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1

TAMAL, K. JANA, and DAS BISWANATH. "Sorption of Carbofuran (2,3-Dihydro-2,2-dimethylbenzofuranylmethylcarbamate) by Soil." Journal of Indian Chemical Society Vol. 75, Jun 1998 (1998): 354–56. https://doi.org/10.5281/zenodo.5937254.

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Department of Agricultural Chemistry &amp; Soil Science, Faculty of Agriculture, Bidhan Chandra Krishi Viswavidyalaya, Mohanpur-741 252 <em>Manuscript received 28 June 1996, revised 3 April 1997, accepted 23 October 1997</em> Sorption of the insecticide Carbofuran by four different soils of West Bengal have been investigated. Adsorption equilibria studies indicated that adsorption of the insecticide by soil was complete within 3 h. The adsorption isotherm yielding S-shaped curve could be described by Frundlich equation. The order of adsorption capacity (K) of the soils for Carbofuran has been
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2

Ananko, T. V., M. I. Gerasimova, and N. V. Savitskaya. "Floodplain soils on the soil map of the Russian Federation, scale 1 : 2.5 M, 1988, in the Russian soil classification, 2004." Dokuchaev Soil Bulletin, no. 113 (December 30, 2022): 5–30. http://dx.doi.org/10.19047/0136-1694-2022-113-5-30.

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The largest area of taiga gley-differentiated soils on the Soil map of Russian Federation, scale 1:2.5 M, is located in the north of West Siberia. Small areas are dispersed over the northwestern European Russia, Eastern Siberia and the North-East. Interpretation of taiga gley-differentiated soils in terms of Russian soil classification system (2004) is rather ambiguous owing to high diversity of ecological conditions where these soils occur, аs well as variability of soil morphological, chemical, and physicochemical properties in diverse mapping units. Comparing properties of taiga gley-differ
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3

Boyraz, Erdem D., and C. Cangir. "Evaluation of Soil Engineering Characteristics of Some Soils in Entisol and Inceptisol." Journal of Scientific and Engineering Research 10, no. 5 (2023): 88–93. https://doi.org/10.5281/zenodo.10457673.

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<strong>Abstract </strong>The soils of the research area are classified in Entisol and Inceptisol Orders. Entisol Order is classified in Typic Xerofluvent Subgroup, Inceptisol Order is classified in Fluventic Haploxerept, Calcic Haploxerept, Typic Haploxerept subgroup. The adhesion, cohesion and shear resistance values of the soils and therefore the behavior of the soils against cultivation and depending on the soil engineering properties are very different. For this reason, the functions of moisture in soils should be well evaluated in the mechanization conditions of soils. Otherwise, air, wa
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4

Gerasimova, M. I., T. V. Ananko, D. E. Konyushkov, and N. V. Savitskaya. "Agrogenic Soils on the Updated Version of the Soil Map of Russia, 1 : 2.5 M Scale: Classification Diversity and Place in the Soil Cover." Почвоведение, no. 2 (February 1, 2023): 143–53. http://dx.doi.org/10.31857/s0032180x22600846.

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Usually, soils changed by farming (agrogenic soils) are not shown on small-scale maps, including the Soil Map of the Russian Federation, 1 : 2.5 M scale (1988). One of the issues of the map updating performed by the Dokuchaev Soil Science Institute is the inclusion of agrogenic soils into the map contents and representation of some of the former native soils as agrogenic soils on the updated map. Preliminarily, all native soils shown on the map have been reclassified into the new Russian soil classification system. Agrogenic soils in this system are separated as agrosoils in different orders a
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5

Foster, Neil, John Spoelstra, Paul Hazlett, et al. "Heterogeneity in soil nitrogen within first-order forested catchments at the Turkey Lakes Watershed." Canadian Journal of Forest Research 35, no. 4 (2005): 797–805. http://dx.doi.org/10.1139/x05-016.

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Topographic positional regulation of nitrogen (N) dynamics in soil within Canadian Shield headwaters, located in calibrated catchments containing mature, tolerant hardwood forest, was examined to determine how N pools, mineralization, nitrification, and leaching in soil relate to N export in drainage waters. A uniformly high net N mineralization and nitrification potential for surficial soil layers rich in organic N was demonstrated for ridge, upper-middle slope, and lower slope – footslope topographic positions. Results from plot-scale studies revealed that NO3– concentrations in soil water f
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6

Petersmann, Marie. "Reordering the European ground – regrounding the European legal order?" European Law Open 3, no. 1 (2024): 180–89. http://dx.doi.org/10.1017/elo.2024.12.

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AbstractThis contribution to the Symposium on Ecosystem Restoration and EU Law assesses the underground protection schemes suggested by the European Green Deal (EGD) for the European Union (EU). By addressing the overground bias that environmental laws and policies have traditionally suffered from, the analysis engages with the EU Soil Strategy for 2030, its ‘Mission “A Soil Deal for Europe”’, and the proposed 2023 Soil Monitoring Directive. The Article explores how and to what extent this agenda for the preservation and restoration of soils is legally reordering the European ground and, simul
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7

Anne Naeth, M., Heather A. Archibald, Candace L. Nemirsky, et al. "Proposed classification for human modified soils in Canada: Anthroposolic order." Canadian Journal of Soil Science 92, no. 1 (2012): 7–18. http://dx.doi.org/10.4141/cjss2011-028.

