SOIL DISTRIBUTION IN STRUMICA RIVER BASIN AND ITS IMPORTANCE FOR AGRICULTURAL PRODUCTION
[...]they have varied effects on agricultural production. [...]soils of the plains occupy 17.784,4 ha (12.01%) and Urbisol 1.755,57 ha (1.18%). [...]they have varied effects on agricultural production. The soils on this terrain (relief) form have the following common properties: a) very pronounced e...
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description | [...]they have varied effects on agricultural production. [...]soils of the plains occupy 17.784,4 ha (12.01%) and Urbisol 1.755,57 ha (1.18%). [...]they have varied effects on agricultural production. The soils on this terrain (relief) form have the following common properties: a) very pronounced erosion (occurrence of Regosols and erosion of horizon A or part thereof, in the soils with A-C, A-(B)-C and A-E-B-C profile type); b) absence of compact rocks as substrate and soil genesis over clastic sediments, resulting in deep solum and physiologically active profiles; c) greater presence of clay resulting from the substrate or the argilogenesis within the profile; d) presence of smectites in some soils (Vertisols) arising mainly from the substrate and partially from the soil genesis, and in relation to that, deterioration of the physical properties of the soils; e) occurrence of textural differentiation at some soils (Vertisols and Albic Luvisols), and in relation to that, deterioration of the physical properties; f) greater presence of the silicate - carbonate substrate in the soil genesis, in comparison to the substrate of the mountainous terrains; g) relative dryness of the soils (which is lower at the lake terraces), caused from insufficient quantity of rainfalls, surface water flow and very deep underground water; e) insufficient quantity of humus and nutrients (especially N and P); f) relatively good chemical properties (the high content of carbonates of Humic Calcaric Regosols and the acidity of the Albic Luvisols are an exception). In order to increase their productive ability, the following joint measures should be undertaken according to relief forms: - Joint measures for soils from mountain terrains: (protection from erosion, fertilization with organic and mineral fertilizers, proper tillage, liming if necessary); - Joint measures for soils from lake terraces and undulating-hilly terrains: (deep tillage, humization: organic fertilizers and phytomeliorations, intensive use of mineral fertilizers N and P2O5, and for plants that need potassium during the entire year and for obtaining much higher yields and K-fertilizers, anti-erosion measures, proper irrigation method); - Joint measures for soils from sloping terrains: (anti-erosion protection measures, irrigation, humization, intensive use of mineral fertilizers); - Joint measures for soils from plain terrains: (regulation of the water regimen, lowering of the level of underground water-drainage, t |
doi_str_mv | 10.17707/AgricultForest.64.4.14 |
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[...]soils of the plains occupy 17.784,4 ha (12.01%) and Urbisol 1.755,57 ha (1.18%). [...]they have varied effects on agricultural production. The soils on this terrain (relief) form have the following common properties: a) very pronounced erosion (occurrence of Regosols and erosion of horizon A or part thereof, in the soils with A-C, A-(B)-C and A-E-B-C profile type); b) absence of compact rocks as substrate and soil genesis over clastic sediments, resulting in deep solum and physiologically active profiles; c) greater presence of clay resulting from the substrate or the argilogenesis within the profile; d) presence of smectites in some soils (Vertisols) arising mainly from the substrate and partially from the soil genesis, and in relation to that, deterioration of the physical properties of the soils; e) occurrence of textural differentiation at some soils (Vertisols and Albic Luvisols), and in relation to that, deterioration of the physical properties; f) greater presence of the silicate - carbonate substrate in the soil genesis, in comparison to the substrate of the mountainous terrains; g) relative dryness of the soils (which is lower at the lake terraces), caused from insufficient quantity of rainfalls, surface water flow and very deep underground water; e) insufficient quantity of humus and nutrients (especially N and P); f) relatively good chemical properties (the high content of carbonates of Humic