{"title":"Evolution of the lithospheric mantle under Boulaye volcano inferred from ultramafic lherzolite xenoliths (Adamawa plateau, Cameroon, Central Africa)","authors":"Sahabo Abobakar Abdoulaye, Okomo Atouba Lise Carole, Bardintzeff Jacques-Marie, Ombolo Auguste, Nkouandou Oumarou Faarouk, Fagny Mefire Aminatou, Adama Haman, Njankouo Ndassa Zénab Nouraan, Dourwe Dogsaye Pierre, Feukam Feuto Joël B., Niraka Voundou Dieudonné, Bonin Bernard, Pouclet André","doi":"10.1007/s12517-025-12224-2","DOIUrl":"10.1007/s12517-025-12224-2","url":null,"abstract":"<div><p>This paper presents new data on mineral chemistry of ultramafic xenoliths from the Boulaye volcanic area, Adamawa plateau in Central Africa. Modal composition (olivine + orthopyroxene + clinopyroxene + spinel + amphibole) indicates spinel lherzolite with protogranular and porphyroclastic textures. Electron microprobe mineral analyses show that olivine is high Fo with variable CaO contents, orthopyroxene is calcium enstatite, clinopyroxene is Cr-diopside and spinel is Cr-spinel. Variations of contents in some major elements exhibited by olivine, pyroxene and spinel denote increasingly large degrees of melt depletion, emphasizing the complex tectono-magmatic history of the Adamawa lithosphere mantle. Xenoliths are equilibrated between 1027 and 1102 °C within pressure range of 0.9 to 1.7 GPa at equilibrium depths of 30 to 56 km. Boulaye xenoliths stand as mantle residues whose evolution is governed by melt extraction process (5 to 20%) overprinted by Ti–rich metasomatic fluid and/or melt. The geodynamic settings involve a Pan-African subduction event prior to upwelling of Adamawa lithospheric mantle, due to Pan-African strike-slip fault activity at Tertiary times.</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 5","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143861415","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Faisal Rehman, Helmy S. O. Abuelnaga, Hussein M. Harbi, Tahir Azeem, Jamil Siddique, Omar Riaz, Muhammad Fahad Ullah, Faisal Rehman
{"title":"Integrated geophysical and hydrogeological techniques for environmental monitoring and assessment: a case study for waste disposal site, Jeddah Saudi, Arabia","authors":"Faisal Rehman, Helmy S. O. Abuelnaga, Hussein M. Harbi, Tahir Azeem, Jamil Siddique, Omar Riaz, Muhammad Fahad Ullah, Faisal Rehman","doi":"10.1007/s12517-025-12245-x","DOIUrl":"10.1007/s12517-025-12245-x","url":null,"abstract":"<div><p>Environmental problems are inevitable phenomena for worldwide. Nowadays in multidisciplinary research era, integrated geophysical techniques are commonly applied for environmental monitoring and assessment along with other techniques. Waste disposal is an alarming problem and causes a lot of environmental issue. In Jeddah City, residential and industrial waste was deposited without treatment et al. Misk (Buraiman) Lake. Geophysical and hydrological investigations were carried out to identify and monitor extent of the contamination in the subsurface. Geophysical techniques comprised of electromagnetic induction and electrical resistivity methods. The hydrogeological investigations included water sample analysis. High electrical conductivity values were observed along the plume compared to the surroundings. The results of the electromagnetic survey, electrical resistivity and water samples were correlated and found in good agreement. The contamination was found in most of the areas with varying concentration levels. The study revives that integrating geophysical techniques with hydrogeological studies eases to map the groundwater contamination.\u0000</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 5","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143856631","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Njifontawouo Ouzerou Mimche, Anatole Eugene Djieto Lordon, Charles Antoine Basseka, Christ Alain Nekuie Mouafo, Yannick Stephan Kengne
{"title":"Application of remote sensing in the identification and analysis of lineaments for groundwater exploration using Landsat-8 Oli and SRTM data in Ebolowa and environs","authors":"Njifontawouo Ouzerou Mimche, Anatole Eugene Djieto Lordon, Charles Antoine Basseka, Christ Alain Nekuie Mouafo, Yannick Stephan Kengne","doi":"10.1007/s12517-025-12249-7","DOIUrl":"10.1007/s12517-025-12249-7","url":null,"abstract":"<div><p>This research aimed to identify and analyse lineaments for groundwater exploration and delineate possible zones for groundwater exploitation. To achieve this, Landsat-8 OLI spectral bands as well as SRTM data covering the study area were obtained from the United States Geological Survey (USGS) website, from which fracture maps were produced. The extraction method of lineaments from remote sensing data required some pre-processing of the Landsat satellite image spectral bands to reduce the effect of the atmosphere and geometric distortions during data acquisition. The automatic lineament extraction was performed with the PCI Geomatica 2016 software for Landsat images and manually for SRTM on ArcGIS. Automatic lineament extraction was applied to the PC1 and PC2 bands of the Landsat-8 OLI image and each of the four shaded relief images of the SRTM images (N0°, N45°, N90°, and N135°). The results reveal 909 lineaments ranging from 21 m to 10.1 km, with an average length of 1.98 km and a standard deviation of 1.27. The lineaments on directional maps and rose diagrams show 8 directions with the predominance NE-SW. The secondary directions are NW–SE and WNW-ESE. The results are validated by the structural data measured in the field, the geological map of Cameroon, the hydrographic network, and the slope map. The results show an important role played by fractures in the occurrence of underground water in the study area. All this has enabled us to identify and characterise the potential areas for groundwater exploitation.