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Grazing effects of the bulk density in a Natraquoll of the flooding pampa of Argentina
The influence of grazing by cattle on soil bulk density was studied in a typic Natraquoll of the Flooding Pampa of Argentina for a period of 33 months, by comparing a grazed situation to an enclosure deferred from grazing for 7 years. Floods took place in this period as usual. Bulk density (BD) at -...
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| Published in: | Journal of range management 1988-11, Vol.41 (6), p.500-503 |
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| Main Authors: | , |
| Format: | Article |
| Language: | English |
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| container_end_page | 503 |
| container_issue | 6 |
| container_start_page | 500 |
| container_title | Journal of range management |
| container_volume | 41 |
| creator | Taboada, M.A Lavado, R.S |
| description | The influence of grazing by cattle on soil bulk density was studied in a typic Natraquoll of the Flooding Pampa of Argentina for a period of 33 months, by comparing a grazed situation to an enclosure deferred from grazing for 7 years. Floods took place in this period as usual. Bulk density (BD) at -33.3 kPa of water retention varied from 1.00 to 1.11 Mg m-3in the ungrazed soil and in the grazed soil from 1.04 to 1.16 Mg m-3. Environmental factors were the primary agent controlling BD; only in some periods were there significant differences between treatments. Slight increases in BD occurred under grazing after the recession of the flood water, and significant decreases occurred in the ungrazed soil during the large and sudden falls in water content. In this case the effect of trampling, therefore, would consist mainly of impeding the decrease in BD. No compaction was observed in periods when no flood occurred or while soil remained submerged in water. The results indicated that the variations of bulk density caused by cattle trampling were superimposed on those produced by floods and showed an interaction between the effects of land-use and the particular environmental conditions of the region. |
| doi_str_mv | 10.2307/3899526 |
| format | article |
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Floods took place in this period as usual. Bulk density (BD) at -33.3 kPa of water retention varied from 1.00 to 1.11 Mg m-3in the ungrazed soil and in the grazed soil from 1.04 to 1.16 Mg m-3. Environmental factors were the primary agent controlling BD; only in some periods were there significant differences between treatments. Slight increases in BD occurred under grazing after the recession of the flood water, and significant decreases occurred in the ungrazed soil during the large and sudden falls in water content. In this case the effect of trampling, therefore, would consist mainly of impeding the decrease in BD. No compaction was observed in periods when no flood occurred or while soil remained submerged in water. The results indicated that the variations of bulk density caused by cattle trampling were superimposed on those produced by floods and showed an interaction between the effects of land-use and the particular environmental conditions of the region.</description><identifier>ISSN: 0022-409X</identifier><identifier>EISSN: 2162-2728</identifier><identifier>DOI: 10.2307/3899526</identifier><language>eng</language><publisher>Society for Range Management</publisher><subject>Agricultural soils ; ARGENTINA ; ARGENTINE ; BOVIN ; CATTLE ; COMPACTACION DEL SUELO ; COMPACTAGE DU SOL ; CONDICIONES AMBIENTALES ; CONDITION DE MILIEU ; CONTENIDO DE AGUA EN EL SUELO ; DENSIDAD ; DENSIDAD DEL SUELO ; DENSITE ; DENSITE DU SOL ; DENSITY ; ENVIRONMENTAL CONDITIONS ; FLOODED LAND ; Flooded soils ; Floods ; Forest soils ; GANADO BOVINO ; Grassland soils ; GRAZING ; GRAZING INTENSITY ; INTENSIDAD DE PASTOREO ; INTENSITE DE PATURAGE ; Organic soils ; PAMPA ; PAMPAS ; PASTOREO ; PATURAGE ; PIETINEMENT ; PISOTEO ; Plant-Animal Interaction ; PROPIEDADES FISICO-QUIMICAS (SUELO) ; PROPRIETE PHYSICO-CHIMIQUE DU SOL ; Rangeland soils ; SOIL CHEMICOPHYSICAL PROPERTIES ; SOIL COMPACTION ; SOIL DENSITY ; Soil water ; SOIL WATER CONTENT ; TENEUR EN EAU DU SOL ; TERRE INONDEE ; TIERRAS INUNDADAS ; TRAMPLING</subject><ispartof>Journal of range management, 1988-11, Vol.41 (6), p.500-503</ispartof><rights>Copyright 1988 The