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1

Yang, X. M., C. F. Drury, W. D. Reynolds, and D. C. MacTavish. "Use of sonication to determine the size distributions of soil particles and organic matter." Canadian Journal of Soil Science 89, no. 4 (2009): 413–19. http://dx.doi.org/10.4141/cjss08063.

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Applying ultrasound energy to soil-water suspensions (sonication) is an established method of determining the size distributions of soil primary mineral particles and associated organic matter. The size distributions may vary, however, with sonication input energy and soil type. The objective of this study was to determine the effects of sonication input energy on the size distributions of soil mineral particles and organic matter for a range of soil textures and carbon contents typical of agricultural soils in southwestern Ontario. The soils included a Brookston clay loam, a Brookston clay, a
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2

BACCHI, O. O. S., K. REICHARDT, and N. A. VILLA NOVA. "FRACTAL SCALING OF PARTICLE AND PORE SIZE DISTRIBUTIONS AND ITS RELATION TO SOIL HYDRAULIC CONDUCTIVITY." Scientia Agricola 53, no. 2-3 (1996): 356. http://dx.doi.org/10.1590/s0103-90161996000200027.

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Fractal scaling has been applied to soils, both for void and solid phases, as an approach to characterize the porous arrangement, attempting to relate particle-size distribution to soil water retention and soil water dynamic properties. One important point of such an analysis is the assumption that the void space geometry of soils reflects its solid phase geometry, taking into account that soil pores are lined by the full range of particles, and that their fractal dimension, which expresses their tortuosity, could be evaluated by the fractal scaling of particle-size distribution. Other authors
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3

Towner, G. D. "The influence of particle size distribution on soil physical properties." Journal of Agricultural Science 106, no. 3 (1986): 527–35. http://dx.doi.org/10.1017/s0021859600063413.

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SummaryBatcombe series soils readily break down to good tilths, Beccles series soils form cloddy seed beds that are resistant to weathering, and Stackyard series soils form unstable tilths that readily break down. The soils differ in their particle-size distribution. The proposition that such differences contributed to the differences in field behaviour was examined by forming artificial soils, each of which was made up from particles of one of the soils, but redistributed with respect to size in the proportion in which they occurred in one of the other soils.As a measure of the relevant physi
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4

Gong, Cang, Yang Shao, Min Luo, Diandou Xu, and Lingling Ma. "Distribution Characteristics of Heavy Metals in Different Particle Size Fractions of Chinese Paddy Soil Aggregates." Processes 11, no. 7 (2023): 1873. http://dx.doi.org/10.3390/pr11071873.

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In recent years, the migration and transformation of heavy metals (HMs) in soil has become a hot issue. Soil particle size has an important effect on the environmental behavior of HMs in soil. The distribution of HMs in soil is strongly affected by the size of a soil aggregate. In this study, paddy samples in both cultivated and uncultivated soils were collected from Anhui Province, China. The soils were sieved into six particle size fractions (diameters of >4000, 4000–2000, 2000–1000, 1000–250, 250–53, and <53 μm) and the wet digestion method was used to determine the concentrations of
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5

Afrazi, Mohammad, and Mahmoud Yazdani. "Determination of the Effect of Soil Particle Size Distribution on the Shear Behavior of Sand." Journal of Advanced Engineering and Computation 5, no. 2 (2021): 125. http://dx.doi.org/10.25073/jaec.202152.331.

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Many geotechnical problems require the determination of soil engineering properties such as shear strength. Therefore, the determination of the reliable values for this parameter is essential. For this purpose, the direct shear test, as one of the oldest tests to examine the shear strength of soils, is the most common way in laboratories to determine the shear parameters of soil. There are far too many variables that influence the results of a direct shear test. In this paper, a series of 10 × 10 cm direct shear tests were carried out on four different poorly graded sands with different partic
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6

Li, Shijin, Adrian R. Russell, and David Muir Wood. "Influence of particle-size distribution homogeneity on shearing of soils subjected to internal erosion." Canadian Geotechnical Journal 57, no. 11 (2020): 1684–94. http://dx.doi.org/10.1139/cgj-2019-0273.