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Naeth, M. A., Archibald, H. A., Nemirsky, C. L., Leskiw, L. A., Brierley, J. A., Bock, M. D., VandenBygaart, A. J. and Chanasyk, D. S. 2012. Proposed classification for human modified soils in Canada: Anthroposolic order. Can. J. Soil Sci. 92: 7–18. With increasing anthropogenic activity, the areal extent of disturbed soils is becoming larger and disturbances more intense. Regulatory frameworks must incorporate reclamation criteria for these disturbed soils, requiring consistent descriptions and interpretations. Many human altered soils cannot be classified using the Canadian System of Soil Cl
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8

N. N. Bhalekar, S. M. Todmal, B. M. Kamble, A. G. Durgude, S. A. Kadam, and U. M. Shetti. "Assessment of Soil Physico-Chemical Traits in Soil Profile from Maheshgad Watershed." Journal of Agriculture Research and Technology 49, no. 03 (2024): 439–43. https://doi.org/10.56228/jart.2024.49310.

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Soil profile studies was conducted in Maheshgad watershed, central campus MPKV, Rahuri, two soil orders viz., Entisol and Inceptisol were analysed for soil physical and chemical properties. These orders were shallow (entisol), and moderately deep (Inceptisol) and identified as Inceptisols (Vertic Haplustepts), Entisols (Typic Ustifluvents) and Entisols (Typic Ustorthents), respectively. The pH of the profile soil samples ranged between 6.59 to 7.56, the EC ranged from 0.17 to 0.21 dSm-1. The SOC content of the soils ranged from 0.31 % to 0.46%. The CaCO3 content was 6.89% to 10.32%. The Bulk d
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9

McKEAGUE, J. A., C. TARNOCAI, and H. A. LUTTMERDING. "EXISTING AND POSSIBLE NEW GLEYSOLIC ORDER CRITERIA APPLIED TO FIVE PEDONS FROM BRITISH COLUMBIA." Canadian Journal of Soil Science 66, no. 2 (1986): 323–36. http://dx.doi.org/10.4141/cjss86-033.

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Use of the current criteria for distinguishing Gleysolic soils from gleyed intergrades to other soil classes resulted in the apparent misclassification of some soils in British Columbia. Pedologists of the area selected five pedons encompassing several degrees of expression of gley features. Current classification criteria based on soil color and possible new differentiating features based on chemical and micromorphological analyses were applied in considering the classification of the soils. Application of the current specific color criteria involving low chromas and prominent mottling result
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10

Lu, Weisheng, Ying Liu, Huike Ye, et al. "Adsorption and Desorption Characteristics of Cadmium on Different Contaminated Paddy Soil Types: Kinetics, Isotherms, and the Effects of Soil Properties." Sustainability 13, no. 13 (2021): 7052. http://dx.doi.org/10.3390/su13137052.

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The adsorption and desorption characteristics of cadmium (Cd) in uncontaminated soils have been investigated in numerous studies. However, similar studies on Cd-polluted soils from different sources, which exhibit complex physicochemical characteristics and internal interactions between Cd and the soil particles, are scarce. Therefore, in order to elucidate the adsorption and desorption characteristics of Cd in Cd polluted soils, six representative Cd-contaminated paddy soil samples were collected from farmlands in the vicinity of a steel plant (Soil 1), a smelter (Soil 2), a thermal power pla
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11

Sakbaeva, Zulfiia, Veronica Acosta-Martínez, Jennifer Moore-Kucera, Wayne Hudnall, and Karabaev Nuridin. "Interactions of Soil Order and Land Use Management on Soil Properties in the Kukart Watershed, Kyrgyzstan." Applied and Environmental Soil Science 2012 (2012): 1–11. http://dx.doi.org/10.1155/2012/130941.

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Surveys of soil properties related to soil functioning for many regions of Kyrgyzstan are limited. This study established ranges of chemical (soil organic matter (SOM), pH and total N (TN)), physical (soil texture), and biochemical (six enzyme activities of C, N, P, and S cycling) characteristics for nine profiles from the Kukart watershed of Jalal-Abad region in Kyrgyzstan. These profiles represent different soil orders (Inceptisols, Alfisols, and Mollisols) and land uses (cultivated, nut-fruit forests, and pasture). The Sierozem (Inceptisols) soils had the highest pH and contained the lowest
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Aditya, Haidar Fari, and Fitri Wijayanti. "Development of soil characteristics in the UPN "Veteran" Jawa Timur experimental field in Wonosalam District, Jombang Regency, East Java." Ilmu Pertanian (Agricultural Science) 9, no. 2 (2024): 77. http://dx.doi.org/10.22146/ipas.91436.