\u0000</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 5","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143821780","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"New constraints on tectonic inversion–based Orogeny of Western Kopet-dagh (NE of Iran)","authors":"Rezvaneh Hamidi, Hojjat Ollah Safari, Arash Amini","doi":"10.1007/s12517-025-12253-x","DOIUrl":"10.1007/s12517-025-12253-x","url":null,"abstract":"<div><p>One of the orogen types in the intra-continental tectonic settings is pop-up structures with bi-vergent thrust tectonics. In this research, the western part of the Kopet-dagh Orogen, as the southern boundary of the Turan Plate, is selected as a case study for investigation on tectonic development and deformation patterns, using surface–subsurface structural studies together with complementary remote sensing and GIS environmental capability as a multi-disciplinary approach. The results of this research determined two sets of faults, consisting of (a) first-stage longitudinal reverse faults with a structural trend of N90–100 to N50–70 (Tangrah, Takal-Kuh, Marave-Tappe, and Golijeh faults), and (b) transversal right-hand strike-slip faults with a trend of N130–150 (Kalaleh, Ughcheh, and Sarighamish faults). These two sets of faults formed the structural framework of this zone and played an important role in the tectonic evolution (initiation, shaping, evolution of sedimentary basins, and forming a fold-thrust belt) of this orogen. A change in the mechanism of the first-stage longitudinal faults, as tectonic inversion, at the onset of the Late Alpine Orogeny caused the re-arrangement of P-axes and thus formed bi-vergent reverse faulting in the northern and southern edges of this zone. Subsequently, fault propagation folds were established due to this event. Finally, an extensive V-shaped compressional pop-up structure with bi-vergent thrusting and fold axial surfaces (as fault-related folds) was formed in the Kopet-dagh fold-thrust belt. Also, the mechanism of the second-stage transversal faults changed to right-hand strike-slip faults with some normal components at the onset of the Late Alpine Orogeny. The normal component of these faults (especially the Kalaleh fault) caused the settlement of the western part of this zone along them and formed the Gorgan-Gonbad plain.</p><h3>Graphical abstract</h3><div><figure><div><div><picture><source><img></source></picture></div></div></figure></div></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 5","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143821779","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Investigation of the effect of climatic parameters in machine learning algorithms for streamflow predicting in Hamoon Helmand Catchment, Iran","authors":"Shabnam Vakili, Seyyed Morteza Mousavi","doi":"10.1007/s12517-025-12243-z","DOIUrl":"10.1007/s12517-025-12243-z","url":null,"abstract":"<div><p> The objective of this study is to identify the effective input parameters for estimating streamflow using an M5 model tree and Genetic Algorithm (GA) and Long Short-Term Memory (LSTM) and to propose a dependable model. These methods were chosen for their ability to model complex relationships, high prediction accuracy, and efficient input optimization capabilities. The study utilized monthly data of rainfall, temperature, evaporation, and streamflow for the latest month (Q<sub>t-1</sub>) and the preceding 2 months (Q<sub>t-2</sub>) in the Hamoon Helmand catchment. Five scenarios were employed in M5 and the linear and nonlinear models of GA and LSTM. The models’ performance was assessed using statistical parameters such as RMSE, MAE, R, and NSE. In the initial scenario where all five parameters were considered, M5, the linear and nonlinear GA models and LSTM produced the most accurate results, with RMSE values of 9.27, 6.87, 5.54, and 5.55, respectively. The second scenario (rainfall; maximum, minimum, and average temperatures; Q<sub>t-1</sub> (discharge for 1 month before) and evaporation) revealed that the linear and nonlinear GA models, with RMSE values of 7.21 and 6.55, respectively, were more accurate than M5 and LSTM with an RMSE value of 8.58 and 6.78, respectively. In Scenarios 3 (rainfall; average temperatures; evaporation; and Q<sub>t-1</sub>, Q<sub>t-2</sub> (discharge for 1, 2 months before)) and 4 (rainfall; average temperatures; Q<sub>t-1</sub>, Q<sub>t-2</sub> (discharge for 1, 2 months before)), LSTM demonstrated superior performance. The results obtained from Scenario 5 (rainfall; maximum, minimum, and average temperatures and evaporation) indicate that in the absence of sufficient runoff data in a basin, there is no necessity to employ a nonlinear model; instead, modeling with an M5 model tree yields sufficiently accurate results. This research demonstrates the global significance of optimizing water resource management models in arid and climate-sensitive regions and contributes to the resilience and sustainability of resources in the face of climate change.