Pedoenvironmental indicators of soil in Western Amazonia, Brazil
This study aimed to ascertain what soil attributes may be an indicator of natural and anthropic pedogenic changes in top grassland (TG), low grassland (LG), ecotone zone (EZ), and forest (F) in Western Amazonia. Twenty samples of the diagnostic horizons were collected from the studied pedoenvironmen...
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description | This study aimed to ascertain what soil attributes may be an indicator of natural and anthropic pedogenic changes in top grassland (TG), low grassland (LG), ecotone zone (EZ), and forest (F) in Western Amazonia. Twenty samples of the diagnostic horizons were collected from the studied pedoenvironments: TG (A 0.0–14 and B
i
0.30–0.66 m); LG (A 0.0–0.15 and C
g1
0.27–0.80 m); EZ (A 0.0–0.15 and B
i
0.32–0.50 m); and forest (F) (A1 0.0–0.15 and B
t1
0.67–0.10 m). Sand, silt, clay, particle density (PD),soil bulk density (BD),saturated soil hydraulic conductivity, calcium (Ca), magnesium (Mg), exchangeable aluminum (Al
3+
), potassium (K), sodium (Na), phosphorus (P), pH in water and KCl, and organic matter (OM) contents were calculated and submitted to variance analysis. LG is more related to OM and clay than SHC value. These same attributes characterized TG. EZ is highlighted by its higher values and relationship with Al and K. It was concluded that for TG, LG, EZ, and F top soil layers, 28% of natural and anthropic changes can be identified based on sand, clay, pH in KCl, and OM data; on the other hand, subsurface 23% of determinations can be attributed to pH in H
2
O, Al, Na, and sand. |
doi_str_mv | 10.1007/s10661-020-08757-6 |
format | Article |
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i
0.30–0.66 m); LG (A 0.0–0.15 and C
g1
0.27–0.80 m); EZ (A 0.0–0.15 and B
i
0.32–0.50 m); and forest (F) (A1 0.0–0.15 and B
t1
0.67–0.10 m). Sand, silt, clay, particle density (PD),soil bulk density (BD),saturated soil hydraulic conductivity, calcium (Ca), magnesium (Mg), exchangeable aluminum (Al
3+
), potassium (K), sodium (Na), phosphorus (P), pH in water and KCl, and organic matter (OM) contents were calculated and submitted to variance analysis. LG is more related to OM and clay than SHC value. These same attributes characterized TG. EZ is highlighted by its higher values and relationship with Al and K. It was concluded that for TG, LG, EZ, and F top soil layers, 28% of natural and anthropic changes can be identified based on sand, clay, pH in KCl, and OM data; on the other hand, subsurface 23% of determinations can be attributed to pH in H
2
O, Al, Na, and sand.</description><identifier>ISSN: 0167-6369</identifier><identifier>EISSN: 1573-2959</identifier><identifier>DOI: 10.1007/s10661-020-08757-6</identifier><identifier>PMID: 33215295</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Aluminium ; Aluminum ; Atmospheric Protection/Air Quality Control/Air Pollution ; Bismuth ; Brazil ; Bulk density ; Calcium ; Clay ; Clay soils ; Diagnostic systems ; Earth and Environmental Science ; Ecology ; Ecotoxicology ; Eigenvalues ; Environment ; Environmental Management ; Environmental Monitoring ; Environmental science ; Forests ; Grasslands ; Habitat selection ; Hydraulic conductivity ; Hydraulics ; Magnesium ; Monitoring/Environmental Analysis ; Organic matter ; Organic phosphorus ; Particle density (concentration) ; pH effects ; Phosphorus ; Potassium ; Potassium chloride ; Sand ; Saturated soils ; Sodium ; Soil ; Soil conductivity ; Soil density ; Soil layers ; Variance analysis</subject><ispartof>Environmental monitoring and assessment, 2020-12, Vol.192 (12), p.768, Article 768</ispartof><rights>Springer Nature Switzerland AG 2020</rights><rights>Springer Nature Switzerland AG 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c375t-aa1160ab93419d16cfc570309d2f0d3bc2dc23b9e45e067a80d023057dbe0e0f3</citedby><cites>FETCH-LOGICAL-c375t-aa1160ab93419d16cfc570309d2f0d3bc2dc23b9e45e067a80d023057dbe0e0f3</cites><orcidid>0000-0002-8183-7069</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10661-020-08757-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10661-020-08757-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33215295$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>de