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Soil characteristic and properties are essential determinants for effective land management. Soil genesis results from the interaction of various pedogenic factors, which are influenced by environmental conditions, thereby producing diverse soil types in different locations. This study was conducted in the Wonosalam sub-district, an area characterized by diverse regional conditions due to its varied physiographic features. The physiographic and climatic conditions in this region significantly influence soil formation processes. This research focused on monitoring soil development at several lo
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13

Mahdy, A. M. "Comparative effects of different soil amendments on amelioration of saline-sodic soils." Soil and Water Research 6, No. 4 (2011): 205–16. http://dx.doi.org/10.17221/11/2011-swr.

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&amp;nbsp; A greenhouse experiment was conducted to test the potential of different soil amendments in saline-sodic soils reclamation; to affect the growth response of alfalfa (Medicago sativa L.) plants grown on two saline-sodic soils; and to evaluate the comparative efficiency of different soil amendments for their effects on salinity, sodicity, and pH&amp;nbsp;levels of the soils. To achieve these objectives, two highly saline-sodic soils were selected (Abees, Typic torrifluvents and Elhammam, Typic calciorthids). Different soil amendments were used (compost, anthracite coal powder, water t
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14

Kunze, B. O., and G. D. Lemme. "Photography for Order 2 Soil Surveys." Soil Horizons 27, no. 3 (1986): 10. http://dx.doi.org/10.2136/sh1986.3.0010.

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15

Morand, David T. "The World Reference Base for Soils (WRB) and Soil Taxonomy: an appraisal of their application to the soils of the Northern Rivers of New South Wales." Soil Research 51, no. 3 (2013): 167. http://dx.doi.org/10.1071/sr12144.

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Few soil surveys in New South Wales have utilised international soil classifications. Extensive morphological and laboratory data collected during soil surveys in the Northern Rivers region provided a strong basis for correlation with the World Reference Base for Soil Resources (WRB), Soil Taxonomy (ST), and the Australian Soil Classification (ASC). Of the 32 reference soil groups comprising the WRB, 20 were present locally; nine of the 12 ST orders were present. After re-classification of soils, correlation of the ASC with the WRB and ST was undertaken. Soils not requiring extensive laborator
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16

Brierley, J. A., H. B. Stonehouse, and A. R. Mermut. "Vertisolic soils of Canada: Genesis, distribution, and classification." Canadian Journal of Soil Science 91, no. 5 (2011): 903–16. http://dx.doi.org/10.4141/cjss10060.

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Brierley, J. A., Stonehouse, H. B. and Mermut, A. R. 2011. Vertisolic soils of Canada: Genesis, distribution, and classification. Can. J. Soil Sci. 91: 903–916. The Vertisolic soil order is the most recent addition to the Canadian System of Soil Classification (1998). Soils of the Vertisolic order in Canada occur within the Brown, Dark Brown, and Black soil zones, associated with the Prairie ecozone. Due to the absence of swelling clays in central Canada, morphological characteristics of Vertisolic or vertic intergrades are not recognized in soils occurring to the east of Manitoba. Finetexture
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17

Cui, Zhi Yi, Xiao Mei Deng, Ru Chun Xi, Rui Ping Li, and Jia Xin Hu. "Nutrient Limiting Factors in Red-Yellow Soil from Different Parent Rocks at Oil-Tea Forest Land in the South-Central Region of China." Applied Mechanics and Materials 694 (November 2014): 568–75. http://dx.doi.org/10.4028/www.scientific.net/amm.694.568.

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Nutrient limiting factors in main soils from oil tree forest land of the south-central region in Hunan Province were assessed by employing the systematic approach developed by Agro Services International and selecting Sorghum as indicate plant in order to evaluate their nutrient status and limiting factors. The results of soil testing showed that the four oil tree forest land soils were low in organic matter, N, P, K was severely deficient, but the available S and Fe were sufficient, the deficiency of Ca, Mg, B, Zn and Mo were rather common. In the tested oil tree Camellia forest land soils, t
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18

Dhaliwal, Salwinder Singh, Vivek Sharma, Janpriya Kaur, et al. "The Pedospheric Variation of DTPA-Extractable Zn, Fe, Mn, Cu and Other Physicochemical Characteristics in Major Soil Orders in Existing Land Use Systems of Punjab, India." Sustainability 14, no. 1 (2021): 29. http://dx.doi.org/10.3390/su14010029.

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The agricultural production in Punjab has increased manifold that aggravated the deficiencies of micronutrients in soils and plants. The availability of soil micronutrients in different soil orders depends upon the soil mineralogy, topography, climatic conditions and cropping sequences. Hence, to study the pedospheric variations of DTPA-extractable micronutrients, viz., zinc (Zn), iron (Fe), manganese (Mn) and copper (Cu), in three prominent soil orders of Punjab, a total of 144 depth-wise soil samples were collected from four major land-use systems (cultivated, horticulture, forest and pastur
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19

Sufardi, S., T. Arabia, K. Khairullah, et al. "Assessment of carbon and nitrogen distribution on several soil orders for sustainable management in dryland farming: A Case Study in Aceh Besar Regency, Indonesia." IOP Conference Series: Earth and Environmental Science 1230, no. 1 (2023): 012062. http://dx.doi.org/10.1088/1755-1315/1230/1/012062.