</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 5","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143801171","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Distribution of organochlorine pesticides and diuron (urea pesticide) in the sediments of Prydz Bay, East Antarctica","authors":"Princy Mundackal John, Vellorkirakathil Narayana Sanjeevan, Anil Kumar Narayanapillai, Anu Gopinath","doi":"10.1007/s12517-025-12247-9","DOIUrl":"10.1007/s12517-025-12247-9","url":null,"abstract":"<div><p>This study provides crucial insights into the extent and impact of human activity on Antarctic ecosystems by shedding light on previously unexplored contamination patterns in one of the earth’s most pristine environments. In modern periods, several pesticides have been developed worldwide, applied, and released into the environment. As a result, information regarding occurrence patterns and spatial variability is limited to easily accessible regions, and only a finite number of research have been published from the remote Antarctic region. Seven surface sediments were collected from Prydz Bay, East Antarctica, by which four organochlorine pesticides (OCPs) were detected along with the presence of a herbicide diuron. The concentration of diuron (range BDL-16.57 ng/g) is several times higher than other OCPs. In the case of OCPs, the highest concentrations were for p,p′ DDD (BDL-0.42 ng/g), followed by dichloran (BDL-0.17 ng/g), BHC β (BDL-0.09 ng/g), and then HCB (BDL-0.02 ng/g).\u0000</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 4","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143749168","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Experimental study on the effect of stress and water content on resilient modulus of unsaturated subgrade soil: implications for pavement design","authors":"Mulugeta Damtew Amare, Tompai Zoltan, Lemlem Abebaw Asaye, Yasir Mahmood","doi":"10.1007/s12517-025-12246-w","DOIUrl":"10.1007/s12517-025-12246-w","url":null,"abstract":"<div><p>Subgrade soils possess essential mechanical properties that influence the load-bearing capacity and deformation behavior of pavements. This directly impacts pavement structural performance and longevity. This paper presents the experimental results on determining the factors affecting the resilient modulus (Mr) of a subgrade soil as determined by the triaxial loading machine. A silty sand subgrade soil, tested in its unsaturated form to represent site conditions, was subjected to characterization and cyclic loading tests. The variables considered for this research are deviatoric and constant stress, confining stress, and water content. The Mr is highly dependent on the deviatoric stress, confining pressure, and water content. The shear stress test result at the end of each cyclic loading shows that the soils at the optimum water content level show better shear resistance and elastic deformation below certain stress levels. In contrast, soils in the other moisture levels show complete plastic deformation. Moreover, while confining stress enhances Mr, deviatoric stress reduces it.\u0000</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 4","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-03-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s12517-025-12246-w.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143707066","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Sobhi Nasir, Kamal Noori Khankahdani, Abdel Rahman Nasir
{"title":"Geochemical and petrological characterization of listwaenite from Oman and Iran ophiolites: implications for hydrothermal carbonation and silicification alteration processes","authors":"Sobhi Nasir, Kamal Noori Khankahdani, Abdel Rahman Nasir","doi":"10.1007/s12517-025-12244-y","DOIUrl":"10.1007/s12517-025-12244-y","url":null,"abstract":"<div><p>Listwaenites (carbonated/silicified ultramafic rocks) are widely spread in the Semail Ophiolite of Oman, mainly in Fanja rea and in Islam Abad area of the Neyriz Ophiolite of Iran. Listwaenite is gaining worldwide interest due to their possible economic value as gold bearing rocks and assessing the global carbon sequestration and flux. This work presents new petrographic and geochemical data of listwaenite from Fanja and Islam Abad area and estimates the physical and chemical conditions of their formation. Three types of listwaenite are known to occur within ophiolites worldwide, and these include silica-, carbonate-, and silica-carbonate. Typical minerals which are usually known to occur in these listwaenite include dolomite, ankerite, calcite, magnesite, quartz, iron oxides, relict chromite grains ± talc and serpentine. Calcite- and magnesite-dolomite listwaenite is more abundant in the Fanja area, while dolomite listwaenite is more abundant in Islam Abad area. The major element chemistry of the different types of listwaenite in both Fanja and Islam Abad area is largely similar to that of altered ultramafic rocks and listwaenites from other ophiolites occurrences. In comparison to the primary mantle and chondrite spider diagrams, the Islam Abad listwaenite shows higher trace and REE elements abundance than those from the Fanja area. The variable and high abundances of