Impact of historical soil management on the interaction of plant-growth-promoting bacteria with maize (Zea mays L.).

Edaphic factors can modulate the effects of microbial inoculants on crop yield promotion. Given the potential complexity of microbial inoculant responses to diverse soil management practices, we hypothesize that sustainable management of soil and water irrigation may improve soil quality and enhance the effects of plant growth-promoting bacteria (PGPB). Consequently, the primary objective was to assess the effectiveness of microbial inoculants formulated with Herbaspirillum seropedicae (Hs) and Azospirillum brasilense (Ab) on maize growth in soils impacted by different historical conservation management systems. We evaluated two soil management systems, two irrigation conditions, and four treatments: T0 - without bioinoculant and 100% doses of NPK fertilization; T1 - Hs + humic substances and 40% of NPK fertilization; T2 - Ab and 40% of NPK fertilization; T3 - co-inoculation (Hs + Ab) and 40% of NPK fertilization. Using a reduced fertilization dose (40% NPK) associated with microbial inoculants proved efficient in increasing maize shoot dry mass : on average, there was a 16% reduction compared to the treatment with 100% fertilization. In co-inoculation (Hs + Ab), the microbial inoculants showed a mutualistic effect on plant response, higher than isolate ones, especially increasing the nitrogen content in no-tillage systems irrigated by swine wastewater. Under lower nutrient availability and higher biological soil quality, the microbial bioinputs positively influenced root development, instantaneous water use efficiency, stomatal conductance, and nitrogen contents.

Nitrogen fertilization regulates crosstalk between marandu palisadegrass and Herbaspirillum seropedicae: An investigation based on 15N isotopic analysis and root morphology.

Strategies seeking to increase the use efficiency of nitrogen (N) fertilizers and that benefit plant growth through multiple mechanisms can reduce production costs and contribute to more sustainable agriculture free of polluting residues. Under controlled conditions, we investigated the compatibility between foliar inoculation with an endophytic diazotrophic bacterium (Herbaspirillum seropedicae HRC54) at control and low, medium and high N fertilization levels (0, 25, 50 and 100 mg of N kg-1 as urea, respectively) in Marandu palisadegrass. Common procedures in our research field (biometric and nutritional assessments) were combined with isotopic techniques (natural abundance - δ15N‰ and 15N isotope dilution) and root scanning to determine the contribution of fixed N and recovery of N fertilizer by the grass. Overall, the combined use of 15N isotopic techniques revealed that inoculation not only improved the recovery of applied N-urea from the soil but also provided fixed nitrogen to Marandu palisade grass, resulting in an increase in the total accumulated N. When inoculated plants grew at control and low levels of N, a positive cascade effect encompassing root growth stimulation (nodes of smaller diameter roots), better soil and fertilizer resource exploitation and increased forage production was observed. In contrast, increasing N reduced the contributions of N fixed by H. seropedicae from 21.5% at the control level to 8.6% at the high N level. Given the minimal to no observed growth promotion, this condition was deemed inhibitory to the positive effects of H. seropedicae. We discuss how to make better use of H. seropedicae inoculation in Marandu palisadegrass, albeit on a small scale, thus contributing to a more rational and efficient use of N fertilizers. Finally, we pose questions for future investigations based on 15N isotopic techniques under field conditions, which have great applicability potential.

Geochemical soil dynamics on a bimodal post-collisional intrusive complex.

The importance of environmental quality for global social and ecological development, including soil degradation, cannot be overstated. Trace elements dispersed in the environment due to anthropogenic or geogenic activities can result in ecotoxicological impacts, negatively influencing environmental quality. The reference values for soil quality concerning trace elements are primarily based on geological, geomorphological, and pedological patterns. However, intrinsic geological factors may diverge some concentration levels from established norms. Therefore, conducting comprehensive surveys of environmental quality reference values becomes imperative, incorporating geological, geomorphological, and pedological patterns. A deeper understanding of the distribution of these elements is also required. Multivariate analysis proves crucial in compartmentalizing the most relevant factors, particularly in regions marked by bimodal magmatism arising from post-collisional distensional processes, such as the Santa Angélica intrusive suite in southeast Brazil. This study collected soil samples from pastures and natural grasslands with minimal anthropogenic intervention at two depths. These samples underwent various chemical and physical analyses. Statistical techniques such as correlation analysis, principal component analysis, hierarchical clustering, and geostatistics were utilized to interpret the data. The analysis revealed a correlation between the clay fraction and trace elements, demonstrating that clustering is an effective methodology for ascertaining landscape distribution patterns of these components. When compared to quality reference values, it was observed that most soil content levels exceeded both global and local standards. This study suggests that the presence of barium (Ba) in the soil might be due to the isomorphic replacement of feldspathic minerals in acidic and intermediate rocks, whereas molybdenum (Mo) seems to be associated with soils in the domain of porphyritic allanite granite. However, additional research is warranted to determine the concentration factor of Mo in this scenario accurately.