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Abstract The study was based on the distribution of soil carbon and nitrogen orders in a dryland farming system in Aceh Besar District, Indonesia. Soil samples were taken to represent 6 (six) soil orders in the drylands of Aceh Besar, namely: Andisols, Entisols, Inceptisols, Mollisols, Oxisols, and Ultisols. For each soil order, 5 observation profiles were made, and each soil profile was sampled at 7 (seven) soil depths from 0-100 cm, namely: 0-0.05 m; 0.05-0.10 m; 0.10-0.20m; 0.20-0.30m; 0.03-0.50m; 0.05-0.70 m; and 0.07-1.00 m so that there are 210 soil samples. The Walkley and Black method
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Echebba, El Mehdi, Hasnae Boubel, Abdelhay El Omari, Mohamed Rougui, Mimoun Chourak, and Fadi Hage Chehade. "Analysis of the Second Order Effect of the SSI on the Building during a Seismic Load." Infrastructures 6, no. 2 (2021): 20. http://dx.doi.org/10.3390/infrastructures6020020.

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The type and the properties of the soil can potentially intensify the internal forces on buildings during seismic loads. To predict the effects of the soil parameters on the soil–structure interaction of buildings, it is necessary to consider the soil–structure interaction (SSI) in the modeling process. Therefore, this document aims to evaluate the seismic effect on the maximal displacement and inter-story drift, and evaluate the behavior of buildings under the second-order effect known in the literature as the P-delta effect. For this purpose, three cases of buildings with 5, 10 and 15 storie
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Qane, Khatera, Rohtas Kumar, Ankush Kamboj, Vikas Kumar, Nasir Ahmad Qazizada, and Asha. "Comparative Analysis of Microbiological Aspects in Forest and Agricultural Soils across Major Soil Orders of Haryana." International Journal of Plant & Soil Science 37, no. 6 (2025): 427–40. https://doi.org/10.9734/ijpss/2025/v37i65522.

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This study evaluates and compares the microbiological properties of forest and agricultural soils across major soil orders (Inceptisols, Entisols, Aridisols, and Alfisols) in Haryana to assess the impact of land use on soil biological health. Surface soil samples were collected at five representative sites of each soil order, spanning districts including Sirsa, Hisar, Jind, Karnal, Ambala, Mahendergarh, and Bhiwani. Composite soil samples were prepared by mixing three randomly collected auger cores per site, avoiding disturbed or recently fertilized areas. Each sample was split: one part air-d
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Tian, An-Hong, Cheng-Biao Fu, Hei-Gang Xiong, and Her-Terng Yau. "Innovative Intelligent Methodology for the Classification of Soil Salinization Degree Using a Fractional-Order Master-Slave Chaotic System." International Journal of Bifurcation and Chaos 29, no. 02 (2019): 1950026. http://dx.doi.org/10.1142/s0218127419500263.

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Soil salinization has become a highly significant eco-system issue that is encountered all over the world. Serious soil salinization leads to soil deterioration and has a negative impact on sustainable development of the eco-system and agriculture. However, the spectral reflectance of soils with high overlap and indecipherability makes it difficult to classify the soil salinization degree quickly and accurately. In this paper, an innovative, intelligent methodology using a fractional-order chaotic system to classify the soil salinization degree is proposed. To select a suitable order for the f
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Silva Neto, Luís de França da, Alberto Vasconcellos Inda, Paulo César Do Nascimento, Elvio Giasson, Catiline Schmitt, and Nilton Curi. "CHARACTERIZATION AND CLASSIFICATION OF FLOODPLAIN SOILS IN THE PORTO ALEGRE METROPOLITAN REGION, RS, BRAZIL." Ciência e Agrotecnologia 39, no. 5 (2015): 423–34. http://dx.doi.org/10.1590/s1413-70542015000500001.

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ABSTRACTIn the Porto Alegre metropolitan region (PAMR) there are a significant proportion of floodplain soils, mainly Planosols and Gleysols, in relation to upland soils. This study aimed to evaluate the morphological, chemical and physical characteristics, and to classify floodplain soils in the PAMR. Six soil profiles were evaluated under different sedimentary lithologies and drainage classes, and samples were collected for chemical and physical analyzes. Two orders of mineral soils (Planosols and Gleysols) and one order of organic soil (Organosols) were identified. The soils were moderately
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Stapelberg, F. D. J. "Case study in the Northern Cape (Loopeng area), South Africa, confirming occurrence of a collapsible sand soil structure in transported soils." South African Journal of Geology 125, no. 2 (2022): 217–24. http://dx.doi.org/10.25131/sajg.125.0014.

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Abstract Testing was performed on transported soils belonging to recently deposited sandy-silty soil deposits occurring in and around Loopeng Village, Northern Cape Province, South Africa, in order to determine the occurrence and order of magnitude of a collapsible sand soil structure. Various empirical geotechnical characteristics including: in situ soil profile structure description, particle grading curve and clay content, soil classification, soil density and void ratio were compared to collapse potential values determined with oedometer testing, in order to judge the success with which the
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Goetz, Andrew J., Robert H. Walker, Glenn Wehtje, and Ben F. Hajek. "Sorption and Mobility of Chlorimuron in Alabama Soils." Weed Science 37, no. 3 (1989): 428–33. http://dx.doi.org/10.1017/s0043174500072179.

