction with Expansive and Non Expansive Soils." Applied Science and Engineering Journal for Advanced Research 4, no. 2 (2025): 8–14. https://doi.org/10.5281/zenodo.15107823.

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This research examines the interaction of alkali contaminants with both expansive and non-expansive soils, specifically black cotton soil and red soil, while assessing the effectiveness of sulphur and gypsum in restoring soil pH for geotechnical stability. Alkaline contamination, commonly caused by industrial effluents, construction activities, and agricultural practices, alters soil behavior by influencing its strength, swelling-shrinkage properties, and overall suitability for construction and infrastructure development. Laboratory experiments are conducted to evaluate the impact of alkalini
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Borůvka, L., M. Valla, H. Donátová, and K. Němeček. "Vulnerability of soil aggregates in relation to soil properties." Plant, Soil and Environment 48, No. 8 (2011): 329–34. http://dx.doi.org/10.17221/4376-pse.

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Stability of soil structure represents an indicator of soil quality. The aim of this paper was to assess the effect of soil properties on structure vulnerability in an Orthic Luvisol. The aggregates were most vulnerable to fast wetting (mean K<sub>v1</sub> = 9.99, i.e. this effect can decrease the aggregate size 9.99 times). Lower destruction was caused by slow wetting and drying (K<sub>v2</sub> = 3.70) and mechanical forces (K<sub>v3</sub> = 1.67). Fine silt (particles of 0.002–0.01 mm) was the most important soil charac
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Fattah, Mohammed A. Fattah, Shadan H. Khurshid Khurshid, and Rebaz A. Ahmad Ahmad. "Soil Cracking Depth as Influenced By Soil Physical Properties." Journal of Zankoy Sulaimani - Part A 2ndInt.Conf.AGR, Special Issue (2018): 105–14. http://dx.doi.org/10.17656/jzs.10657.

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Kodešová, R., M. Vlasáková, M. Fér, et al. "Thermal properties of representative soils of the Czech Republic." Soil and Water Research 8, No. 4 (2013): 141–50. http://dx.doi.org/10.17221/33/2013-swr.

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Knowledge of soil thermal properties is essential when assessing heat transport in soils. Thermal regime of soils is associated with many other soil processes (water evaporation and diffusion, plant transpiration, contaminants behaviour etc.). Knowledge of thermal properties is needed when assessing effectivity of energy gathering from soil profiles using horizontal ground heat exchangers, which is a topic of our research project. The study is focused on measuring of thermal properties (thermal conductivity and heat capacity) of representative soils of the Czech Republic. Measurements were per
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Vopravil, Jan, Pavel Formánek, and Tomáš Khel. "Comparison of the physical properties of soils belonging to different reference soil groups." Soil and Water Research 16, No. 1 (2020): 29–38. http://dx.doi.org/10.17221/31/2020-swr.

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Soil properties can be influenced by long-term agricultural management practices as described in pedological literature. In this study, selected physical properties (particle density and bulk density, total porosity, maximum capillary water capacity, minimum air capacity, field capacity, permanent wilting point and available water capacity) of topsoils from different reference soil groups (Cambisols, Luvisols, Fluvisols, Chernozems and Phaeozems, Leptosols, Stagnosols and Gleysols) were sampled and analysed in the years 2016–2017. The topsoil samples were taken from points of so-called S (spec
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7

Prajakta, Labade, Jagtap D.N., R. Sonawane Unnati, P.Thul Pooja., and B.L.Ayare. "Use Sentinel Satellite Data for Estimation of Soil Properties: A Review." International Journal of Environmental and Agriculture Research 10, no. 10 (2024): 139–51. https://doi.org/10.5281/zenodo.14016023.

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<strong><em>Abstract</em></strong><strong>&mdash;</strong> <em>Soils are an important component of the critical zone and a finite resource. Mapping and monitoring these resources in the field, regional, and global stages is crucial for better management and prevention of degradation.</em><em> </em><em>Remote sensing (RS) techniques provide several advantages over conventional approaches for evaluating soil parameters, including large-scale coverage, non-destructive nature, temporal monitoring, multispectral capabilities, and rapid data collecting.</em><em> </em><em>Aside from laboratory circum
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8

Ejikeme, CS, and IA Nweke. "Physical and Chemical Characterisation of Soils of Anambra State College of Agriculture, Mgbakwu." Greener Journal of Agricultural Sciences 6, no. 10 (2016): 326–30. https://doi.org/10.15580/GJAS.2016.10.102116189.