Trace metals in Rio Doce sediments before and after the collapse of the Fundão iron ore tailing dam, Southeastern Brazil.

The collapse of the Fundão Dam, in Southeastern Brazil, caused about 50 million m³ of iron ore tailings to sluice down the mountain to Rio Doce, in what is considered the greatest environmental disaster in Brazilian history. The fluvial system received an intense and sudden mudflow that was transported for more than 650 km, before reaching the Atlantic Ocean. Because the area was already impacted by the mineral activities in the region, it becomes essential to evaluate the environmental conditions before the disaster to correctly assess the disaster real damage. This study compares the concentration of trace metals in the sediments of the Rio Doce alluvial plain, before and after the dam collapse, as well as the newly deposited iron ore tailings that became part of the sedimentary framework. The data indicate that the fine particles deposited have since been incorporated into the sandy river sediments. The cadmium and arsenic contents in the sediments increased to levels above the National Environment Council thresholds. The comparison between the levels of trace metals in the situations before and after disaster shows that the mining mud is the source of cadmium while the arsenic was present before the environmental disaster, and its concentration increased due to sediment remobilization. The iron ore tailings deposited on the alluvial sediments also affected the physical parameters since the formed ferruginous crusts waterproofed the ground surface and may, gradually, release toxic metals when exposed to weathering and river reworking.

Ensaio em colunas de solo para estudo da influência dos resíduos finos de rochas ornamentais na qualidade da água / Soil column test to study the influence of dimension stone fine wastes on water quality

RESUMO A geração de resíduos finos provenientes do processo de beneficiamento de rochas ornamentais cresce na mesma proporção da produção de chapas para a construção civil. A adoção de medidas preventivas, remediadoras e punitivas está atrelada ao conhecimento do verdadeiro potencial que esses materiais têm para causar impactos negativos ao ambiente. O objetivo deste trabalho foi simular, em laboratório, possíveis alterações na qualidade da água de recarga de aquíferos provocadas pela disposição inadequada desses resíduos. Foram realizados testes de percolação de água em colunas de solo recoberto por resíduos com diferentes taxas de umidade: resíduos sem tratamento, saídos diretamente do tear (TE); resíduos que passaram por filtro prensa (FP) para redução de umidade e resíduos secos em leito de secagem (LS). A água de percolação foi analisada para avaliar alterações em comparação com um branco ou testemunha. Não foram detectadas alterações significativas no pH da água percolada em nenhum dos casos estudados. Porém, no tratamento TE houve alterações em vários parâmetros de qualidade. A água percolada através do resíduo FP se assemelhou àquela do TE em alguns parâmetros e à do LS em outros. ­Conclui-se que os resíduos saídos diretamente da boca do tear possuem alto potencial de degradação da qualidade da água, mas a redução de umidade é eficaz para reduzir os riscos ambientais. O uso de LS pode ser um método tão eficaz quanto o FP, se conduzido de forma adequada e respeitando as normas legais.

ABSTRACT The generation of fine wastes from cutting of ornamental stones grows at the same rate of plate production for civil construction. The adoption of safe, remediating and punitive measures are linked to the knowledge of the actual potentiality that these materials have for causing negative impacts to the environment. The aim of this work was to simulate, in laboratory, possible alterations in the recharging groundwater quality provoked by the improper disposal of these wastes. We conducted tests of percolating water through soil columns covered by wastes with different humidity rates: wastes without treatment, outgoing directly from the looms (TE); wastes that passed by filter press for humidity reducing (FP) and wastes dried in a drying pond (LS). Percolated water was analyzed to evaluate alterations of its quality in relation to a blank (B) or control. Significant changes did not occur in pH-values of percolated water in any of the cases studied. However, many water quality parameters were changed during TE treatment. The water percolated through FP residues was similar to that of the looms in relation to some parameters and with the LS wastes, in others. We concluded that the wastes that just left the loom have high potential for changing water quality, but the reduction of waste´s humidity is efficient for minimizing environmental risks. The use of drying bed could be as efficient as the filter press, if conducted in a proper form and according to legal regulations.