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Soil thin-layer chromatography and a soil solution technique were used to evaluate chlorimuron adsorption and mobility in five Alabama soils. The order of adsorption was atrazine &gt; metribuzin &gt; chlorimuron; mobility was chlorimuron &gt; metribuzin &gt; atrazine. The order of adsorption of chlorimuron in the five soils was Sumter clay &gt; Eutaw clay &gt; Lucedale fine sandy loam &gt; Decatur silt loam &gt; Dothan sandy loam, and Rfvalues were 0.63, 0.73, 0.69, 0.76, and 0.80, respectively. Chlorimuron mobility and adsorption were not highly correlated to any one soil type. Adsorption of
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El Boukili, Abdellah, Nidae Loudiyi, Ahmed El Bazaoui, Abderrahim El Hourch, M'Hamed Taibi, and Abderrahman EL Boukili. "Adsorption and Desorption Behavior of Herbicide Mefenpyr-diethyl in the Agricultural Soils of Morocco." Mediterranean Journal of Chemistry 7, no. 5 (2018): 386–95. http://dx.doi.org/10.13171/mjc7519111210255aeb.

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The present study was conducted in order to investigate the adsorption and desorption behavior of Mefenpyr-diethyl (MFD) using the batch equilibration technique in four soils, with different ranges of organic matter content, from different regions of Morocco orders of Benimellal (Soil 1), Settat (Soil 2), Sidi Bettach (Soil 3) and EL Hajeb (Soil 4). The adsorption isotherm models Langmuir, linear and Freundlich were used to compare the adsorption capacity of the soils. The results indicated that the Freundlich equation provided the best fit for all adsorption data. The values of KF and Kd rang
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Nursyamsi, Dedi, Komaruddin Idris, Supiandi Sabiham, Djunaedi Abdul Rachim, and Agus Sofyan. "NH4+, dan Fe3+ terhadap Ketersediaan K Jerapan dan Pengaruh Na+, NH4+ pada Tanah-tanah yang Didominasi Mineral Liat Smektit." JOURNAL OF TROPICAL SOILS 14, no. 1 (2009): 33. http://dx.doi.org/10.5400/jts.2009.v14i1.33-40.

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Total content of potassium in smectitic soils is commonly high, however its availability for plant growth is frequently problem because it is fixed at interlayer space of 2:1 type of clay mineral. The research was aimed to study the sorption and effect of Na+, NH +, and Fe3+ on soil available K at smectitic soils. It was conducted in Laboratory of Research and Soil Test, Indonesian Soil Research Institute by using four of soil samples taken from Bogor (Typic Hapludalfs), Cilacap (Chromic Endoaquerts), Ngawi (Typic Endoaquerts), and Blora (Typic Haplustalfs). Incubation experiment used Randomiz
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Pidkova, Oksana M. "Determination of the amount of damage caused to the land and soils of Ukraine by military actions: calculation methods and current issues." Physical Geography and Geomorphology 47, no. 2 (2024): 35–42. http://dx.doi.org/10.17721/phgg.2024.3-4.04.

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The purpose of the publication is to review the documents of the regulatory framework of Ukraine that address the issues of determining the damage caused to soils and land as a result of the armed aggression of the russian federation, and to highlight the topical issues of theoretical, methodological and practical nature related to the determination of such damage. The article considers military soil degradation as a set of degradation processes that develop in soils as a result of military actions. Together with other types of degradation, military degradation worsens the current ecological s
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Dessureault-Rompré, Jacynthe, Bernie J. Zebarth, David L. Burton, and Alex Georgallas. "Predicting soil nitrogen supply from soil properties." Canadian Journal of Soil Science 95, no. 1 (2015): 63–75. http://dx.doi.org/10.4141/cjss-2014-057.

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Dessureault-Rompré, J., Zebarth, B. J., Burton, D. L. and Georgallas, A. 2015. Predicting soil nitrogen supply from soil properties. Can. J. Soil Sci. 95: 63–75. Prediction functions based on simple kinetic models can be used to estimate soil N mineralization as an aid to improved fertilizer N management, but require long-term incubations to obtain the necessary parameters. Therefore, the objective of this study was to examine the feasibility of predicting the mineralizable N parameters necessary to implement prediction functions and in addition to verify their efficiency in modeling soil N su
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Wu, Leiye, Wei Cheng, and Zhehao Zhu. "Fractional-Order Elastoplastic Modeling of Sands Considering Cyclic Mobility." Journal of Marine Science and Engineering 9, no. 4 (2021): 354. http://dx.doi.org/10.3390/jmse9040354.

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Seabed soil may experience a reduction in strength or even liquefaction when subjected to cyclic loadings exerted by offshore structures and environmental loadings such as ocean waves and earthquakes. A reasonable and robust constitutive soil model is indispensable for accurate assessment of such structure–seabed interactions in marine environments. In this paper, a new constitutive model is proposed by enriching subloading surface theory with a fractional-order plastic flow rule and multiple hardening rules. A detailed validation of both stress- and strain-controlled undrained cyclic test res
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31

Krishnasamy, R., and KK Krishnamoorthy. "Cationic interferences on zinc adsorption." Soil Research 29, no. 4 (1991): 527. http://dx.doi.org/10.1071/sr9910527.