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Internal erosion (suffusion) is caused by water seeping through the matrix of coarse soil and progressively transporting out fine particles. The mechanical strength and stress–strain behavior of soils within water-retaining structures may be affected by internal erosion. Some researchers have set out to conduct triaxial erosion tests to study the mechanical consequences of erosion. Prior to conducting a triaxial test they subject a soil sample, which has an initially homogeneous particle-size distribution and density throughout, to erosion by causing water to enter one end of a sample and wash
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7

Tong, Chen-Xi, Glen J. Burton, Sheng Zhang, and Daichao Sheng. "A simple particle-size distribution model for granular materials." Canadian Geotechnical Journal 55, no. 2 (2018): 246–57. http://dx.doi.org/10.1139/cgj-2017-0098.

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Particle-size distribution (PSD) is a fundamental soil property that plays an important role in soil classification and soil hydromechanical behaviour. A continuous mathematical model representing the PSD curve facilitates the quantification of particle breakage, which often takes place when granular soils are compressed or sheared. This paper proposes a simple and continuous PSD model for granular soils involving particle breakage. The model has two parameters and is able to represent different types of continuous PSD curves. It is found that one model parameter is closely related to the coef
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8

Bagarello, Vincenzo, Vito Ferro, and Giuseppe Giordano. "ESTIMATING SOIL PARTICLE-SIZE DISTRIBUTION FOR SICILIAN SOILS." Journal of Agricultural Engineering 40, no. 3 (2009): 33. http://dx.doi.org/10.4081/jae.2009.3.33.

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The soil particle-size distribution (PSD) is commonly used for soil classification and for estimating soil behavior. An accurate mathematical representation of the PSD is required to estimate soil hydraulic properties and to compare texture measurements from different classification systems. The objective of this study was to evaluate the ability of the Haverkamp and Parlange (HP) and Fredlund et al. (F) PSD models to fit 243 measured PSDs from a wide range of 38 005_Bagarello(547)_33 18-11-2009 11:55 Pagina 38 soil textures in Sicily and to test the effect of the number of measured particle d
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9

Abakumov, E. V. "Particle-size distribution in soils of West Antarctica." Eurasian Soil Science 43, no. 3 (2010): 297–304. http://dx.doi.org/10.1134/s1064229310030075.

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10

Radzii, Volodymyr. "Modern methods of grain size distribution of soils." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 302–8. http://dx.doi.org/10.30970/vgg.2013.44.1236.

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Grain size distribution of soil determines much of water and physical properties of the soil mass. However, it defines ecological functions and morphological memory of soils in the study of their genesis, evolution and use. This article describes the main methods of particle size analysis and suggests the modern methods used increasingly in the research in soil science, geology, chemical, pharmaceutical and other industries. Key words: particle size distribution of soil, sedimentograph, laser diffraction.
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11

Luo, Sha, Erdin Ibraim, and Andrea Diambra. "AE Signature Interpretation of Single Particle Crushing under Uniaxial Compression." E3S Web of Conferences 92 (2019): 09005. http://dx.doi.org/10.1051/e3sconf/20199209005.

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Granular soils exhibit particle crushing under certain loading circumstances, and it significantly affects their mechanical behaviour. However, the estimation of the particle crushing is extremely challenging. Therefore, new a technic based on passive non-destructive Acoustic Emission (AE) monitoring is explored to infer the extent and evolution of soil's particle size distribution. However, in this paper only individual particles under uniaxial compression are studied and the results should inform the interpretation of the laboratory tests on small scale soil samples. Different material types
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12

de Jesus Duarte, Sara, Bruno Glaser, and Carlos Pellegrino Cerri. "Effect of Biochar Particle Size on Physical, Hydrological and Chemical Properties of Loamy and Sandy Tropical Soils." Agronomy 9, no. 4 (2019): 165. http://dx.doi.org/10.3390/agronomy9040165.

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The application of biochar is promising for improving the physical, chemical and hydrological properties of soil. However, there are few studies regarding the influence of biochar particle size. This study was conducted to evaluate the effect of biochar size on the physical, chemical and hydrological properties in sandy and loamy tropical soils. For this purpose, an incubation experiment was conducted in the laboratory with eight treatments (control (only soil), two soils (loamy and sandy soil), and three biochar sizes (<0.15 mm; 0.15–2 mm and >2 mm)). Analyses of water content, bulk den
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13

Kim, Donggeun, Jisu Song, and Jaesung Park. "Quantifying Soil Particle Settlement Characteristics through Machine Vision Analysis Utilizing an RGB Camera." Agriculture 13, no. 9 (2023): 1674. http://dx.doi.org/10.3390/agriculture13091674.