Calcaric Regosols and the acidity of the Albic Luvisols are an exception). In order to increase their productive ability, the following joint measures should be undertaken according to relief forms: - Joint measures for soils from mountain terrains: (protection from erosion, fertilization with organic and mineral fertilizers, proper tillage, liming if necessary); - Joint measures for soils from lake terraces and undulating-hilly terrains: (deep tillage, humization: organic fertilizers and phytomeliorations, intensive use of mineral fertilizers N and P2O5, and for plants that need potassium during the entire year and for obtaining much higher yields and K-fertilizers, anti-erosion measures, proper irrigation method); - Joint measures for soils from sloping terrains: (anti-erosion protection measures, irrigation, humization, intensive use of mineral fertilizers); - Joint measures for soils from plain terrains: (regulation of the water regimen, lowering of the level of underground water-drainage, tillage and creating a deep fallow, fertilization with mineral and organic fertilizers with previous soil fertility control, proper irrigation).</description><identifier>ISSN: 0554-5579</identifier><identifier>EISSN: 1800-9492</identifier><identifier>DOI: 10.17707/AgricultForest.64.4.14</identifier><language>eng</language><publisher>Titograd: University of Montenegro, Biotechnical Faculty</publisher><subject>Acidity ; Agricultural production ; Agrochemicals ; Carbonates ; Chemical properties ; Clay minerals ; Decomposing organic matter ; Depth profiling ; Deterioration ; Fertilization ; Fertilizers ; Geography ; Humus ; Irrigation ; Laboratories ; Lakes ; Liming ; Mineral fertilizers ; Mineralogy ; Nutrients ; Organic chemistry ; Organic fertilizers ; Phosphorus pentoxide ; Physical properties ; Potassium ; River basins ; Rivers ; Sediments ; Smectites ; Soil erosion ; Soil fertility ; Soil formation ; Soil properties ; Substrates ; Surface water ; Taxonomy ; Terraces ; Tillage ; Vegetation ; Vertisols ; Water flow</subject><ispartof>Poljoprivreda i šumarstvo, 2018-12, Vol.64 (4), p.121</ispartof><rights>2018. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,861,27905,27906</link.rule.ids></links><search><creatorcontrib>MARKOSKI, Mile</creatorcontrib><creatorcontrib>MITKOVA, Tatjana</creatorcontrib><creatorcontrib>TANASKOVIK, Vjekoslav</creatorcontrib><creatorcontrib>SPALEVIC, Velibor</creatorcontrib><title>SOIL DISTRIBUTION IN STRUMICA RIVER BASIN AND ITS IMPORTANCE FOR AGRICULTURAL PRODUCTION</title><title>Poljoprivreda i šumarstvo</title><description>[...]they have varied effects on agricultural production. [...]soils of the plains occupy 17.784,4 ha (12.01%) and Urbisol 1.755,57 ha (1.18%). [...]they have varied effects on agricultural production. The soils on this terrain (relief) form have the following common properties: a) very pronounced erosion (occurrence of Regosols and erosion of horizon A or part thereof, in the soils with A-C, A-(B)-C and A-E-B-C profile type); b) absence of compact rocks as substrate and soil genesis over clastic sediments, resulting in deep solum and physiologically active profiles; c) greater presence of clay resulting from the substrate or the argilogenesis within the profile; d) presence of smectites in some soils (Vertisols) arising mainly from the substrate and partially from the soil genesis, and in relation to that, deterioration of the physical properties of the soils; e) occurrence of textural differentiation at some soils (Vertisols and Albic Luvisols), and in relation to that, deterioration of the physical properties; f) greater presence of the silicate - carbonate substrate in the soil genesis, in comparison to the substrate of the mountainous terrains; g) relative dryness of the soils (which is lower at the lake terraces), caused from insufficient quantity of rainfalls, surface water flow and very deep underground water; e) insufficient quantity of humus and nutrients (especially N and P); f) relatively good chemical properties (the high content of carbonates of Humic Calcaric Regosols and the acidity of the Albic Luvisols are an exception). In order to increase their productive ability, the following joint measures should be undertaken according to relief forms: - Joint measures for soils from mountain terrains: (protection from erosion, fertilization with organic and mineral fertilizers, proper tillage, liming if necessary); - Joint measures for soils from lake terraces and