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The effects of bivalent cations such as Mg2+, MN2+, FE2+ and Cu2+ on zinc adsorption in 16 surface soil samples (0-25 cm depth), representing major soil series of Tamil Nadu (India), and of the soil orders Vertisol and lnceptisol were studied. The study revealed that the interference of the four bivalent cations on zinc adsorption was in the order Cu2+ &gt; Mn2+ &gt; Me2 + &gt; Mg2+. The effects of these ions on zinc adsorption could be explained on the basis of chemical properties such as magnetic moment value, kinetic classification, crystal field stabilization energy (CFSE) and kinetics of
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Gowthamchand, Salwinder Singh Dhaliwal, Vivek Sharma, Gayatri Verma, Jagdish Singh, and Manpreet Kaur. "Variation of Physico-Chemical Properties among Different Soil Orders under Different Land Use Systems of the Majha Region in North-Western India." Sustainability 15, no. 6 (2023): 4779. http://dx.doi.org/10.3390/su15064779.

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The impact of different soil orders and land use systems on the distribution of physico-chemical properties is the most critical matter to address in order to maintain sustainable agricultural production. Hence, the present investigation was carried out to study the variation in the physico-chemical characteristics of soil in diverse land use systems (LUSs), i.e., agriculture, horticulture, and forestry, under major soil orders (entisol, inceptisol, and alfisol) in the Majha region of Punjab. A total of 225 depth-wise (at 0–20 cm, 20–40 cm, 40–60 cm, 60–80 cm and 80–100 cm) soil samples were c
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Miltenyi, Gregory P. L., Malte C. Ebach, and John Triantafilis. "Assessing the Australian Soil Classification using cladistic analysis." Soil Research 53, no. 7 (2015): 772. http://dx.doi.org/10.1071/sr14323.

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The Australian Soil Classification (ASC) has its roots in both the Handbook of Australian Soils and the Factual Key. The scheme’s use of mutually exclusive characteristics has led to Soil Orders containing a diverse range of soils, such as the Dermosols. The extent of these groupings has resulted in classes of soils sharing greater relationships with soils from other classes than they do with soils in the same class. Situations such as this arise from artificial classifications and highlight the need for natural classifications. Natural classifications accurately represent what is occurring in
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Basak, Nirmalendu, Ashim Datta, Tarik Mitran, et al. "Assessing soil-quality indices for subtropical rice-based cropping systems in India." Soil Research 54, no. 1 (2016): 20. http://dx.doi.org/10.1071/sr14245.

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Rice-based cropping systems are the foundation of food security in countries of Southeast Asia, but productivity of such systems has declined with deterioration in soil quality. These systems are different from other arable systems because rice is grown under submergence, and this may require a different set of key soil attributes for maintenances of quality and productivity. A minimum dataset was screened for assessing quality of soils belonging to three Soil Orders (Inceptisols, Entisols and Alfisols) by using statistical and mathematical models and 27 physical, chemical and biological attri
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Chen, L., and K. Tan. "ESTIMATION OF SOIL HEAVY METAL COMBINING FRACTIONAL ORDER DERIVATIVE." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLIII-B3-2020 (August 22, 2020): 1439–44. http://dx.doi.org/10.5194/isprs-archives-xliii-b3-2020-1439-2020.

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Abstract. It is important for the sustainable development of soil and monitoring the soil quality to obtain the heavy metal contents. Visible and near-infrared (Vis–NIR) spectroscopy provides an alternative method for soil heavy metal estimation. A total of 80 soil samples collected in Xuzhou city of China were utilized as data sets for calibration and validation to establish the relationship between the soil reflectance and soil heavy metal content. To amplify the weak spectral characteristic, improve the estimation ability, and explore the characteristic band regions, the preprocessing metho
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Wood, M., and A. M. Litterick. "Soil health - What should the doctor order?" Soil Use and Management 33, no. 2 (2017): 339–45. http://dx.doi.org/10.1111/sum.12344.

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Ling, Felix Ngee Leh, Khairul Anuar Kassim, Ahmad Tarmizi Abdul Karim, and Tze Wei Chan. "Stabilization of Artificial Organic Soil at Room Temperature Using Blended Lime Zeolite." Advanced Materials Research 723 (August 2013): 985–92. http://dx.doi.org/10.4028/www.scientific.net/amr.723.985.

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Organic content in soil is believed to inhibit formation of reaction products in lime stabilization which resulted in low gain of strength when dealing with organic soils. Zeolite, a kind of pozzolan with high CEC capacity is proposed to be use in this study in order to improve lime stabilization of organic soil. The effectiveness of blended lime zeolite in stabilization of organic soils was investigated by using two types of artificial organic soils with predetermined organic contents. Artificial organic soils were formed by mixing inorganic soil (commercial kaolin) with organic matter (comme
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Tarnocai, Charles, and James Bockheim. "Cryosolic soils of Canada: Genesis, distribution, and classification." Canadian Journal of Soil Science 91, no. 5 (2011): 749–62. http://dx.doi.org/10.4141/cjss10020.