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Soil particle size distribution is a crucial factor in determining soil properties and classifying soil types. Traditional methods, such as hydrometer tests, have limitations in terms of time required, labor, and operator dependency. In this paper, we propose a novel approach to quantify soil particle size analysis using machine vision analysis with an RGB camera. The method aims to overcome the limitations of traditional techniques by providing an efficient and automated analysis of fine-grained soils. It utilizes a digital camera to capture the settling properties of soil particles, eliminat
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14

Papuga, Krzysztof, Jarosław Kaszubkiewicz, Dorota Kawałko, and Maria Kreimeyer. "Effect of Organic Matter Removal by Hydrogen Peroxide on the Determination of Soil Particle Size Distribution Using the Dynamometer Method." Agriculture 12, no. 2 (2022): 226. http://dx.doi.org/10.3390/agriculture12020226.

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The dynamometer method of determining particle size distribution was developed several years ago. The principles of sample preparation for this method are based on those used in other sedimentation methods. With improvements in these procedures, an investigation of the effect on obtained particle size distribution results by removing organic matter using hydrogen peroxide was proposed. For this purpose, the particle size distributions were determined in 50 soil samples with varying organic matter content, before and after organic matter removal. A comparative analysis of the results, including
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15

Wu, Q., M. Borkovec, and H. Sticher. "On Particle-Size Distributions in Soils." Soil Science Society of America Journal 57, no. 4 (1993): 883–90. http://dx.doi.org/10.2136/sssaj1993.03615995005700040001x.

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16

Beemer, Ryan D., Alexandre Bandini-Maeder, Jeremy Shaw, and Mark J. Cassidy. "Volumetric Particle Size Distribution and Variable Granular Density Soils." Geotechnical Testing Journal 43, no. 2 (2019): 20180286. http://dx.doi.org/10.1520/gtj20180286.

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17

Wanogho, S., G. Gettinby, and B. Caddy. "Particle size distribution analysis of soils using laser diffraction." Forensic Science International 33, no. 2 (1987): 117–28. http://dx.doi.org/10.1016/0379-0738(87)90147-2.

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18

MIHAILOVIĆ, ALEKSANDRA, SAVKA ADAMOVIĆ, JORDANA NINKOV, et al. "Bimodal distribution of potentially toxic elements in urban soils: the impact of particle size." Romanian Reports in Physics 76, no. 2 (2025): 702. https://doi.org/10.59277/romrepphys.2025.77.702.

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The aim of the study was to ascertain the distribution of potentially toxic elements (PTEs) across different soil particle sizes, particularly on Fluvisol soil type in Novi Sad, Serbia, characterised by a significant proportion of sand as coarser particles. PTEs, such as As, Co, Cr, Cu, Mn, Ni, and Pb were analysed in urban soil near major roads. Bulk samples of urban soil were collected and subsequently subdivided into seven different particle size fractions using the wet sieving technique. Based on PTE concentrations and PTE mass loadings, the research confirmed a bimodal binding of PTEs acc
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19

Sa, S. H., T. Masuda, and Y. Hosoi. "A study of SS size distribution during runoff and fractionation of phosphates depending on soil size in agricultural watershed." Water Science and Technology 51, no. 3-4 (2005): 393–400. http://dx.doi.org/10.2166/wst.2005.0614.

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Characterization of the differences and algal-available fractions of P in soils, suspended solids, and bottom sediments have been the main topics of research during the past decade. However, the size distribution and properties of particulate matter in runoff have not been much studied in Japan. Here we study particle size distribution during runoff and the chemical characteristics of P in each soil size fraction and relate them to land use. The temporal variation of particulate sizes during rain events is different in each watershed. Most particles have the size in the range of 10∼100 μm. Als
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20

Golodnaya, Olga M., and Elena A. Zharikova. "Particle-Size Distribution in Soils of the Khankaiskiy Nature Reserve (Primorye Territory)." UNIVERSITY NEWS. NORTH-CAUCASIAN REGION. NATURAL SCIENCES SERIES, no. 2 (210) (June 28, 2021): 99–105. http://dx.doi.org/10.18522/1026-2237-2021-2-99-105.