undulating-hilly terrains: (deep tillage, humization: organic fertilizers and phytomeliorations, intensive use of mineral fertilizers N and P2O5, and for plants that need potassium during the entire year and for obtaining much higher yields and K-fertilizers, anti-erosion measures, proper irrigation method); - Joint measures for soils from sloping terrains: (anti-erosion protection measures, irrigation, humization, intensive use of mineral fertilizers); - Joint measures for soils from plain terrains: (regulation of the water regimen, lowering of the level of underground water-drainage, tillage and creating a deep fallow, fertilization with mineral and organic fertilizers with previous soil fertility control, proper irrigation).</description><subject>Acidity</subject><subject>Agricultural production</subject><subject>Agrochemicals</subject><subject>Carbonates</subject><subject>Chemical properties</subject><subject>Clay minerals</subject><subject>Decomposing organic matter</subject><subject>Depth profiling</subject><subject>Deterioration</subject><subject>Fertilization</subject><subject>Fertilizers</subject><subject>Geography</subject><subject>Humus</subject><subject>Irrigation</subject><subject>Laboratories</subject><subject>Lakes</subject><subject>Liming</subject><subject>Mineral fertilizers</subject><subject>Mineralogy</subject><subject>Nutrients</subject><subject>Organic chemistry</subject><subject>Organic fertilizers</subject><subject>Phosphorus pentoxide</subject><subject>Physical properties</subject><subject>Potassium</subject><subject>River basins</subject><subject>Rivers</subject><subject>Sediments</subject><subject>Smectites</subject><subject>Soil erosion</subject><subject>Soil fertility</subject><subject>Soil formation</subject><subject>Soil properties</subject><subject>Substrates</subject><subject>Surface water</subject><subject>Taxonomy</subject><subject>Terraces</subject><subject>Tillage</subject><subject>Vegetation</subject><subject>Vertisols</subject><subject>Water flow</subject><issn>0554-5579</issn><issn>1800-9492</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNpVkEtPwzAQhC0EEhX0N2CJc4Lfjo9p-sBSmlROgrhZeaJWhRanPfDvMZQLe1ntavTNaAB4wCjEUiL5FL-5bXven5YH14-nULCQhZhdgQmOEAoUU-QaTBDnLOBcqlswHccd8iMZoghPwGuR6xTOdVEaPatKnWdQZ9Bf1VonMTT6ZWHgLC78M87mUJcF1OtNbso4SxZwmRsYr4xOqrSsTJzCjcnnVfKDuQc3Q70f--nfvgPVclEmz0Garzw5DVpMfCollCKib-qGRpxiQepaKk6ihklBZYO6puNkoG3NurprGWkU5oOgUTuIruddR-_A44V7dIfPs-_A7g5n9-EtLcHCe3DGiVfJi6p1h3F0_WCPbvteuy-Lkf1t0v5v0gpmmcWMfgMwdmOT</recordid><startdate>20181215</startdate><enddate>20181215</enddate><creator>MARKOSKI, Mile</creator><creator>MITKOVA, Tatjana</creator><creator>TANASKOVIK, Vjekoslav</creator><creator>SPALEVIC, Velibor</creator><general>University of Montenegro, Biotechnical Faculty</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>BYOGL</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>M0K</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20181215</creationdate><title>SOIL DISTRIBUTION IN STRUMICA RIVER BASIN AND ITS IMPORTANCE FOR AGRICULTURAL PRODUCTION</title><author>MARKOSKI, Mile ; MITKOVA, Tatjana ; TANASKOVIK, Vjekoslav ; SPALEVIC, Velibor</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1254-969926ebab3853162aa79528b47637b0dbd52f3ca4dadc42b915f638cf6de5dd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Acidity</topic><topic>Agricultural production</topic><topic>Agrochemicals</topic><topic>Carbonates</topic><topic>Chemical properties</topic><topic>Clay minerals</topic><topic>Decomposing organic matter</topic><topic>Depth profiling</topic><topic>Deterioration</topic><topic>Fertilization</topic><topic>Fertilizers</topic><topic>Geography</topic><topic>Humus</topic><topic>Irrigation</topic><topic>Laboratories</topic><topic>Lakes</topic><topic>Liming</topic><topic>Mineral fertilizers</topic><topic>Mineralogy</topic><topic>Nutrients</topic><topic>Organic chemistry</topic><topic>Organic fertilizers</topic><topic>Phosphorus pentoxide</topic><topic>Physical properties</topic><topic>Potassium</topic><topic>River basins</topic><topic>Rivers</topic><topic>Sediments</topic><topic>Smectites</topic><topic>Soil erosion</topic><topic>Soil fertility</topic><topic>Soil formation</topic><topic>Soil properties</topic><topic>Substrates</topic><topic>Surface water</topic><topic>Taxonomy</topic><topic>Terraces</topic><topic>Tillage</topic><topic>Vegetation</topic><topic>Vertisols</topic><topic>Water