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Tarnocai, C. and Bockheim, J. G. 2011. Cryosolic soils of Canada: Genesis, distribution, and classification. Can. J. Soil. Sci. 91: 749–762. Cryosols are permafrost-affected soils whose genesis is dominated by cryogenic processes, resulting in unique macromorphologies, micromorphologies, thermal characteristics, and physical and chemical properties. In addition, these soils are carbon sinks, storing high amounts of organic carbon collected for thousands of years. In the Canadian soil classification, the Cryosolic Order includes mineral and organic soils that have both cryogenic properties and
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Pozniak, Stepan, and Natalia Havrysh. "Social soil science as a new approach in soil science." Polish Journal of Soil Science 53, no. 1 (2020): 73. http://dx.doi.org/10.17951/pjss.2020.53.1.73.

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&lt;p&gt;The article contains the authors’ reflections on the formation and substantiation of many aspects in soil science, concerning its connections with social sciences. Arguments about the exceptional importance of soil resources in the modern world and the importance of scientific research in soil science, which can become an important instrument of solving social problems, are found. It is shown that soil resources, being the basis of agricultural development, are the long-term capital through which different nations exist and develop. In order to maintain the normal living conditions of
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Jamil, Norashira, Aziman Madun, Saiful Azhar Ahmad Tajudin, and Zaidi Embong. "An Overview of Electrokinetic Remediation Assisted Phytoremediation to Remediate Barren Acidic Soil." Applied Mechanics and Materials 773-774 (July 2015): 1476–80. http://dx.doi.org/10.4028/www.scientific.net/amm.773-774.1476.

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Electrokinetic has proven to be alternative technique to remediate pollution and increase soil strength for soft soil. This remediation method has been applied to remediate the hydrocarbon and heavy metal contaminant. Phytoremediation is a technique used to remediate the hydrocarbon and heavy metal contaminant. Both of this remediation technique has been proven as attractive alternative to clean up polluted soils. Although barren acidic soil is not categories as hazardous, the necessity of covered soil surface is on demand in order to minimize the surface erosion. Other than that, this remedia
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Ananko, T. V., M. I. Gerasimova, and D. E. Konyushkov. "PALE SOILS ON CARBONATE-FREE DEPOSITS IN CENTRAL SIBERIA AND THEIR TAXONOMIC POSITION IN THE SOIL CLASSIFICATION OF RUSSIA." Dokuchaev Soil Bulletin, no. 77 (March 1, 2015): 29–50. http://dx.doi.org/10.19047/0136-1694-2015-77-29-50.

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Based upon a comprehensive analysis of detailed descriptions of soil profiles and analytical data obtained by I. Sokolov, V. Zolnikov, L. Yelovskaya and other researchers, as well as upon data on the soil-forming factors, an attempt is made to determine the taxonomic level of pale undifferentiated neutral and slightly acid soils derived from carbonate-free deposits in the new classification system of Russian soils (versions 2004, 2008). The above group of soils is not uniform. According to their diagnostic morphological and physical-chemical properties the loamy permafrost-affected soils with
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Jing, Sun, Ma Xiu Lan, Wang Wen, Zhang Jing, Zhang Hao, and Wang Yu Jun. "Adsorption characteristics of atrazine on different soils in the presence of Cd(II)." Adsorption Science & Technology 38, no. 7-8 (2020): 225–39. http://dx.doi.org/10.1177/0263617420928845.

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In this study, the effects of temperature, pH, and biochar under cadmium stress on the adsorption characteristics of atrazine in soils in northeast China were studied by batch adsorption method. In the atrazine–Cd(II) coexistence system, the adsorption of atrazine by the soils reached equilibrium within 24 h, but there were some differences in sorption capacities of the three types of soil and the order of adsorption is albic soil &gt; black soil &gt; saline-alkaline soil. With the concentration of atrazine increased, the adsorption capacity of atrazine in the three types of soil gradually inc
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O., P. Bansal. "Effect of different organic material on lead adsorption in soils of Aligarh district." Journal of Indian Chemical Society Vol. 85, Jan 2008 (2008): 59–63. https://doi.org/10.5281/zenodo.5808536.

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Chemistry Department, D. S. College, Aligarh-202 001, Uttar Pradesh, India <em>E-mail :</em> drop31@rediffmail.com <em>Manuscript received 19 June 2006, revised 19 September 2007, accepted 25 September 2007</em> The effect of different organic material (FYM, sewage sludge and poultry litter) on adsorption-desorption of lead on three soil samples of Aligarh district was studied. The adsorption isotherms were of &#39;L&#39; type and adsorption-desorption data conformed to Freundlich isotherm equation. The adsorption increased with the increase in organic material and followed the order : sewage
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Altobelli, Filiberto, Ronald Vargas, Giuseppe Corti, et al. "Improving soil and water conservation and ecosystem services by sustainable soil management practices: From a global to an Italian soil partnership." Italian Journal of Agronomy 15, no. 4 (2020): 293–98. http://dx.doi.org/10.4081/ija.2020.1765.