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The physical and chemical characterisation of Anambra State College of Agriculture at Mgbakwu, Awka North Local Government Area was conducted using composite samples from two representative profile pits. Six soil samples were collected from various depths, dried, sieved with 2 mm sieve and subjected to a routine soil analysis and the characteristics of the soils described. The findings from the study shows that the texture of the soils varied from loamy sand to sand clay loam, with the total sand ranging from 640 &ndash; 840 gkg<sup>-1</sup>, clay from 70 to 290 gkg<sup>-1</sup>&nbsp;and silt
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9

Kirilov, Ivaylo, Biser Hristov, and Pavel Pavlov. "Soils over Calcareous Rocks in Golo Burdo Mountain." Bulgarian Journal of Soil Science 6, no. 2 (2021): 146–56. https://doi.org/10.5281/zenodo.5767870.

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The paper deals with calcareous soils in Golo Bardo Mountain in western Bulgaria. Until now no significant studies have been made for the soils of Golo Bardo Mountain. Our goal was to give assess data for their soil features, characteristics, main diagnostic indicators and properties in order to define the soil formation processes, as well as their complete morphological description. Eight soil profiles were studied in different parts of the mountain. Due to the carbonate soil-forming rocks, the leaching processes in these soils are extremely weak and it is usually difficult to distinguish the
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10

Szara, Ewa, Tomasz Sosulski, and Magdalena Szymańska. "Soil phosphorus sorption properties in different fertilization systems." Plant, Soil and Environment 65, No. 2 (2019): 78–82. http://dx.doi.org/10.17221/696/2018-pse.

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The study aimed at the evaluation of the accumulation and vertical distribution of different forms of phosphorus (P) in reference to phosphorus sorption properties subject to mineral (NPK), mineral-organic (NPK + M), and organic (M) fertilisation. It was carried out in a long-term experimental field in Skierniewice (Central Poland) conducted since 1923 under rye monoculture. Total P content in the M and NPK soil profile was similar and lower than in the NPK + M soil. The content of organic P in A&lt;sub&gt;p&lt;/sub&gt; and E&lt;sub&gt;et&lt;/sub&gt; horizons of both manured soils was similar
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11

PK, Srivastava, M. Gupta, A. Pandey, V. Pandey, N. Singh, and Tewari SK. "Effects of sodicity induced changes in soil physical properties on paddy root growth." Plant, Soil and Environment 60, No. 4 (2014): 165–69. http://dx.doi.org/10.17221/926/2013-pse.

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A study was conducted to investigate the influence of sodicity induced changes in soil physical properties on paddy root growth in the normal agriculture, semi-reclaimed and sodic soils. The root growth (length, length density, biomass and distribution pattern) were unfavourably affected by the soil physical properties (bulk density, soil aggregate stability, available water content, hydraulic conductivity and soil water retention potential) in the case of sodic soil. The microbial biomass carbon, bacterial, fungal population and dehydrogenase activity showed the lower values in the case of so
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12

Komiljon Ogli, Nurullaev Azamkhon, and Djalilova Gulnora Tulkunovna. "EFFECT OF EROSION PROCESSES ON SOIL PROPERTIES." American Journal Of Agriculture And Horticulture Innovations 3, no. 12 (2023): 5–12. http://dx.doi.org/10.37547/ajahi/volume03issue12-02.

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Today, global climate change, along with drought, the processes of soil degradation are becoming one of the urgent problems for scientists all over the world. In this regard, a number of works are being carried out in Uzbekistan. According to the National Report on the State of Land Resources of the Republic of Uzbekistan, only 10% (4.3 million ha) of the 44.9 million hectares in the Republic are irrigated. About 2 million hectares (45%) of these lands are subject to secondary salinization. There are problems with water erosion on 800,000 hectares and wind erosion on 2 million hectares. The ob
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13

Zulkarnain. "Study of some Chemical Properties of Ultisols Soils Based on the Existence of Earth Worms." International Journal of Environmental & Agriculture Research 8, no. 7 (2022): 01–04. https://doi.org/10.5281/zenodo.6944794.

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<strong><em>Abstract</em>&mdash;</strong><em>The purpose of the study was to determine some of the chemical properties of the soil on Ultisols inhabited and uninhabited by earthworm populations.</em> <em>The research was carried out from April to June 2019, taking soil samples on mixed garden land in the Bukit Pinang Urban Village, Samarinda and soil analysis at the Soil Science Laboratory, Faculty of Agriculture, Mulawarman University, Samarinda, East Kalimantan Province.</em> <em>The research activities are: field observations, determining the location of soil sampling, soil sampling, collec
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14

Kholopov, Yu V., D. D. Khaydapova, A. B. Novakovsky, and E. M. Lapteva. "Rheological Properties of Boreal Semihydromorphic Soils: Relationship with Physico-Chemical Properties and Temperature Conditions." Počvovedenie, no. 6 (December 19, 2024): 813–30. https://doi.org/10.31857/s0032180x24060036.