Society for Range Management</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c236t-25c78868d1fe71b20a357c23b71eb56f67938ce185a7339143176e9f9d900b803</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids></links><search><creatorcontrib>Taboada, M.A</creatorcontrib><creatorcontrib>Lavado, R.S</creatorcontrib><title>Grazing effects of the bulk density in a Natraquoll of the flooding pampa of Argentina</title><title>Journal of range management</title><description>The influence of grazing by cattle on soil bulk density was studied in a typic Natraquoll of the Flooding Pampa of Argentina for a period of 33 months, by comparing a grazed situation to an enclosure deferred from grazing for 7 years. Floods took place in this period as usual. Bulk density (BD) at -33.3 kPa of water retention varied from 1.00 to 1.11 Mg m-3in the ungrazed soil and in the grazed soil from 1.04 to 1.16 Mg m-3. Environmental factors were the primary agent controlling BD; only in some periods were there significant differences between treatments. Slight increases in BD occurred under grazing after the recession of the flood water, and significant decreases occurred in the ungrazed soil during the large and sudden falls in water content. In this case the effect of trampling, therefore, would consist mainly of impeding the decrease in BD. No compaction was observed in periods when no flood occurred or while soil remained submerged in water. The results indicated that the variations of bulk density caused by cattle trampling were superimposed on those produced by floods and showed an interaction between the effects of land-use and the particular environmental conditions of the region.</description><subject>Agricultural soils</subject><subject>ARGENTINA</subject><subject>ARGENTINE</subject><subject>BOVIN</subject><subject>CATTLE</subject><subject>COMPACTACION DEL SUELO</subject><subject>COMPACTAGE DU SOL</subject><subject>CONDICIONES AMBIENTALES</subject><subject>CONDITION DE MILIEU</subject><subject>CONTENIDO DE AGUA EN EL SUELO</subject><subject>DENSIDAD</subject><subject>DENSIDAD DEL SUELO</subject><subject>DENSITE</subject><subject>DENSITE DU SOL</subject><subject>DENSITY</subject><subject>ENVIRONMENTAL CONDITIONS</subject><subject>FLOODED LAND</subject><subject>Flooded soils</subject><subject>Floods</subject><subject>Forest soils</subject><subject>GANADO BOVINO</subject><subject>Grassland soils</subject><subject>GRAZING</subject><subject>GRAZING INTENSITY</subject><subject>INTENSIDAD DE PASTOREO</subject><subject>INTENSITE DE PATURAGE</subject><subject>Organic soils</subject><subject>PAMPA</subject><subject>PAMPAS</subject><subject>PASTOREO</subject><subject>PATURAGE</subject><subject>PIETINEMENT</subject><subject>PISOTEO</subject><subject>Plant-Animal Interaction</subject><subject>PROPIEDADES FISICO-QUIMICAS (SUELO)</subject><subject>PROPRIETE PHYSICO-CHIMIQUE DU SOL</subject><subject>Rangeland soils</subject><subject>SOIL CHEMICOPHYSICAL PROPERTIES</subject><subject>SOIL COMPACTION</subject><subject>SOIL DENSITY</subject><subject>Soil water</subject><subject>SOIL WATER CONTENT</subject><subject>TENEUR EN EAU DU SOL</subject><subject>TERRE INONDEE</subject><subject>TIERRAS INUNDADAS</subject><subject>TRAMPLING</subject><issn>0022-409X</issn><issn>2162-2728</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNp90D1PwzAQBmALgUQpiJ3JAxJTwD4n_hirCgpSBQMUsUWXxC4paVxsdyi_nlYtK9Pp7p674SXkkrNbEEzdCW1MAfKIDIBLyECBPiYDxgCynJmPU3IW42LbylyaAXmfBPxp-zm1ztk6ReodTZ-WVuvuiza2j23a0LanSJ8xBfxe-677M67zvtndrnC5wt10FOa2T22P5-TEYRftxaEOyezh_m38mE1fJk_j0TSrQciUQVErraVuuLOKV8BQFGq7qhS3VSGdVEbo2nJdoBLC8FxwJa1xpjGMVZqJIbnZ_62DjzFYV65Cu8SwKTkrd3GUhzi28novFzH58A-72jOHvsR5aGM5e9UGoMi1-AV1lmQZ</recordid><startdate>198811</startdate><enddate>198811</enddate><creator>Taboada, M.A</creator><creator>Lavado, R.S</creator><general>Society for Range Management</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>198811</creationdate><title>Grazing effects of the bulk density in a Natraquoll of the flooding pampa of Argentina</title><author>Taboada, M.A ; Lavado, R.S</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c236t-25c78868d1fe71b20a357c23b71eb56f67938ce185a7339143176e9f9d900b803</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>Agricultural soils</topic><topic>ARGENTINA</topic><topic>ARGENTINE</topic><topic>BOVIN</topic><topic>CATTLE</topic><topic>COMPACTACION DEL