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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Veröffentlicht in:Environmental monitoring and assessment 2020-12, Vol.192 (12), p.768, Article 768
Hauptverfasser: de Oliveira, Ivanildo Amorim, Campos, Milton César Costa, Siqueira, Diego Silva, de Freitas, Ludmila, de Aquino, Renato Eleotério, de Oliveira, Flavio Pereira
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container_issue 12
container_start_page 768
container_title Environmental monitoring and assessment
container_volume 192
creator de Oliveira, Ivanildo Amorim
Campos, Milton César Costa
Siqueira, Diego Silva
de Freitas, Ludmila
de Aquino, Renato Eleotério
de Oliveira, Flavio Pereira
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.
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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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