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Soil texture is determined and the features of particle-size vertical distribution in soils of different landscapes of the Khankaiskiy Nature Reserve are considered. Three variants of the distribution of clay (<0.001 mm) and physical clay (<0.01 mm) fractions along the vertical profiles soils are identified: accumulative, regressive, with a maximum in the middle-profile horizon and with their approximately equal contents in the upper and the lower horizons. A regressive variant is revealed in burozems gleyic, podzoliс-brownzems, dark-humus gley and alluvial meadow gley soils. The
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21

Gorączko, Aleksandra, and Szymon Topoliński. "Particle Size Distribution of Natural Clayey Soils: A Discussion on the Use of Laser Diffraction Analysis (LDA)." Geosciences 10, no. 2 (2020): 55. http://dx.doi.org/10.3390/geosciences10020055.

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Particle size distribution is one of the most significant factors determining physical soil properties. Laser diffraction analysis (LDA) is an alternative method to the traditional hydrometric methods (HM) used to determine particle size distribution in soils. However, significant differences in fraction content are found in relation to the applied methods of a particle size test. Above all, measurements performed by LDA for clayey soils usually produce different results to those based on Stokes’ equation. Methodical problems, such as an appropriate method of dispersing the sample and the sele
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22

Wang, Mingqiang, Pan Chen, Panpan Yi, and Tiantian Ma. "Effect of Fines Content on Pore Distribution of Sand/Clay Composite Soil." Sustainability 15, no. 12 (2023): 9216. http://dx.doi.org/10.3390/su15129216.

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Plant sand fixation is the most durable and environmentally friendly sand mitigation measure for windblown sand hazards. For aeolian–sand composite soil, the fines content is the main factor affecting the pore size distribution characteristics and determines the soil water retention characteristics. Sandy soil with uniform particle size was used as the material, low-plasticity clay as a fine particle, and composite soils with different fines content were prepared. The evolution of the pore size distribution of composite soils was quantitatively determined using low-field nuclear magnetic reson
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23

Исаев, А. В., Ю. П. Демаков та Р. Н. Шарафутдинов. "Закономерности изменения гранулометрического состава аллювиальных почв в процессе развития пойм рек". Vestnik of Volga State University of Technology Series Forest. Ecology. Nature Management, № 2(54) (9 листопада 2022): 80–93. https://doi.org/10.25686/2306-2827.2022.2.80.

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Введение. Гранулометрический состав является одной из важнейших базовых характеристик почвы, во многом определяя их, в том числе и концентрацию в них химических элементов. Его изучение необходимо для выявления закономерностей эволюции аллювиальных почв, а также объяснения причин формирования геохимических аномалий. Цель исследования – оценить характер изменения гранулометрического состава аллювиальных почв в ходе развития поймы реки Большая Кокшага. Объекты и методы. Изучение гранулометрического состава аллювиальных почв проведено на 33 временных пробных площадях на участках поймы с различными
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Li, Shijin, and Adrian R. Russell. "A sample formation procedure to obtain homogeneous post-erosion particle size distribution." E3S Web of Conferences 92 (2019): 02015. http://dx.doi.org/10.1051/e3sconf/20199202015.

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Internal erosion (suffusion) is caused by water seeping through the matrix of coarse soil and progressively transporting out fine particles. The mechanical strength of soils within water retaining structures may be affected after internal erosion occurs. However, most experimental investigations on the mechanical consequences of internal erosion have used triaxial tests on samples having nonhomogeneous particle size distributions along their lengths. Such nonhomogeneities arise from the most commonly used sample formation procedure, in which seeping water enters one end of a sample and washes
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25

Kurniawan, R., T. Nghia-Nguyen, and M. Kikumoto. "Mechanical behavior of porous crushable soils: effect of intragranular porosity." IOP Conference Series: Earth and Environmental Science 1249, no. 1 (2023): 012024. http://dx.doi.org/10.1088/1755-1315/1249/1/012024.