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The results of rheological studies of soils on the modular rheometer MCR 302 (Anton Paar, Austria) by the amplitude sweep method (oscillatory method) are considered. Study objects are represented by semi-hydromorphic soils of taiga zone in the Northeast of European part of Russia. We found that the strongest interactions between soil particles are developed in the horizons with high content of mobile humus compounds (fulvic acids) and Al/Fe-humus complexes (ELhi,g–ELg–CRM horizons). Increased structural durability is due to the cementation of soil particles resulting from the intake of humus s
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15

Weber, Jerzy, Peter Leinweber, Yakov Kuzyakov, et al. "Soil management effects on soil organic matter properties and carbon sequestration (SOMPACS)." ARPHA Conference Abstracts 6 (October 17, 2023): e108213. https://doi.org/10.3897/aca.6.e108213.

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SOMPACS is a project recommended by EJP SOIL for funding under the 1st External Call "Towards Healthy, Resilient and Sustainable Agricultural Soils". The goal of this project is to assess management practices that enrich organic matter pools that are resilient to rapid microbial decomposition. The project started in 2022 as a consortium of 12 research institutions from Poland, Germany, Ireland, Lithuania, UK, Italy and USA for a period of three years.Soil and vegetation samples from eight long-term experiments that differ in soil management practices (i.e., conventional vs. no-tillage; mineral
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Savich, Vitaliy, Vladimir Sedykh, and Nikolay Minaev. "Information assessment of the interrelationships of soil properties, processes and regimes." АгроЭкоИнфо 6, no. 54 (2022): 42. http://dx.doi.org/10.51419/202126642.

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The interrelationships of soil properties, processes and regimes occurring in them characterize the genesis, agroecological state and fertility of soils. The use of organic and mineral fertilizers changes the properties of soils and the relationship between soil properties. The effect of the introduction of siderates and NPK into the soil on the enzymatic and microbiological activity of soils is shown. Data on changes in the fractional composition of iron in different horizons of podzolic soil are presented. It is proved that the relationship between soil properties is one of the factors deter
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17

Zádorová, T., O. Jakšík, R. Kodešová, and V. Penížek. " Influence of terrain attributes and soil properties on soil aggregate stability." Soil and Water Research 6, No. 3 (2011): 111–19. http://dx.doi.org/10.17221/15/2011-swr.

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&amp;nbsp; The study on the relationship between the soil aggregates stability assessed using water stable aggregate (WSA) index and the selected terrain and soil properties was performed on a morphologically diverse study site in Chernozem soil region of Southern Moravia. Soil analyses and detailed digital elevation model processing were the main methods adopted in the study. The soil structure stability is negatively influenced by the soil material removal from the steep parts of the back-slope and re-deposition of the mineral loess material at the base of the slope. The highest aggregates s
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18

K., I. OFEM, F. EDIENE V., KINGSLEY JOHN, and U. AKPAN-IDIOK A. "SPATIAL VARIABILITY OF SOIL PROPERTIES IN YAKURR LOCAL GOVERNMENT AREA, SOUTHEAST NIGERIA." Asian Journal of Plant and Soil Sciences 2, no. 1 (2017): 6–16. https://doi.org/10.5281/zenodo.1407329.

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The status and spatial variability of soil properties across agrarian communities in Yakurr Local Government Area, Southeast Nigeria were assessed and soil management strategies suggested for limiting soil properties. Nine communities were identified within the study area and soil samples collected from young fallow lands measuring 40 m by 40 m at depths of 0 &ndash; 20 cm and 20 &ndash; 40 cm to represent surface and subsurface soils respectively. The interpolation of the area was done using the deterministic methods of inverse distance weighting (IDW) in ArcGIS 10.2.2 software. The soils wer
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19

Petr, Šařec, and Novák Petr. "Changes in soil properties due to the application of activators in conditions of very heavy soils." Research in Agricultural Engineering 63, Special Issue (2017): S40—S45. http://dx.doi.org/10.17221/39/2017-rae.

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This paper deals with verification of the effect of fermented manure (with and without Z'fix activators) and soil activators (PRP Sol) on a soil properties change. Their application should lead to a change in physical, physical-chemical and biological properties of soil, along with ecological material fixation, improved water retention and infiltration, reduction of soil susceptibility to water erosion and decreased soil tillage energy requirements. Field trial was established in Sloveč in Central Bohemia in the year 2014. The experiment was divided into several variants and was designed as mu
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20

Shubham, SIngh, Swami Sanjay, Gogoi Jyotim, et al. "Effect of biochar-mediated treatments on the enhancement of soil acidity, crop performance and soil properties." Agricultural Mechanization in Asia, Africa and Latin America 54, no. 4 (2023): 13575–603. https://doi.org/10.5281/zenodo.8157837.