SUELO</topic><topic>COMPACTAGE DU SOL</topic><topic>CONDICIONES AMBIENTALES</topic><topic>CONDITION DE MILIEU</topic><topic>CONTENIDO DE AGUA EN EL SUELO</topic><topic>DENSIDAD</topic><topic>DENSIDAD DEL SUELO</topic><topic>DENSITE</topic><topic>DENSITE DU SOL</topic><topic>DENSITY</topic><topic>ENVIRONMENTAL CONDITIONS</topic><topic>FLOODED LAND</topic><topic>Flooded soils</topic><topic>Floods</topic><topic>Forest soils</topic><topic>GANADO BOVINO</topic><topic>Grassland soils</topic><topic>GRAZING</topic><topic>GRAZING INTENSITY</topic><topic>INTENSIDAD DE PASTOREO</topic><topic>INTENSITE DE PATURAGE</topic><topic>Organic soils</topic><topic>PAMPA</topic><topic>PAMPAS</topic><topic>PASTOREO</topic><topic>PATURAGE</topic><topic>PIETINEMENT</topic><topic>PISOTEO</topic><topic>Plant-Animal Interaction</topic><topic>PROPIEDADES FISICO-QUIMICAS (SUELO)</topic><topic>PROPRIETE PHYSICO-CHIMIQUE DU SOL</topic><topic>Rangeland soils</topic><topic>SOIL CHEMICOPHYSICAL PROPERTIES</topic><topic>SOIL COMPACTION</topic><topic>SOIL DENSITY</topic><topic>Soil water</topic><topic>SOIL WATER CONTENT</topic><topic>TENEUR EN EAU DU SOL</topic><topic>TERRE INONDEE</topic><topic>TIERRAS INUNDADAS</topic><topic>TRAMPLING</topic><toplevel>online_resources</toplevel><creatorcontrib>Taboada, M.A</creatorcontrib><creatorcontrib>Lavado, R.S</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><jtitle>Journal of range management</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Taboada, M.A</au><au>Lavado, R.S</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Grazing effects of the bulk density in a Natraquoll of the flooding pampa of Argentina</atitle><jtitle>Journal of range management</jtitle><date>1988-11</date><risdate>1988</risdate><volume>41</volume><issue>6</issue><spage>500</spage><epage>503</epage><pages>500-503</pages><issn>0022-409X</issn><eissn>2162-2728</eissn><notes>8922548</notes><notes>P33</notes><notes>F01</notes><notes>L02</notes><abstract>The influence of grazing by cattle on soil bulk density was studied in a typic Natraquoll of the Flooding Pampa of Argentina for a period of 33 months, by comparing a grazed situation to an enclosure deferred from grazing for 7 years. Floods took place in this period as usual. Bulk density (BD) at -33.3 kPa of water retention varied from 1.00 to 1.11 Mg m-3in the ungrazed soil and in the grazed soil from 1.04 to 1.16 Mg m-3. Environmental factors were the primary agent controlling BD; only in some periods were there significant differences between treatments. Slight increases in BD occurred under grazing after the recession of the flood water, and significant decreases occurred in the ungrazed soil during the large and sudden falls in water content. In this case the effect of trampling, therefore, would consist mainly of impeding the decrease in BD. No compaction was observed in periods when no flood occurred or while soil remained submerged in water. The results indicated that the variations of bulk density caused by cattle trampling were superimposed on those produced by floods and showed an interaction between the effects of land-use and the particular environmental conditions of the region.</abstract><pub>Society for Range Management</pub><doi>10.2307/3899526</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0022-409X |
| ispartof | Journal of range management, 1988-11, Vol.41 (6), p.500-503 |
| issn | 0022-409X 2162-2728 |
| language | eng |
| recordid | cdi_crossref_primary_10_2307_3899526 |
| source | Alma/SFX Local Collection |
| subjects | Agricultural soils ARGENTINA ARGENTINE BOVIN CATTLE COMPACTACION DEL SUELO COMPACTAGE DU SOL CONDICIONES AMBIENTALES CONDITION DE MILIEU CONTENIDO DE AGUA EN EL SUELO DENSIDAD DENSIDAD DEL SUELO DENSITE DENSITE DU SOL DENSITY ENVIRONMENTAL CONDITIONS FLOODED LAND Flooded soils Floods Forest soils GANADO BOVINO Grassland soils GRAZING GRAZING INTENSITY INTENSIDAD DE PASTOREO INTENSITE DE PATURAGE Organic soils PAMPA PAMPAS PASTOREO PATURAGE PIETINEMENT PISOTEO Plant-Animal Interaction PROPIEDADES FISICO-QUIMICAS (SUELO) PROPRIETE PHYSICO-CHIMIQUE DU SOL Rangeland soils SOIL CHEMICOPHYSICAL PROPERTIES SOIL COMPACTION SOIL DENSITY Soil water SOIL WATER CONTENT TENEUR EN EAU DU SOL TERRE INONDEE TIERRAS INUNDADAS TRAMPLING |
| title | Grazing effects of the bulk density in a Natraquoll of the flooding pampa of Argentina |
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