Oliveira, Ivanildo Amorim</creatorcontrib><creatorcontrib>Campos, Milton César Costa</creatorcontrib><creatorcontrib>Siqueira, Diego Silva</creatorcontrib><creatorcontrib>de Freitas, Ludmila</creatorcontrib><creatorcontrib>de Aquino, Renato Eleotério</creatorcontrib><creatorcontrib>de Oliveira, Flavio Pereira</creatorcontrib><title>Pedoenvironmental indicators of soil in Western Amazonia, Brazil</title><title>Environmental monitoring and assessment</title><addtitle>Environ Monit Assess</addtitle><addtitle>Environ Monit Assess</addtitle><description>This study aimed to ascertain what soil attributes may be an indicator of natural and anthropic pedogenic changes in top grassland (TG), low grassland (LG), ecotone zone (EZ), and forest (F) in Western Amazonia. Twenty samples of the diagnostic horizons were collected from the studied pedoenvironments: TG (A 0.0–14 and B
i
0.30–0.66 m); LG (A 0.0–0.15 and C
g1
0.27–0.80 m); EZ (A 0.0–0.15 and B
i
0.32–0.50 m); and forest (F) (A1 0.0–0.15 and B
t1
0.67–0.10 m). Sand, silt, clay, particle density (PD),soil bulk density (BD),saturated soil hydraulic conductivity, calcium (Ca), magnesium (Mg), exchangeable aluminum (Al
3+
), potassium (K), sodium (Na), phosphorus (P), pH in water and KCl, and organic matter (OM) contents were calculated and submitted to variance analysis. LG is more related to OM and clay than SHC value. These same attributes characterized TG. EZ is highlighted by its higher values and relationship with Al and K. It was concluded that for TG, LG, EZ, and F top soil layers, 28% of natural and anthropic changes can be identified based on sand, clay, pH in KCl, and OM data; on the other hand, subsurface 23% of determinations can be attributed to pH in H
2
O, Al, Na, and sand.</description><subject>Aluminium</subject><subject>Aluminum</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Bismuth</subject><subject>Brazil</subject><subject>Bulk density</subject><subject>Calcium</subject><subject>Clay</subject><subject>Clay soils</subject><subject>Diagnostic systems</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Ecotoxicology</subject><subject>Eigenvalues</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Environmental Monitoring</subject><subject>Environmental science</subject><subject>Forests</subject><subject>Grasslands</subject><subject>Habitat selection</subject><subject>Hydraulic conductivity</subject><subject>Hydraulics</subject><subject>Magnesium</subject><subject>Monitoring/Environmental Analysis</subject><subject>Organic matter</subject><subject>Organic phosphorus</subject><subject>Particle density (concentration)</subject><subject>pH effects</subject><subject>Phosphorus</subject><subject>Potassium</subject><subject>Potassium chloride</subject><subject>Sand</subject><subject>Saturated soils</subject><subject>Sodium</subject><subject>Soil</subject><subject>Soil conductivity</subject><subject>Soil density</subject><subject>Soil layers</subject><subject>Variance analysis</subject><issn>0167-6369</issn><issn>1573-2959</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>BENPR</sourceid><recordid>eNp9kE1LAzEQhoMotlb_gAdZ8OrqJNkkzc22-AUFPSgeQ3aTlS3dpCZbwf56U7fqzdPAzDPvDA9CpxguMYC4ihg4xzkQyGEsmMj5HhpiJmhOJJP7aAiYpyblcoCOYlwAgBSFPEQDSglmCRqi6ydrvHUfTfCuta7Ty6xxpql050PMfJ1F32xb2auNnQ0um7R6412jL7Jp0JtmeYwOar2M9mRXR-jl9uZ5dp_PH-8eZpN5XlHBulxrjDnoUtICS4N5VVdMAAVpSA2GlhUxFaGltAWzwIUegwFCgQlTWrBQ0xE673NXwb-v0zNq4dfBpZOKFIISRqlkiSI9VQUfY7C1WoWm1eFTYVBbaaqXppI09S1N8bR0totel601vys_lhJAeyCmkXuz4e_2P7FfakN2sA</recordid><startdate>20201201</startdate><enddate>20201201</enddate><creator>de Oliveira, Ivanildo Amorim</creator><creator>Campos, Milton César Costa</creator><creator>Siqueira, Diego Silva</creator><creator>de Freitas, Ludmila</creator><creator>de Aquino, Renato Eleotério</creator><creator>de