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Abstract Soils consisting of porous particles, such as pumice sands and calcareous sands, exhibit unique characteristics due to the presence of intraparticle voids. Although significant impacts of intraparticle voids on mechanical behavior, such as reduced single-particle crushing strength and shear modulus in pumice sands, have been reported, quantifying the intraparticle porosity is still challenging. Therefore, the previous research has primarily focused on macroscopic behavior, overlooking the influence of intra-particle voids. This study proposes an analytical approach to quantify intrapa
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26

Lucian, Charles. "Characterization of Particle Size Distribution in Expansive Soils using Logarithmic Density Distribution." International Journal of Engineering Trends and Technology 49, no. 3 (2017): 161–69. http://dx.doi.org/10.14445/22315381/ijett-v49p225.

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27

Owonubi, Ayodele. "Evaluation of Physical Characteristics of Soils Derived from Basement Complex Rocks of the Jos Plateau." UMYU Scientifica 1, no. 2 (2022): 39–45. http://dx.doi.org/10.56919/usci.1222.005.

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The physical characteristics of soils to a large extent influences soil productivity. The objective of this study therefore is to evaluate the physical characteristics of soils derived from basement complex rocks of the Jos Plateau. According to the methodology outlined in the Soil Survey manual, the stratification of the study region into three geologic units—granite gneiss, biotite granite, and migmatite—was the first step in the soil research process. Additionally, soil samples were collected from genetic strata and soil profile pits were dug in each of these geologic units. Following stand
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28

Indraratna, Buddhima, Vo Trong Nguyen, and Cholachat Rujikiatkamjorn. "Hydraulic conductivity of saturated granular soils determined using a constriction-based technique." Canadian Geotechnical Journal 49, no. 5 (2012): 607–13. http://dx.doi.org/10.1139/t2012-016.

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This study presents a new semi-empirical approach for predicting the saturated hydraulic conductivity of noncohesive (granular) soils through a constriction size–based technique. For the same particle-size distribution of a granular filter material, there can be many different void distributions depending on the as-compacted density. Therefore, particle-size distribution is not unique in determining the hydraulic conductivity as proposed in numerous earlier studies. In contrast, the constriction-size distribution is unique for a given as-placed density of the material, and therefore it is a be
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29

Kinoshita, Alicia M., Rey Becerra, Marta Miletić, and Natalie Mladenov. "Upland and Riparian Surface Soil Processes in an Urban Creek with Native and Non-Native Vegetation after Fire." Fire 5, no. 2 (2022): 32. http://dx.doi.org/10.3390/fire5020032.

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Wildfires can pose environmental challenges in urban watersheds by altering the physical and chemical properties of soil. Further, invasive plant species in urban riparian systems may exacerbate changes in geomorphological and soil processes after fires. This research focuses on the 2018 Del Cerro fire, which burned upland and riparian areas surrounding Alvarado Creek, a tributary to the San Diego River in California. The study site has dense and highly flammable non-native vegetation cover (primarily Arundo donax) localized in the stream banks and has primarily native vegetation on the hillsl
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30

W., Medugu D., M. Maina, and Y.B. Dibal. "Particle Size Analysis of Soil Obtainable in Maiduguri, Nigeria." International Journal of Sciences Volume 6, no. 2017-09 (2017): 85–93. https://doi.org/10.5281/zenodo.3350108.

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Soil is a substantial resource and displays adaptable physical, chemical, mineralogical, hydrological and geochemical properties. Particle size is a fundamental analysis procedure for soils, and pedological and paleopedological analysis. In view of this particle size distribution of soil samples were conducted and analysed for 10 locations in Maiduguri, Nigeria by sieving technique. Their sand, silt, and clay contents were determined. The distribution of particle size influences the moisture retention and transmission properties of soils. The overall result showed that the soil in Maiduguri is
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31

Botula, Yves-Dady, Wim M. Cornelis, Geert Baert, Paul Mafuka, and Eric Van Ranst. "Particle size distribution models for soils of the humid tropics." Journal of Soils and Sediments 13, no. 4 (2013): 686–98. http://dx.doi.org/10.1007/s11368-012-0635-5.