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Biochar, a carbon-rich material derived from biomass pyrolysis, has gained considerable attention as a soil amendment for improving soil fertility and crop productivity. One of the key benefits of biochar is its ability to mediate soil acidity, influencing soil pH and buffering capacity. Biochar can act as a liming agent, raising soil pH in acidic soils, or as an acidifying agent, lowering pH in alkaline soils, through its alkaline or acidic functional groups, respectively. This property makes biochar a versatile tool for managing soil acidity in different agricultural systems. The application
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21

Lynn, Tin Mar, Ei Phyu Kyaw, San San Yu, et al. "Investigation on the variations of soil properties of different agricultural soils in central Myanmar." Journal of Scientific and Innovative Research 11, no. 1 (2022): 1–7. http://dx.doi.org/10.31254/jsir.2022.11101.

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Soil properties are varied under human disturbance and understanding how the soil properties change is vital to know the potential of soils and their sensitivity to different soil managements. The aim of this study was to analyze the variation in soil physicochemical characters as influenced by different soil managements (orchards, crop rotation, and intensive use of fertilizer), in central dry zone in Myanmar. Eight soil properties such as soil texture, pH, electrical conductivity (EC), organic matter (OM), total nitrogen, available phosphate (Olsen P), extractable potassium (extractable K),
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22

Hussein Razzaq Nayyef. "Effect of continuous cultivation and soil texture on some soil properties." GSC Advanced Research and Reviews 13, no. 1 (2022): 077–84. http://dx.doi.org/10.30574/gscarr.2022.13.1.0271.

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The effects of soil continuous cultivation and soil texture on some of its properties, electrical conductivity, total porosity, and calcium carbonate content and soil penetration resistance. Six samples of soil material for a layer of 0-30 cm were collected from three different texture sites are Clay, Loam and Loamy Sand in Basra Governorate for three sites Abi al-Khasib, Karma and Zubair. Three of these samples represented the treatment of soil continuous cultivation, soil planted with alfalfa crop (Medicago sativa) for 7 consecutive years, and the other three samples from the same sites for
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Ilinkin, Vladimir, Simeon Bogdanov, and Antonia Goleva. "Characteristics of Rendzinas in the Ludogorie Region." Bulgarian Journal of Soil Science 2, no. 1 (2017): 32–41. https://doi.org/10.5281/zenodo.2585635.

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The paper presents results from an investigation on soils located in the Ludogorie region. Rendzinas (Rendzic Leptosols, FAO, 2006) have been studied. They are situated in the Lower forest vegetation zone (0&ndash;600 m a.s.l.) of the Moesian forest vegetation area. Soil samples have been taken from seven soil profiles. The study covers an area of 3000 m2 . The factors of soil formation have been characterized. Soil physical and chemical properties have been investigated. The results have been processed by a statistical programme. The arithmetic means (M) and standard deviations (&plusmn;SD) h
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Hussein, Razzaq Nayyef. "Effect of continuous cultivation and soil texture on some soil properties." GSC Advanced Research and Reviews 13, no. 1 (2022): 077–84. https://doi.org/10.5281/zenodo.7664723.

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The effects of soil continuous cultivation and soil texture on some of its properties, electrical conductivity, total porosity, and calcium carbonate content and soil penetration resistance. Six samples of soil material for a layer of 0-30 cm were collected from three different texture sites are Clay, Loam and Loamy Sand in Basra Governorate for three sites Abi al-Khasib, Karma and Zubair. Three of these samples represented the treatment of soil continuous cultivation, soil planted with alfalfa crop (Medicago sativa) for 7 consecutive years, and the other three samples from the same sites for
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H.A., Rayimberdiev, Eshonkulov M.A., Kholboev B., Raxmonov I., and Mirsharipova G. "Mechanical composition and properties of irrigated soils of syrdarya region." American Journal Of Agriculture And Horticulture Innovations 5, no. 3 (2025): 9–13. https://doi.org/10.37547/ajahi/volume05issue03-03.

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The article presents the main soil types in the region and their distribution by mechanical composition. It also presents methods for determining the mechanical composition of the region's soils and the results of the analysis of the mechanical composition of the soil by fractionation
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Gelybó, G., E. Tóth, C. Farkas, Á. Horel, I. Kása, and Z. Bakacsi. "Potential impacts of climate change on soil properties." Agrokémia és Talajtan 67, no. 1 (2018): 121–41. http://dx.doi.org/10.1556/0088.2018.67.1.9.

