Resumo É fornecida uma primeira lista de verificação das espécies de Rotifera em ambientes de água doce no Estado da Bahia, nordeste do Brasil. A lista de espécies inclui dados de amostragem de 26 ambientes aquáticos (lóticos e lênticos) de 2010 a 2016. Cento e cinquenta e cinco espécies foram registradas, com 68 novos registros para o estado. As famílias Brachionidae e Lecanidae foram as mais representativas (54,8%). A maior riqueza foi registrada no rio Colônia (57 espécies). Esses resultados provavelmente refletem o número de estudos na região, sugerindo mais pesquisas sobre a biodiversidade de Rotifera na Bahia, o quinto maior estado do Brasil (567.295 km2) com grande número de corpos aquáticos de água doce.

Abstract A first checklist of Rotifera species in freshwater environments in Bahia State, in northeastern Brazil, is provided. The list includes sampling data from 26 aquatic environments (lotic and lentic) undertaken from 2010 to 2016. One hundred and fifty-five species were recorded, with 68 new records for the state. The family Brachionidae and Lecanidae were the most representative (54.8%). The greatest richness was recorded in the Colônia River (57 species). Those results reflect the low numbers of studies previously undertaken in the region, indicating more research needs to be focused on Rotifera biodiversity in Bahia, the fifth largest state in Brazil (567,295 km2) with large numbers of freshwater bodies.

Catalytic ozonation has been recognized in the scientific community as an efficient technique, reaching elevated rates of recalcitrant organic material mineralization, even at the presence of scavenger species of hydroxyl free radicals. This study presents the most significant factors involving the leachate treatment stabilized by the municipal landfill of the city of Guaratinguetá, State of São Paulo, Brazil, by using a catalytic ozonation activated by metallic ions Fe3+, Zn2+, Mn2+, Ni2+ and Cr3+. The Taguchi L16 orthogonal array and its associated statistical methods were also used in this study. Among the researched ions, the most notable catalysis was obtained with ferric ion, statistically significant in the reduction of COD with a confidence level of 99.5%.

A influência dos materiais de origem, rochas do Pré-Cambriano e sedimentos coluviais e aluvionares delas derivados, e da posição topográfica na gênese de solos foi estudada em uma toposseqüência representativa das feições geomorfológicas da Baixada Litorânea Fluminense (RJ), no campus da Universidade Federal Rural do Rio de Janeiro (UFRRJ). Foram analisados seis perfis de solo, localizados no terço superior (P1 e P2), médio (P3) e inferior da encosta (P4 e P5), e na baixada (P6). Os processos pedogenéticos e as características dos solos foram relacionados com as unidades geomorfológicas e litoestratigráficas descritas na região. Os perfis P1 e P2, formados 'in situ' a partir do regolito do gnaisse, têm elevada saturação por bases, textura média/argilosa e minerais primários facilmente intemperizáveis na fração areia (micas e feldspatos). O P3, relacionado com uma rampa de colúvio, difere dos anteriores pela elevada saturação por alumínio e ausência de minerais primários facilmente intemperizáveis. P4 e P5, também formados de colúvio, diferem do P3 pela textura superficial arenosa e presença de horizonte E sobrejacente a fragipã. O P6, originado de sedimentos colúvio-aluvionais, tem cores cinzentas, estrutura maciça, textura argilosa e baixa saturação por bases. Os perfis foram classificados como Argissolo (P1, P2 e P3), Planossolo (P4 e P5) e Gleissolo (P6).

The influence of parent materials, Pre-Cambrian rocks, and colluvial and alluvial sediments derived from them, as well as their topographical position in the soil genesis were studied in a toposequence representative of the Baixada Litorânea Fluminense landscape, at the Federal Rural University of Rio de Janeiro, Brazil. Six soil profiles, located on the shoulder position (P1 and P2), backslope (P3), footslope (P4 and P5), and foot slope position (P6) were analyzed. The pedogenic processes and soil properties were related to the geomorphologic and lithostratigraphic units described in the region. Profiles P1 and P2, formed in situ from the gneiss mantle, had high base saturation, medium clayey texture, and easily weathered primary minerals in the sand fraction (mica and feldspar). Profile P3, related to a thick colluvium mantle, differed from P1 and P2 due to a high aluminum saturation and absence of easily weathered primary minerals. Profiles P4 and P5, also formed from colluvial materials, had a sandier surface texture than P3, and showed an E horizon overlying a fragipan. Profile P6, formed from mixed colluvium and alluvium sediments, had gray colors, massive structure, clayey texture, and low base saturation. The soil profiles were classified as Argissol (P1, P2 and P3), Planossol (P4 and P5), and Gleissol (P6).