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Extreme climatic events may be translated into a higher frequency of both dry and wet years. Frequent droughts pose a challenge to water supply in terms of both quantity and quality. In order to cope with this, there has to be a documentation on the concentration of chemicals in water during such events. The southeast region of Brazil experienced a major drought event in 2014 leading to number of social, economic, and environmental impacts. The objective of the present paper is to understand the effect of an extreme drought on dissolved organic and inorganic carbon concentrations of the Piracicabal river, which is under high human pressure. Concentrations of both dissolved organic (DOC) and inorganic carbon (DIC) were monitored daily, for 30 days, during a dry month in 2014. DOC values found here were at least twice those observed in the river in non-extreme conditions. Rain events within this drought led to significant differences in discharge, DOC, and DIC. We built a dilution-concentration model which described an exponential relationship between discharge and both carbon forms. This indicated that drastic changes in concentrations of DOC and DIC are expected during such events. Our results may also apply to a number of regions in the world especially those of the developing countries where rivers are highly subjected to sewage impact.

Therehave been a number of studies dealing with soil hydraulic properties. Yet,there is a poor discussion on the number of samples necessary to represent suchvariables that usually vary orders of magnitude in space. In the present paper,we examine the adequate number of samples for two soil saturated hydraulicconductivity (Ksat) data sets: (1) normal distribution (a 40 year-old pasture)and (2) non-normal distribution (primary forest). To assess the adequate numberof samples in each case, we used for normal distribution, an statisticalcriterion of standard deviation lower than 5% compared to a high samplingeffort (n = 25) as an indicative of a proper representation of Ksatvariability. In the case of non-normal distribution, we used the same criterionbut using median absolute deviation (a non-parametric statistics). Both data sets were available in Salemi et al. (2013) and were Ksat measured at 0.15 msoil depth for medium-textured inceptisols in São Paulo State, Brazil. For eachdata set, we simulated 10 ‘new’ samplings in which we calculated mean andstandard deviation from sample 1 to 25 (for normal data) and median and medianabsolute deviation (for non-normal data). We found that, on average, at least17 to 22 samples had to be collected to meet the adopted criterion for normaldata whereas 20 to 25 had to be collected for non-normal data. Such numbers ofsamples exceed those used in a number of papers. Additional examples of thismethod with a light modification are given to establish number of samples innew study areas as well as to estimate number of samples when comparing two (ormore) land-uses. Simple and practical procedures like those presented herecould estimate the number of samples that adequately represents soil hydraulicproperties variability. &nbsp

© 2019 Elsevier B.V. Soil erosion leads to land degradation and translocation of soil particles together with associated particulate organic carbon (POC)and nutrients, thereby influencing the global carbon cycle. In the present study, we estimated the contribution of POC delivered to a first-order stream from upslope sugarcane fields and a riparian forest in southeast Brazil. The results show that the amount of surface runoff and soil erosion generated in the riparian forest is significantly lower than in the upslope sugarcane field. However, the contribution of the forest to the total stream bed POC was above 70%, even though most sediments delivered to the stream originated from the upland sugarcane fields. The discrepancy between sediment and POC delivery from both land uses is a consequence of the presence of preferential runoff pathways from the agricultural fields, through the buffer strips, to the stream. This disconnection between the main sources of sediment and POC to the first-order stream is a potentially important mechanism influencing the transfer of POC from upslope areas to waterways. This mechanism should be considered in order to more reliably assess fluxes of OC from upslope areas to first-order streams in landscapes where arable land is separated from streams by a semi-natural buffer zone with permanent vegetation. ispartof: CATENA vol:181 status: published

Sugarcane is an annual crop with a dynamic canopy that changes over time mainly because of genetic adaptation. There is uncertainty about the temporal trends of throughfall (TF) in this important commercial crop. In the present paper, we used troughs to measure TF in a third and fourth ratoon and subsequently in a fourth and fifth ratoon. Additional measurements were carried out in an adjacent riparian forest. There were no significant differences between cycles of sugarcane, growth phases and riparian forest. The TF results for ratoon crop and riparian forest in 2011/2012 were 76% and 79.5% of gross rainfall, respectively, while in 2012/2013, they were 79% and 78%, respectively. However, TF was remarkably lower in the riparian forest relative to ratoon from the second half of the culm formation and elongation phase (280 days after harvest) until harvest. Copyright © 2016 John Wiley & Sons, Ltd.

RESUMO Necrochorume é um efluente gerado a partir da decomposição de corpos. Em cemitérios, a principal causa de poluição subsuperficial é a sua percolação, que altera significativamente o solo, impedindo-o de realizar suas funções naturais. Particularmente no Brasil, pela falta de planejamento consequente do histórico cultural, os cemitérios se localizam totalmente integrados à malha urbana, representando um problema de saúde pública. O risco de contaminação está associado à presença de elementos, como compostos nitrogenados, metais pesados, vírus e bactérias, com riscos inerentes à saúde humana. Na literatura, esses contaminantes têm sido constantemente identificados no ambiente geológico a partir de resultados analíticos de água e solo quando comparados a uma área não impactada. A presente pesquisa objetivou investigar eventuais alterações no meio físico subsuperficial do cemitério municipal da cidade de Rio Claro, São Paulo, por meio dos resultados analíticos dos poços, apoiados por dados obtidos da técnica geofísica da sondagem elétrica vertical (SEV). Os resultados apontaram boa correlação com a evolução espacial e temporal da ocupação do cemitério ao longo de sua história. ABSTRACT Putrefative liquid is an effluent generated from the decomposition of bodies. In cemeteries, the leading cause of subsurface pollution is the liquefaction products percolation, which substantially alter the physical-chemical and biological characteristics of the soil. In Brazil, due to the lack of consistent planning due to cultural history, cemeteries are fully integrated into urban areas, which can be a public health problem. The risk of contamination is associated with the presence of elements such as nitrogen compounds, heavy metals, viruses and bacteria, with risks to human health. In the literature, these contaminants have been consistently identified in the geological environment through analytical results of water and soil compared to non affected areas. This research aimed to investigate possible changes in the subsurface physical environment of the Rio Claro city (São Paulo, Brazil) municipal cemetery, through the analytical results of the wells, supported by data obtained from the geophysical technique of vertical electrical sounding (VES). The results showed good correlation with the spatial and temporal evolution of the occupation of the cemetery throughout its history.