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Climate change is expected to have a vigorous impact on soils and ecosystems due to elevated temperature and changes in precipitation (amount and frequency), thereby altering biogeochemical and hydrological cycles. Several phenomena associated with climate change and anthropogenic activity affect soils indirectly via ecosystem functioning (such as higher atmospheric CO2 concentration and N deposition). Continuous interactions between climate and soils determine the transformation and transport processes. Long-term gradual changes in abiotic environmental factors alter naturally occurring soil
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Turdimetov, Shakhobiddin M., and Mokhinur M. Musurmanova. "PROPERTIES OF SOILS LOCATED IN DIFFERENT GEOMORPHOLOGICAL CONDITIONS." American Journal Of Agriculture And Horticulture Innovations 02, no. 11 (2022): 1–6. http://dx.doi.org/10.37547/ajahi/volume02issue11-01.

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Soil properties can vary to some extent depending on the geomorphological conditions in which they are located. This is due to the diversity of parent rocks, layering and mechanical composition of the soil. The article presents and compares the properties of irrigated gray-meadow, meadow and marsh-meadow soils located on terraces I, II, III of the Syrdarya River. Based on the results obtained, recommendations are given for the rational placement of plants.
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Cobo, Vidal Yakelin, Baró Elio Angarica, Gutiérrez George Martín, Gutierrez Adrián Serrano, Gómez Juan Alejandro Villazón, and Fajardo Alegna Rodríguez. "Chemical Properties that Determine Boron Availability in Sugar Cane Soils." Agrisost 25, no. 2 (2019): 1–5. https://doi.org/10.5281/zenodo.10014788.

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<strong>Context:&nbsp;</strong>Several factors are limiting the behavior and dynamics of boron (B) in the soil. Few results on assimilable B contents in the soil and its relation to other chemical properties have been published.<strong>Objective:</strong> To determine the contents of assimilable B and the chemical properties that condition its availability in three of the main soil types where sugar cane is cultivated.<strong>Methods:</strong> The samples were taken at random from the surface (0-20 cm) of three of the main soil types where sugar cane is cultivated in Cuba. Soil assimilable B w
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Poyon Kizi, Khayitova Sanobar. "SOIL SCIENCE AND SOIL TERMINOLOGY." European International Journal of Multidisciplinary Research and Management Studies 02, no. 11 (2022): 42–44. http://dx.doi.org/10.55640/eijmrms-02-11-12.

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Soil science involves the study of the formation and distribution of soil, the biological, chemical and physical properties and processes of soil and how these processes interact with wider systems to help inform environmental management, industry and sustainable development.
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Ilinkin, Vladimir, Peter Zhelev, and Dimitar Dimitrov. "Statistical Assessment of Fluvisols in "Gladino" Gravel Quarry, Chelopechene, Bulgaria." Bulgarian Journal of Soil Science 2, no. 2 (2017): 133–47. https://doi.org/10.5281/zenodo.2586011.

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The paper presents results of an investigation on Fluvisols. The soils are located in &ldquo;Gladino&rdquo; gravel quarry, Chepintsy district, Bulgaria, on an area of 1.043 km2 . Soil samples were taken from fifteen soil profiles at a depth of 0-100 cm. The factors of soil formation were characterized and it`s physicochemical properties were studied. The changes in physicochemical properties were investigated at different soil depths and the relationships between different soil characteristics were tested by correlation analysis. The results reveal that some soil characteristics, such as the c
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Dashko, Regina, and Anna Shidlovskaya. "Impact of microbial activity on soil properties." Canadian Geotechnical Journal 53, no. 9 (2016): 1386–97. http://dx.doi.org/10.1139/cgj-2015-0649.

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There are microorganisms in soils and their activity can have a positive or negative impact on soil properties and groundwater. The positive effect of microorganisms includes the self-purification and self-regulation of contaminated groundwater and soil. The negative effect on soil is the change in grain-size composition; the weakening of engineering properties of soils; and the development processes, such as biogas generation, microbial quick-sand formation, and soil liquefaction. This paper addresses the negative effects of microbial activity on soil. Research on the impact of microbial acti
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Merdun, Hasan, and Virgil L. Quisenberry. "Relating model parameters to basic soil properties." Soil Research 42, no. 7 (2004): 841. http://dx.doi.org/10.1071/sr03098.