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The UN Sustainable Development Goals (SDGs) identify the need to restore degraded soils in order to improve productivity and the provision of ecosystem services. The aim is to support food production, store and supply clean water, conserve biodiversity, sequester carbon, and improve soil resilience in a context of climate change. Within this framework, in order to achieve the SDGs and to correct land management in the long-term, soil management is considered mandatory. The reduction of land degradation should be based on various sustainable soil management practices that improve and maintain s
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Li, Qin. "Study on photodegradation of typical new brominated flame retardants on soil minerals and actual soil." E3S Web of Conferences 630 (2025): 01007. https://doi.org/10.1051/e3sconf/202563001007.

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The photodegradation process of hexabromobenzene (HBB) adsorbed on four soil minerals and actual soil was studied under simulated sunlight irradiation. The results showed that the photodegradation of HBB on all soils was in accordance with the pseudo-first-order kinetic process. In different soil types, the order of photodegradation rate from fast to slow was silica gel (simulated soil mineral system) &gt; montmorillonite &gt; kaolinite &gt; Sanya soil &gt; quartz sand &gt; Haikou soil. The higher the thickness of soil laying, the lower the photodegradation efficiency of HBB. The photodegradat
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Ouimet, Rock, Sylvie Tremblay, Catherine Périé, and Guy Prégent. "Ecosystem carbon accumulation following fallow farmland afforestation with red pine in southern Quebec." Canadian Journal of Forest Research 37, no. 6 (2007): 1118–33. http://dx.doi.org/10.1139/x06-297.

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We assessed the organic C stocks and inferred their changes in vegetation biomass, forest floor, and soil using a 50 year chronosequence of red pine ( Pinus resinosa Ait.) plantations established on postagricultural fields in southern Quebec, Canada. The data come from soil and tree field surveys carried out in the 1970s in 348 sites. Organic C concentrations were usually measured in three major mineral soil horizons; for the remaining soil horizons, they were estimated using pedotransfer functions. The effect of soil order, drainage, and texture was analysed. Over 22 years, organic C accumula
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Yong, Raymond N., and Yuwaree Phadungchewit. "pH influence on selectivity and retention of heavy metals in some clay soils." Canadian Geotechnical Journal 30, no. 5 (1993): 821–33. http://dx.doi.org/10.1139/t93-073.

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The problem of varying species of heavy metals existing as individual species or in combination with each other in simulated contaminant leachates (solutions) is studied in relation to selectivity and retention in four different kinds of soil. The influence of pH on the retention characteristics is also examined. The results obtained from the heavy metals single-species and composite-species adsorption tests indicate that in evaluating the attenuation potential of the soil substrate (i.e., contaminant attenuation), account needs to be given to the sensitivity of the soil – heavy metals contami
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Dudek, Michał, Beata Łabaz, Magdalena Bednik, and Agnieszka Medyńska-Juraszek. "Humic Substances as Indicator of Degradation Rate of Chernozems in South-Eastern Poland." Agronomy 12, no. 3 (2022): 733. http://dx.doi.org/10.3390/agronomy12030733.

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Unfavourable quantitative and qualitative changes of soil organic matter result from degradation processes, such as water erosion connected with intense arable land use. In order to take adequate preventive action, the proper indicators of soil quality or degradation are urgently needed. In particular, tests considering the soil organic matter quality seem to be beneficial for soil monitoring. In this paper, we performed organic matter fractionation using the Tyurin and IHSS procedures on eight profiles of chernozemic soils (non-degraded, eroded, forest and accumulative soils). The study condu
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Dinesh, Mani, and Kumar Mourya Vishv. "The depth wise enrichment of heavy metals (Cd, Pb, Cu, Zn) in sewage irrigated soils of Allahabad." Journal of Indian Chemical Society Vol. 90, May 2013 (2013): 699–702. https://doi.org/10.5281/zenodo.5772480.

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Sheila Dhar Institute of Soil Science, Department of Chemistry, University of Allahabad, Allahabad-211 002, Uttar Pradesh, India <em>E-mail </em>: vishv0007@gmail.com <em>Manuscript received 13 December 2011, revised 10 May 2012, accepted 11 July 2012</em> The depth wise enrichment of heavy metals (Cd, Pb, Cu and Zn) were studied in different profiles of sewage irrigated soils of Allahabad. The representative soil samples were collected from three different sites. The samples were collected from different depth, i.e. 0-10, 10-20, 20-30 and 30-40 cm. Maximum accumulation of heavy metals was obs
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Han, Guilin, Anton Eisenhauer, Jie Zeng, and Man Liu. "Calcium Biogeochemical Cycle in a Typical Karst Forest: Evidence from Calcium Isotope Compositions." Forests 12, no. 6 (2021): 666. http://dx.doi.org/10.3390/f12060666.

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In order to better constrain calcium cycling in natural soil and in soil used for agriculture, we present the δ44/40Ca values measured in rainwater, groundwater, plants, soil, and bedrock samples from a representative karst forest in SW China. The δ44/40Ca values are found to differ by ≈3.0‰ in the karst forest ecosystem. The Ca isotope compositions and Ca contents of groundwater, rainwater, and bedrock suggest that the Ca of groundwater primarily originates from rainwater and bedrock. The δ44/40Ca values of plants are lower than that of soils, indicating the preferential uptake of light Ca is
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