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Esmaeelnejad, Leila, Fatemeh Siavashi, Javad Seyedmohammadi, and Mahmood Shabanpour. "The best mathematical models describing particle size distribution of soils." Modeling Earth Systems and Environment 2, no. 4 (2016): 1–11. http://dx.doi.org/10.1007/s40808-016-0220-9.

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Wang, Ning, Mamattursun Eziz, Donglei Mao, and Nazupar Sidekjan. "Fractal Characteristics of the Particle Size Distribution of Soil along an Urban–Suburban–Rural–Desert Gradient." Land 12, no. 12 (2023): 2120. http://dx.doi.org/10.3390/land12122120.

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In order to investigate the difference in particle size distribution of soil along an urban–suburban–rural–desert (USRD) gradient in an arid zone, surface soil (0–20 cm) samples were gathered at the urban, suburban, rural, and desert gradients in Urumqi, a northwestern Chinese city. Laser diffraction technology was adopted for determining the particle size distribution of the soil. Comparisons were made regarding the particle size distribution traits and soil properties in different gradient zones based on parameters such as the mean particle size (MG), fractal dimension (Dv), sorting coeffici
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34

Manmatharajan, Mathan V., Edouardine-Pascale Ingabire, Alex Sy, and Mason Ghafghazi. "Effect of particle size and particle size distribution on the post-liquefaction strength of granular soils." Soils and Foundations 63, no. 4 (2023): 101336. http://dx.doi.org/10.1016/j.sandf.2023.101336.

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35

Uday, Sankar Banerjee, Guo Zhao-hui, Zhou Kanggen, and Chai Li-Yuan. "Distribution and plant availability of Cd, Pb, Cu and As in different particlesize soil fractions." Journal of Indian Chemical Society Vol. 94, Sep 2017 (2017): 1029–35. https://doi.org/10.5281/zenodo.5637767.

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Institute of Environmental Engineering, School of Metallurgy and Environment, Central South University, Changsha 410083, China <em>E-mail</em> : banerjeesme@csu.edu.cn, banerjeeenvsc@gmail.com <em>Manuscript received 06 July 2017, accepted 08 August 2017</em> The present study was conducted to evaluate the distribution and plant availability of Cd, Pb, Cu and As in different particle-size soil fractions. The distribution of total heavy metals and their plant availability were investigated in a metal mining area in the Hunan Province, China. Soils were partitioned into five particle-size fracti
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Oades, JM, and AG Waters. "Aggregate hierarchy in soils." Soil Research 29, no. 6 (1991): 815. http://dx.doi.org/10.1071/sr9910815.

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An Alfisol, a Mollisol and an Oxisol were fractionated into different particle sizes after a range of disaggregating treatments from gentle to vigorous. The Alfisol and the Mollisol appeared to break down in steps; macroaggregates &gt;250 �m diameter breaking down to microaggregates 20-250 �m diameter before particles &lt;20 �m were released. Vigorous disruption led to particle size distributions similar to those obtained by classical methods used to determine particle size distributions. The Oxisol was stable to rapid wetting treatments but when aggregate disruption was initiated by vigorous
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37

Rhee, Hakjun, Randy B. Foltz, James L. Fridley, Finn Krogstad, and Deborah S. Page-Dumroese. "An alternative method for determining particle-size distribution of forest road aggregate and soil with large-sized particles." Canadian Journal of Forest Research 44, no. 1 (2014): 101–5. http://dx.doi.org/10.1139/cjfr-2013-0327.

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Measurement of particle-size distribution (PSD) of soil with large-sized particles (e.g., 25.4 mm diameter) requires a large sample and numerous particle-size analyses (PSAs). A new method is needed that would reduce time, effort, and cost for PSAs of the soil and aggregate material with large-sized particles. We evaluated a nested method for sampling and PSA by comparing it with the methods that follow the American Association of State Highway and Transportation Officials (AASHTO) standard T88-00 and the American Society for Testing and Materials (ASTM) standard D422-63. Using 33 forest road
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Sufardi, S., T. Arabia, K. Khairullah, and I. Apriani. "Particle size distribution and clay minerals in dryland soils of Aceh Besar, Indonesia." IOP Conference Series: Earth and Environmental Science 922, no. 1 (2021): 012013. http://dx.doi.org/10.1088/1755-1315/922/1/012013.