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Relating model parameters to basic soil characteristics can help to differentiate and classify soils based on their flow and transport characteristics and ultimately helps to develop a sound management tool to protect groundwater from industrial and agricultural contaminants. In this study, the model parameters (effective diffusion path-length or aggregate half-width, boundary soil water pressure, boundary hydraulic conductivity, saturated hydraulic conductivity, tortuosity in macropores, dispersivity, mixing depth) obtained from simulation of water flow and solute transport for 3 soils (Maury
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Khudoyarovna, Hayitalieva Madina, Musurmanov Alisher Amirkulovich, and Muratkasimov Alisher Sattorovich. "General Physical Properties of Rain-Soaked Soils (On the Example of Zaaminsky District)." European International Journal of Multidisciplinary Research and Management Studies 5, no. 4 (2025): 44–46. https://doi.org/10.55640/eijmrms-05-04-09.

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The article analyzes the general physical properties of rain-soaked soils of the Zaaminsky district. In conditions of climatic changes on rich soils, and always planting the same type of crop leads to a change in soil properties. The general physical properties of soils are of great importance for determining soil fertility, moisture consumption, mobility, and nutrient absorption. In the upper layer of undeveloped typical gray-earth soils, the density is 1.30-1.32 g/cm3, in the lower layers 1.38-1.40 g/cm3, compacting from top to bottom. On the southern slope of the rain-fed soils, it can be s
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Al-Yasir, Abdullah Talib, and Abbas Jawad Al-Taie. "Geotechnical Review for Gypseous Soils: Properties and Stabilization." Jurnal Kejuruteraan 34, no. 5 (2022): 785–99. http://dx.doi.org/10.17576/jkukm-2022-34(5)-04.

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In many arid and semi-arid regions, collapsible soils are well-known to be problematic in nature and negatively affect the performance of engineering structures. Gypseous soil considers one of the well-known types of collapsible soil. It represents a real challenge to engineers due to different problems encountered by engineering projects implemented in this soil. The mineralogy, composition, and fabric of gypseous soil affect its ability to deform when subjected to wetting (due to changing the whole structure soil particles). Numerous studies considered the problems of gypseous soils and thei
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35

Asmar, Asmar, Amrizal Saidi, and Masliyunas Masliyunas. "HUBUNGAN KESUBURAN TANAH DENGAN PRODUKTIVITAS TANAMAN." Jurnal Solum 7, no. 1 (2010): 27. http://dx.doi.org/10.25077/js.7.1.27-36.2010.

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A research about relationship between soil properties and crop yield was conducted in Pandai Sikek, Tanah Datar Region, center for cabbage and carrot production, West Sumatra in 2004 and 2005. Soil samples were collected from rainfed paddy soils by purposive random sampling. Soil samples were analyzed in Soil Laboratory, Agriculture Faculty and Agriculture Polytechnique Laboratory, Andalas University. Several soil physical properties analysed were soil bulk density and total soil pores by using gravimetric method, permeability with de Boodt method, soil water content at several pF values using
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36

Brmež, Mirjana, Josipa Puškarić, Tamara Siber, Emilija Raspudić, Dinka Grubišić, and Brigita Popović. "Influence of liquid chicken manure preparation on soil health and agrochemical soil properties." Poljoprivreda 24, no. 1 (2018): 3–9. http://dx.doi.org/10.18047/poljo.24.1.1.

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37

Sayad, E., S. M. Hosseini, V. Hosseini, and M. H. Salehe-Shooshtari. "Soil macrofauna in relation to soil and leaf litter properties in tree plantations." Journal of Forest Science 58, No. 4 (2012): 170–80. http://dx.doi.org/10.17221/58/2011-jfs.

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Soil communities exert strong influences on the processing of organic matter and nutrients. Plantations of trees, especially of nitrogen fixing ones, may affect the soil macrofauna through litter quality and quantity. This study was conducted in a randomized block design with three blocks consisting of Populus euphratica, Eucalyptus camaldulensis, Eucalyptus microtheca, Acacia farnesiana, Acacia salicina, Acacia saligna, Acacia stenophylla and Dalbergia sissoo monoculture plantations that were established in 1992. Soils and soil macrofauna were sampled in November 2006. Leaf litterfall was col
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38

Fahmi, Arifin, Ani Susilawati, and Ahmad Rachman. "Influence of Height Waterlogging on Soil Physical Properties of Potential and Actual Acid Sulphate Soils." JOURNAL OF TROPICAL SOILS 19, no. 2 (2015): 67. http://dx.doi.org/10.5400/jts.2014.v19i2.67-73.