flow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>MARKOSKI, Mile</creatorcontrib><creatorcontrib>MITKOVA, Tatjana</creatorcontrib><creatorcontrib>TANASKOVIK, Vjekoslav</creatorcontrib><creatorcontrib>SPALEVIC, Velibor</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>East Europe, Central Europe Database</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Agricultural Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><jtitle>Poljoprivreda i šumarstvo</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>MARKOSKI, Mile</au><au>MITKOVA, Tatjana</au><au>TANASKOVIK, Vjekoslav</au><au>SPALEVIC, Velibor</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>SOIL DISTRIBUTION IN STRUMICA RIVER BASIN AND ITS IMPORTANCE FOR AGRICULTURAL PRODUCTION</atitle><jtitle>Poljoprivreda i šumarstvo</jtitle><date>2018-12-15</date><risdate>2018</risdate><volume>64</volume><issue>4</issue><spage>121</spage><pages>121-</pages><issn>0554-5579</issn><eissn>1800-9492</eissn><abstract>[...]they have varied effects on agricultural production. [...]soils of the plains occupy 17.784,4 ha (12.01%) and Urbisol 1.755,57 ha (1.18%). [...]they have varied effects on agricultural production. The soils on this terrain (relief) form have the following common properties: a) very pronounced erosion (occurrence of Regosols and erosion of horizon A or part thereof, in the soils with A-C, A-(B)-C and A-E-B-C profile type); b) absence of compact rocks as substrate and soil genesis over clastic sediments, resulting in deep solum and physiologically active profiles; c) greater presence of clay resulting from the substrate or the argilogenesis within the profile; d) presence of smectites in some soils (Vertisols) arising mainly from the substrate and partially from the soil genesis, and in relation to that, deterioration of the physical properties of the soils; e) occurrence of textural differentiation at some soils (Vertisols and Albic Luvisols), and in relation to that, deterioration of the physical properties; f) greater presence of the silicate - carbonate substrate in the soil genesis, in comparison to the substrate of the mountainous terrains; g) relative dryness of the soils (which is lower at the lake terraces), caused from insufficient quantity of rainfalls, surface water flow and very deep underground water; e) insufficient quantity of humus and nutrients (especially N and P); f) relatively good chemical properties (the high content of carbonates of Humic Calcaric Regosols and the acidity of the Albic Luvisols are an exception). In order to increase their productive ability, the following joint measures should be undertaken according to relief forms: - Joint measures for soils from mountain terrains: (protection from erosion, fertilization with organic and mineral fertilizers, proper tillage, liming if necessary); - Joint measures for soils from lake terraces and undulating-hilly terrains: (deep tillage, humization: organic fertilizers and phytomeliorations, intensive use of mineral fertilizers N and P2O5, and for plants that need potassium during the entire year and for obtaining much higher yields and K-fertilizers, anti-erosion measures, proper irrigation method); - Joint measures for soils from sloping terrains: (anti-erosion protection measures, irrigation, humization, intensive use of mineral fertilizers); - Joint measures for soils from plain terrains: (regulation of the water regimen, lowering of the level of underground water-drainage, tillage and creating a deep fallow, fertilization with mineral and organic fertilizers with previous soil fertility control, proper irrigation).</abstract><cop>Titograd</cop><pub>University of Montenegro, Biotechnical Faculty</pub><doi>10.17707/AgricultForest.64.4.14</doi><oa>free_for_read</oa></addata></record> |
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subjects | Acidity Agricultural production Agrochemicals Carbonates Chemical properties Clay minerals Decomposing organic matter Depth profiling Deterioration Fertilization Fertilizers Geography Humus Irrigation Laboratories Lakes Liming Mineral fertilizers Mineralogy Nutrients Organic chemistry Organic fertilizers Phosphorus pentoxide Physical properties Potassium River basins Rivers Sediments Smectites Soil erosion Soil fertility Soil formation Soil properties Substrates Surface water Taxonomy Terraces Tillage Vegetation Vertisols Water flow |
title | SOIL DISTRIBUTION IN STRUMICA RIVER BASIN AND ITS IMPORTANCE FOR AGRICULTURAL PRODUCTION |
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