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Abstract Soil particle size distribution is a fundamental physical property affecting other soil properties. This research aims to determine the distribution of soil particles and the composition of clay minerals on each layer of the horizon in four soil profiles (P1, P2, P3, and P4) with different parent materials in the dryland of Aceh Besar district which includes Entisols Jantho, Andisols Saree, Inceptisols Cucum, and Oxisols Lembah Seulawah. Particle size distribution (or texture) and bulk density (BD) were analyzed in the laboratory. Soil structure and consistency were observed directly
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Choe, Yonghwan, Sang Hyeop Park, and Deok Hyun Moon. "Remediation of Petroleum-Contaminated Gas Station Soil Using High-Pressure Soil Washing Technology." Journal of Korean Society of Environmental Engineers 45, no. 12 (2023): 541–50. http://dx.doi.org/10.4491/ksee.2023.45.12.541.

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Objectives : In this study, high-pressure soil washing was performed on in-situ gas station soils for the remediation of petroleum-contaminated gas station sites.Methods : On-site gas station soils (GSS) collected from four different locations were subjected to high-pressure soil washing to analyze the amount of fine soil removal and TPH concentration after washing according to the cut-off size (0.075, 0.105 mm). In addition, the four GSS were evaluated for the relationship between the organic matter content of each soil and TPH removal efficiency. Furthermore, to evaluate the disintegration f
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Langmi, H. W., and J. Watt. "Evaluation of computer-controlled SEM in the study of metal-contaminated soils." Mineralogical Magazine 67, no. 2 (2003): 219–31. http://dx.doi.org/10.1180/0026461036720096.

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Computer-controlled scanning electron microscopy (CCSEM) has been assessed for the determination of form and size distribution of heavy metals in urban contaminated soils. Metal distributions within individual particles were determined using X-ray element mapping. The sites selected for study were (1) around a landfill site, previously a colliery in Wolverhampton, UK and (2) a private garden adjacent to a railway in Nottingham, UK. Backscattered thresholding techniques were used to isolate the Pb-containing categories. The classification results for both Wolverhampton and Nottingham soils were
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Straż, Grzegorz, and Małgorzata Szostek. "The Use of a Laser Diffractometer to Analyze the Particle Size Distribution of Selected Organic Soils." Applied Sciences 14, no. 18 (2024): 8104. http://dx.doi.org/10.3390/app14188104.

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This study was conducted to verify the usefulness of the laser diffractometer method for determining the particle size distribution of selected organic soils from the Podkarpacie region in Poland. The soil selected for this research represented three main classification groups, namely, low-organic, medium-organic and high-organic soil, in accordance with the standard criterion. Particle size distribution was determined using two types of laser diffractometers: the Helos laser diffractometer manufactured by Sympatec GmbH (Clausthal-Zellerfeld, Germany) and the laser particle size analyzer Analy
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Samuel-Rosa, Alessandro, Ricardo Simão Diniz Dalmolin, and Pablo Miguel. "Building predictive models of soil particle-size distribution." Revista Brasileira de Ciência do Solo 37, no. 2 (2013): 422–30. http://dx.doi.org/10.1590/s0100-06832013000200013.

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Is it possible to build predictive models (PMs) of soil particle-size distribution (psd) in a region with complex geology and a young and unstable land-surface? The main objective of this study was to answer this question. A set of 339 soil samples from a small slope catchment in Southern Brazil was used to build PMs of psd in the surface soil layer. Multiple linear regression models were constructed using terrain attributes (elevation, slope, catchment area, convergence index, and topographic wetness index). The PMs explained more than half of the data variance. This performance is similar to
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Huisz, Andrea, Steven Sleutel, Tibor Tóth, Georges Hofman, Stefaan De Neve, and Tamás Németh. "The effect of soil cultivation systems on organic matter distribution in different grain size fractions of the soil based on three years of experience." Acta Agraria Debreceniensis, no. 22 (May 23, 2006): 22–30. http://dx.doi.org/10.34101/actaagrar/22/3186.