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Water management is main factor that determines the successful of rice cultivation in acid sulphate soil. Soil waterlogging determines the direction and rate of chemical, geochemical and biological reaction in the soil, indirectly these reactions may influence to the changes of soil psycal properties during soil waterlogging process. The experiment was aimed to study the changes of two type of acid sulphate soils physical properties during rice straw decomposition processes. The research was conducted in the greenhouse consisting of the three treatment factors using the completely randomized d
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39

Gannon, Travis W., Adam C. Hixson, Kyle E. Keller, Jerome B. Weber, Stevan Z. Knezevic, and Fred H. Yelverton. "Soil Properties Influence Saflufenacil Phytotoxicity." Weed Science 62, no. 4 (2014): 657–63. http://dx.doi.org/10.1614/ws-d-13-00171.1.

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Saflufenacil, a pyrimidinedione herbicide, is used for contact and residual broadleaf weed control in various crops. Bioactivity of saflufenacil in soil was tested in greenhouse and laboratory studies on 29 soils representing a wide range of soil properties and geographic areas across the United States. A greenhouse bioassay method was developed using various concentrations of saflufenacil applied PPI to each soil. Whole canola plants were harvested 14 d after treatment, and fresh and dry weights were recorded. Nonlinear regression analysis was used to determine the effective saflufenacil dose
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40

Ngole-Jeme, Veronica M. "Fire-Induced Changes in Soil and Implications on Soil Sorption Capacity and Remediation Methods." Applied Sciences 9, no. 17 (2019): 3447. http://dx.doi.org/10.3390/app9173447.

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Vegetation changes caused by fire events are visible instantly but changes in soils are less apparent, and could be short-term, long-term or permanent in nature. Research has shown that soils undergo changes in their mineralogical, geochemical, physico-chemical and biological properties after a fire event that may vary depending on the intensity and duration of the fire, and the properties of the soil. Some of these properties make significant contributions towards soil’s ability to sorb contaminants. Changes in these properties could affect soil sorption complex and the effectiveness of remed
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41

Tkachenko, A. N., M. N. Kozachuk, and O. V. Tkachenko. "Morphological properties of underwater soils of river deltas." Dokuchaev Soil Bulletin, no. 99 (December 9, 2019): 62–75. http://dx.doi.org/10.19047/0136-1694-2019-99-62-75.

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The results of the study of the morphological properties of underwater soils in the deltas of the Volga, Don and Kuban rivers are shown. This paper is based on field descriptions of profiles of underwater soils found in deltas. Genetic horizons have been identified, their basic properties (pH, Eh, electrical conductivity, grain size composition, organic carbon content) have been studied and the main types of soils, which are formed under different types of sedimentation and under different types of aquatic vegetation, have been described. Names of horizons and types of soils are given due to t
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42

Behrens, T., K. Gregor, and W. Diepenbrock. "Separation of soil and canopy reflectance signatures of Mid German agricultural soils." Plant, Soil and Environment 51, No, 7 (2011): 296–303. http://dx.doi.org/10.17221/3589-pse.

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Remote sensing can provide visual indications of crop growth during production season. In past, spectral optical estimations were well performed in the ability to be correlated with crop and soil properties but were not consistent within the whole production season. To better quantify vegetation properties gathered via remote sensing, models of soil reflectance under changing moisture conditions are needed. Signatures of reflected radiation were acquired for several Mid German agricultural soils in laboratory and field experiments. Results were evaluated at near-infrared spectral region at the
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43

Maheswari, Anusuri Uma. "Improving Soil Properties by Using Coir." International Journal for Research in Applied Science and Engineering Technology 9, no. VIII (2021): 80–86. http://dx.doi.org/10.22214/ijraset.2021.37280.

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Construction on these soils is found to be expensive because of their low bearing strength. Soil having poor bearing need stabilization to make it suitable for construction purpose. In this study coir (extracted from coconut) is used as natural fiber for stabilization of soil. Stabilization using natural fiber is a cost-effective and eco-friendly approach to improve properties of soil. The study is carried out to evaluate the effects of coir fiber on properties of soil. Coconut coir in the soil were varied from 0, 0.5, 1.0, 1.5, and 2.0% and various soil properties were studied.
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Romanova, Tatyana, Aliaksandr Chervan, and Nadezhda Ivakhnenko. "The essence of soil and soil formation in accordance with soil water regime." Journal of Geography and Cartography 7, no. 2 (2024): 6271. http://dx.doi.org/10.24294/jgc.v7i2.6271.

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The obtaining of new data on the transformation of parent materials into soil and on soil as a set of essential properties is provided on the basis of previously conducted fundamental studies of soils formed on loess-like loams in Belarus (15,000 numerical indicators). The study objects are autochthonous soils of uniform granulometric texture. The basic properties without which soils cannot exist are comprehensively considered. Interpolation of factual materials is given, highlighting the essential properties of soils. Soil formation is analyzed as a natural phenomenon depending on the life ac
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45

Watkar, Amita M. "Physico-Chemical Properties of Soil Collected from Chandrabhaga River in Kalmeshwar, Nagpur, Maharashtra." Journal of Advanced Research in Alternative Energy, Environment and Ecology 07, no. 02 (2020): 1–3. http://dx.doi.org/10.24321/2455.3093.202006.