Oliveira, Flavio Pereira</creator><general>Springer 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indicators of soil in Western Amazonia, Brazil</title><author>de Oliveira, Ivanildo Amorim ; Campos, Milton César Costa ; Siqueira, Diego Silva ; de Freitas, Ludmila ; de Aquino, Renato Eleotério ; de Oliveira, Flavio Pereira</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c375t-aa1160ab93419d16cfc570309d2f0d3bc2dc23b9e45e067a80d023057dbe0e0f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Aluminium</topic><topic>Aluminum</topic><topic>Atmospheric Protection/Air Quality Control/Air Pollution</topic><topic>Bismuth</topic><topic>Brazil</topic><topic>Bulk density</topic><topic>Calcium</topic><topic>Clay</topic><topic>Clay soils</topic><topic>Diagnostic systems</topic><topic>Earth and Environmental Science</topic><topic>Ecology</topic><topic>Ecotoxicology</topic><topic>Eigenvalues</topic><topic>Environment</topic><topic>Environmental Management</topic><topic>Environmental 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Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Environmental monitoring and assessment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>de Oliveira, Ivanildo Amorim</au><au>Campos, Milton César Costa</au><au>Siqueira, Diego Silva</au><au>de Freitas, Ludmila</au><au>de Aquino, Renato Eleotério</au><au>de Oliveira, Flavio Pereira</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Pedoenvironmental indicators of soil in Western Amazonia, Brazil</atitle><jtitle>Environmental monitoring and assessment</jtitle><stitle>Environ Monit Assess</stitle><addtitle>Environ Monit Assess</addtitle><date>2020-12-01</date><risdate>2020</risdate><volume>192</volume><issue>12</issue><spage>768</spage><pages>768-</pages><artnum>768</artnum><issn>0167-6369</issn><eissn>1573-2959</eissn><abstract>This study aimed to ascertain what soil attributes may be an indicator of natural and anthropic pedogenic changes in top grassland (TG), low grassland (LG), ecotone zone (EZ), and forest (F) in Western Amazonia. Twenty samples of the diagnostic horizons were collected from the studied pedoenvironments: TG (A 0.0–14 and B
i
0.30–0.66 m); LG (A 0.0–0.15 and C
g1
0.27–0.80 m); EZ (A 0.0–0.15 and B
i
0.32–0.50 m); and forest (F) (A1 0.0–0.15 and B
t1
0.67–0.10 m). Sand, silt, clay, particle density (PD),soil bulk density (BD),saturated soil hydraulic conductivity, calcium (Ca), magnesium (Mg), exchangeable aluminum (Al
3+
), potassium (K), sodium (Na), phosphorus (P), pH in water and KCl, and organic matter (OM) contents were calculated and submitted to variance analysis. LG is more related to OM and clay than SHC value. These same attributes characterized TG. EZ is highlighted by its higher values and relationship with Al and K. It was concluded that for TG, LG, EZ, and F top soil layers, 28% of natural and anthropic changes can be identified based on sand, clay, pH in KCl, and OM data; on the other hand, subsurface 23% of determinations can be attributed to pH in H
2
O, Al, Na, and sand.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><pmid>33215295</pmid><doi>10.1007/s10661-020-08757-6</doi><orcidid>https://orcid.org/0000-0002-8183-7069</orcidid></addata></record> |
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subjects | Aluminium Aluminum Atmospheric Protection/Air Quality Control/Air Pollution Bismuth Brazil Bulk density Calcium Clay Clay soils Diagnostic systems Earth and Environmental Science Ecology Ecotoxicology Eigenvalues Environment Environmental Management Environmental Monitoring Environmental science Forests Grasslands Habitat selection Hydraulic conductivity Hydraulics Magnesium Monitoring/Environmental Analysis Organic matter Organic phosphorus Particle density (concentration) pH effects Phosphorus Potassium Potassium chloride Sand Saturated soils Sodium Soil Soil conductivity Soil density Soil layers Variance analysis |
title | Pedoenvironmental indicators of soil in Western Amazonia, Brazil |
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