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Changes in the physical distribution (particle size and the state stability against decomposition) of the organic carbon pool in tilled layers of Hungarian field soil under different tillage treatments were studied. Three years after starting the experiment, soil samples were fractionated (they were taken in March 2005) by their particle size and density. The treatments caused well measurable, significant effects on two fractions of intra-microaggregate organic matter (53-250μm particle-sized, well and less decomposition-resistant pools) and onto their relative rate in the organic carbon pool
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Dan, Han-Cheng, Zhuo-Min Zou, Jia-Qi Chen, and An-Ping Peng. "DEM-aided method for predicting the hydraulic properties with particle-size distribution of porous media." Engineering Computations 36, no. 5 (2019): 1716–43. http://dx.doi.org/10.1108/ec-09-2018-0398.

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Purpose The soil water retention curve (SWRC) and unsaturated hydraulic conductivity (UHC) are crucial indices to assess hydraulic properties of porous media that primarily depend on the particle and pore size distributions. This study aims to present a method based on the discrete element model (DEM) and the typical Arya and Paris model (AP model) to numerically predict SWRC and UHC. Design/methodology/approach First, the DEM (PFC3D software) is used to construct the pore and particle size distributions in porous media. The number of particles is calculated according to the AP model, which ca
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Bova, O. V. "Physico-chemical and chemical properties of chernozems of the Pselsko-Vorskla interfluve of the Sumy region." Prirodničì nauki 17, no. 1 (2020): 110–13. https://doi.org/10.5281/zenodo.4482106.

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The article presents the results of field and chemical-analytical studies of chernozem soils of the forest-steppe of Sumy region. The main physicochemical parameters of soils (aqueous extracts pH, total humus, amount of absorbed bases, hydrolytic acidity, absorption capacity), particle size distribution and composition of water extract ions were determined. Their distribution in the soil profile was analyzed.
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Chaudhari, S. K., and R. K. Batta. "Predicting unsaturated hydraulic conductivity functions of three Indian soils from particle size distribution data." Soil Research 41, no. 8 (2003): 1457. http://dx.doi.org/10.1071/sr03040.

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The present study compares experimental unsaturated hydraulic conductivity functions, K(θ), of 9 soils of Maharashtra State of India, 3 each in the clay, clay loam, and loam textural classes, all predicted by a particle size distribution (PSD) based model. PSD data were transformed into pore-size distribution using Aryas' modified model. Experimental K(θ) curves were determined by the horizontal infiltration method. Fifteen soils, 5 each with clay, clay loam, and loam texture, were used to evaluate the parameters of flow model (i.e. qi = crix) empirically. These parameters deviated from Hagen-
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Bittelli, Marco, Gaylon S. Campbell, and Markus Flury. "Characterization of Particle-Size Distribution in Soils with a Fragmentation Model." Soil Science Society of America Journal 63, no. 4 (1999): 782–88. http://dx.doi.org/10.2136/sssaj1999.634782x.

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Khitrov, N. B. B., and L. V. Rogovneva. "Particle-size distribution patterns in Vertisols and vertic soils of Russia." Eurasian Soil Science 50, no. 3 (2017): 312–26. http://dx.doi.org/10.1134/s1064229317030061.

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Pearson, M. J., S. E. Monteith, R. R. Ferguson, et al. "A method to determine particle size distribution in soils with gypsum." Geoderma 237-238 (January 2015): 318–24. http://dx.doi.org/10.1016/j.geoderma.2014.09.016.

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Guo, Shuyang, Jie Cui, Yi Shan, Yadong Li, Kelin Chen, and Kezheng Yang. "Experimental Study on Liquefaction Characteristics of Coral Gravelly Soils with Different Particle Size Distributions." Journal of Marine Science and Engineering 11, no. 7 (2023): 1356. http://dx.doi.org/10.3390/jmse11071356.

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Many laboratory studies have shown that particle size distribution (PSD) affects the liquefaction susceptibility of granular materials. However, few studies have focused on the impact of PSD on coral particles. In this study, two different soil families were prepared: one with three levels of mean particle size (D50) with identical uniformity coefficient (Cu)and the other with four levels of Cu with the same D50 for coral gravelly soils. In addition, a series of undrained cyclic triaxial tests were conducted on coral gravelly particles with two groups of PSDs at a relative density of 40% and a
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