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Soil, itself means Soul of Infinite Life. Soil is the naturally occurring unconsolidated or loose covering on the earth’s surface. Physical properties depend upon the amount, size, shape, arrangement, and mineral composition of soil particles. It also depends on the organic matter content and pore spaces. Chemical properties depend on the Inorganic and organic matter present in the soil. Soils are the essential components of the environment and foundation resources for nearly all types of land use, besides being the most important component of sustainable agriculture. Therefore, assessment of
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Edet, J. A., C. N. Tom, I. E. Ahaneku, U. J. Etoamaihe, C. U. Orji, and Eunice N. Gam. "Response Surface Modelling of The Physicochemical Properties and Hydraulic Conductivity Prediction Using Selected Properties of Soil in Abia State, Nigeria." Contemporary Research Analysis Journal 05, no. 05 (2025): 268–77. https://doi.org/10.5281/zenodo.15393892.

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Understanding the dynamic interplay between soil physicochemical properties and water transmission behavior is crucial in enhancing agricultural productivity, resource efficiency, and environmental sustainability. In line with this, the present research focuses on the response surface modeling (RSM) of the physicochemical properties and hydraulic conductivity (K) of soils in Abia State, Nigeria, spanning the three senatorial districts: Abia North, Abia Central, and Abia South. The study is situated within the broader framework of Agricultural Bioresources Engineering, a field concerned with op
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Okorie, A., and C. Njoku. "Comparative Assessment of Selected Chemical Properties of Soils in Ivo, Ohaozara and Onicha L.G.As of Ebonyi State, Nigeria." Greener Journal of Agricultural Sciences 3, no. 2 (2013): 097–100. https://doi.org/10.15580/GJAS.2013.2.111512263.

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<strong>This study was carried out at Ivo, Ohaozara and Onicha L.G.As. to compare selected chemical properties of soils in those areas.&nbsp; Four replicates of soil samples were collected in each L.G.A. at depths of 0 to 30 cm using soil auger. These soil samples were used for the determination of soil texture, soil pH, organic C, total N, C/N ratio, available P, exchangeable K and cation exchange capacity. Data collected were analysed using standard error and coefficient of variance. Results of the study showed that the soils of the three L.G.As were sandy loam. The pH of soils studied were
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Lapuag, Ryan Carlo. "Electrical Properties of Soil in Bohol: Basis for Automated Irrigation System." Psychology and Education: A Multidisciplinary Journal 25, no. 6 (2024): 756–66. https://doi.org/10.5281/zenodo.13825120.

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Irrigation is vital for Philippine agriculture, particularly in regions like Bohol, where water resources are under pressure due to competing demands and seasonal droughts. Despite introducing automated irrigation technologies designed to enhance efficiency, many areas still need to rely on updated manual methods, leading to water wastage and reduced productivity. This study explores the potential of automated irrigation systems to improve water use efficiency by evaluating soil's physical and electrical properties in Bohol's greenhouses. Specifically, it investigates soil texture, bulk densit
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Laktionova, T., V. Medvedev, K. Savchenko, O. Bigun, S. Nakis’ko, and S. Sheyko. "“Ukrainian soil properties” database and its application." Agricultural Science and Practice 2, no. 3 (2015): 3–8. http://dx.doi.org/10.15407/agrisp2.03.003.

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The structure and the main characteristics of the multi-purpose soil database “Ukrainian Soil Properties”, de- signed on the basis of the data of long-term soil studies comprisin, analysis of the samples and mapping of the soils are presented. The attributive data for the 2,075 soil profiles are ranked and grouped into nine separate thematic tables. The key field of each table is the indexing number for the soil profile. It ensures a genuine link between the profile sets of attributive data and the cartographic units on the soil maps in the different scales, on the map chart of economic and ag
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50

Ross, PJ, and BJ Bridge. "Thermal properties of swelling clay soils." Soil Research 25, no. 1 (1987): 29. http://dx.doi.org/10.1071/sr9870029.

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The thermal properties of swelling clay soils do not appear to have been previously studied, even though they should be different from those of non-swelling soils because of changes in pore size and structure with water content. We measured the thermal diffusivity of small discs cut from cores of a highly swelling black earth (Pellustert) using the pulse method, common in materials science but not previously applied to soils. Thermal conductivity was calculated from thermal diffusivity and heat capacity per unit volume. The behaviour of these thermal properties was indeed different from those
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