Ca, Mg, Ba, Zr, Sr, Pb, Zn, Mo, and W in the carbonate- and silica-carbonate listwaenite indicate a hydrothermal source from the sedimentary and metamorphic units of the Arabian Platform underlaying the listwaenite. Depletion and enrichment of major and trace elements in the listwaenite are indicative of large fluctuations in major and trace element mobility, where listwaenite preserves different stages of gradual alteration of their ultramafic protoliths. The listwaenite content of CaO, SiO<sub>2</sub>, and MgO depends on the stage of listwaenite formation, in which carbonate listwaenite is formed in the first stage, progressing to silica-carbonate listwaenite in the final stage. The listwaenite in Islam Abad and Fanja area was altered to different stages by hydrothermal alteration of serpentinite and harzburgite along Late Cretaceous thrust and Paleocene-Miocene extensional faults and shear zones, which acted as pathway for trace elements and Ca and/or Si rich fluids at different times probably during subduction and/or post obduction stages.</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 4","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-03-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143688287","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Improving iron ore blending using radial basis function neural network (RBFNN) for enhanced steel production in Egypt","authors":"Hamdy A. M. Sayedahmed","doi":"10.1007/s12517-025-12209-1","DOIUrl":"10.1007/s12517-025-12209-1","url":null,"abstract":"<div><p>Ores are vital to the economies of developing countries, significantly contributing to growth and industrialization. In Egypt, iron ore is particularly impactful, forming the backbone of the country’s mineral sector. Among the stages of iron processing, blending is crucial as it directly affects the final quality of the processed iron. Currently, blending is done manually by mineral researchers who analyze samples, set blending specifications, and create blends, often compromising the overall quality. This study proposes the use of an artificial neural network (ANN) model, specifically the radial basis function neural network (RBFNN), to classify blend quality in Egypt’s Aswan region. The model, powered by the radial basis function (RBF), efficiently handles large datasets and reduces the costs of achieving optimal blending. Using expert-judged “best blend” data for analysis and prediction, the RBFNN model demonstrates superior performance in terms of accuracy, precision, recall, and F1 score compared to traditional methods. Additionally, a thorough analysis of iron ores was conducted during deployment, confirming the model’s effectiveness in identifying and improving blend quality.</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 4","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-03-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143688556","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Prashant Shriram Wagh, Ravishankar Kumar, Sanjeev Bhasin, Pawan Pal
{"title":"Chemometric quantification of trace element impurities within kaolin and talc white clay minerals in Kutch and Banas-Mahi basin, India","authors":"Prashant Shriram Wagh, Ravishankar Kumar, Sanjeev Bhasin, Pawan Pal","doi":"10.1007/s12517-025-12242-0","DOIUrl":"10.1007/s12517-025-12242-0","url":null,"abstract":"<div><p>The unique properties of kaolin-talc white clays such as hydration, plasticity, rheological, color, and adsorption capacities are affected by the existence of elemental/trace metal impurities. A systematic and comprehensive study regarding elemental/trace metal impurities in kaolin and talc is lacking. Thus, the present study investigated elemental impurities in kaolin and talc and their source apportionment pattern. For this concern, a total of 50 kaolin samples from the Bhuj area of the Kutch basin (Gujarat, India) and 30 talc samples from the Mahi-Banas basin of Rajasthan (Bhilwara, Udaipur, and Dungarpur) were analyzed. The major trace element impurities such as lead (Pb), chromium (Cr), copper (Cu), nickel (Ni), arsenic (As), manganese (Mn), and zinc (Zn) were detected in kaolin-talc clays from inductively coupled plasma optical emission spectrometry (ICP-OES) technique. Further, the source apportionment study was carried out by using multivariate analyses such as principal component analysis (PCA), hierarchical cluster analysis (HCA), and Pearson correlation matrix (PCM). The results indicated that the mean concentrations of trace elements Cr, Pb, Mn, Ni, Zn, Cu, and As in kaolin were 114, 57.82, 33.31, 20.36, 16.51, 10.98, and 0.05 mg/kg, respectively, whereas 2.53, 0.63, 159, 5.05, 20.11, 1.22, and 11.23 mg/kg, correspondingly, in talc samples. However, the toxic elemental impurity level was low as compared to Indian and European Union standards for soils. The present study explores the existence of major trace elemental impurities in kaolin-talc clays. Furthermore, the multivariate analyses described that the major sources of existing elemental impurities are attributed as being from different geogenic sources.</p></div>","PeriodicalId":476,"journal":{"name":"Arabian Journal of Geosciences","volume":"18 4","pages":""},"PeriodicalIF":1.827,"publicationDate":"2025-03-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143676473","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}