Spatiotemporal Variability in Soil Properties and Composition in Mangrove Forests in Baia de Todos os Santos (NE Brazil)

被引:5
|
作者
Ramos, Monica Arlinda Vasconcelos [1 ,2 ]
Perez-Alberti, Augusto [1 ]
Nobrega, Gabriel Nuto [3 ]
Otero, Xose Luis [1 ,4 ]
机构
[1] Univ Santiago de Compostela, Dept Edafoloxia & Quim Agr, CRETUS, Fac Biol, Santiago 15705, Spain
[2] Univ Fed Reconcavo Bahia, Ctr Ciencias Agr Ambientais & Biol CCAAB, BR-44380000 Cruz Das Almas, Brazil
[3] Univ Fed Ceara, Ctr Ciencias Agr CCA, Dept Ciencias Solo, BR-60020181 Fortaleza, Brazil
[4] Univ Santiago de Compostela, Estn Biol Marina Grana Ferrol, Rede Estn Biol, Ferrol 15590, Spain
关键词
soil geochemistry; pyrites; iron partitioning; organic matter; isotopic signatures; FESEM; SEQUENTIAL EXTRACTION PROCEDURE; TRACE-METAL CONTAMINATION; ORGANIC-MATTER; ESTUARINE SYSTEM; CARBON; SEDIMENTS; BAY; BAHIA; IRON; RHIZOPHORA;
D O I
10.3390/land12071392
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil properties and components in mangrove ecosystems influence their geochemical processes and services. Despite the extensive mangrove areas present in Brazil, few studies focusing on these themes are under development. In this sense, this work aimed to investigate the spatial variability in soil attributes and composition, the geochemistry of Fe, and the isotopic characteristics of organic matter in mangroves in Baia de Todos os Santos (Cacha Prego, Ponta Grossa, Ilha de Mare, Pitinga), which constitutes Brazil's second largest bay. The soils investigated showed spatial and temporal changes affecting their properties (pH, Eh) and composition (TOC, Fe fractions), as well as clear spatial changes in the redox potential values (+30-+188 mV), with higher values in PT. Soil textures ranged from predominantly sandy (CP, PT, PG: sand, >70%) to a finer granulometry (IM: sand, 33-64%). These characteristics influenced Fe partitioning and organic matter content, with higher TOC and pyrite values observed in IM (FeS2: 2720-9233 mg kg(-1); TOC: 4.4-6.6%) and lower sulfide values found in PT, mainly in the dry season (FeS2: 85-235 mg kg(-1)). The soil & delta;C-13 and N/C ratios seem to suggest a mixed origin of organic matter.
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页数:20
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