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Limited knowledge is available regarding biochar (BC) obtained from beach-cast seaweed, which needs to be characterized to better prospect its potential applications. Beach-cast seaweed BCs were produced at two temperatures (300 and 600 °C) and two residence times (1 and 3 h). First, an extensive characterization of feedstock and their derived BCs was performed. Then, an incubation experiment was conducted to investigate the potential of these BCs as ameliorants in two acidic soils, classified as Umbrisols. Proximate and elemental analyses suggested the presence of more stable C structures in BCs at 600 °C with a high C, fixed carbon (FC) and low H, O and volatile matter (VM); additionally, thermogravimetric graphics showed less weight loss. Some features from the raw material were present in biochars obtained at 300 °C but absent at 600 °C. Dissolved organic carbon was much lower in BCs pyrolyzed at 600 °C than at 300 °C, suggesting the higher aromaticity of the former, allowing more resistance to water extraction. The breakdown of proteinaceous soluble materials after pyrolysis was revealed by fluorescence. Residence time caused minor effects in biochar properties compared to temperature. The soil pH and macronutrient availability of the two studied soils increased after beach-cast seaweed biochar addition.

Industrial wastewater effluent containing dyes and hazardous waste, such as olive waste, pose serious threat to health and environment. This work investigated the removal of azo and non-azo dyes from a single and binary aqueous system using hydrochar produced from hazardous olive waste using hydrothermal carbonization (HTC). Optimisation suggested hydrochar obtained at 250°C (HC-9) exhibited best physiochemical, structural properties and around 300% increase in carboxylic and carbonyl groups indicated by nuclear magnetic resonance spectroscopy. HC-9 removed ∼100% of Methylene blue and Congo red in single (120 and 180 min) and binary system (60 min), respectively. Ex situ X-ray photon electron spectroscopy and surface area analysis after adsorption suggested chemisorption supported by pseudo-second order reaction, Langmuir, and Redlich-Peterson model. HC-9 exhibited around 80% reusability in three adsorption cycles. Thus, better working efficiency of our hydrochar in the complex wastewater make it a potential candidate to be employed in commercial plants.

Per- and polyfluoroalkyl substances (PFAS) are ubiquitous global environmental contaminants, environmentally persistent, mobile, can bioaccumulate and are toxic. Increasing emphasis is placed on the immobilisation and removal of PFAS from contaminated environmental matrices such as: potable water, surface water, groundwater, wastewater, sediments and soils (Dauchy et al., 2017; Cao et al., 2019; Hepburn et al., 2019). To achieve this, development of PFAS sorbents is increasingly undertaken (Du et al., 2014). Sorption studies are used to observe the interaction of sorbent and sorbate, but have two key limitations when undertaking sorption experiments for PFAS (1) the experimental protocol and (2) analytical techniques. The current batch sorption methods approached recommended by OECD Guideline 106 (OECD, 2000) are problematic, firstly, due to large sample numbers and PFAS specific laboratory difficulties, including near ubiquitous background PFAS contamination. Secondly, PFAS analytical techniques currently require solid-phase extraction (SPE) to be employed, which is slow and expensive, prior to instrumental analysis with liquid chromatography-mass spectrometry (LC-MS). A suitable alternative approach is needed to mitigate the drawbacks of current methodologies whilst catering for the high sample throughput required by benchtop trials characterising the sorption behaviour of PFAS - sorbent pairings. • A suitable method for PFAS measurement, overcoming shortcomings of current batch sorption methodologies is presented • The method can be applied to a wide range of sorbents and sorption environment conditions associated with PFAS immobilisation or removal in the environment • The presented method is novel through its high sample throughput, simple approach and minimisation of cross contamination sources

Biochar, the product of biomass pyrolysis, has been explored as a soil amendment and carbon capture vessel. Recent literature has aligned biochar as a novel sorbent for a host of environmental contaminants. Through the variation of pyrolysis conditions, biochars can be engineered to have qualities desirable in sorbents whilst maintaining their agronomic benefits. This study focuses on identifying the effects that feedstock type and process temperature have on biochar characteristics which may in turn shed light on their potential environmental applications. Using this approach, six biochars were created from two waste biomasses. The biochars exhibited wide ranges of pH (5.6–11.1), surface area (16.2–397.4 m2/g), electrical conductivity (19–2,826 µS/cm), fixed carbon (72–97%), heavy metal and polycyclic aromatic hydrocarbons (PAHs). Statistically significant trends (P 13 mg/kg), chromium (>93 mg/kg), copper (>143 mg/kg) and PAH (>6 mg/kg) concentrations presented themselves as obstacles to land application in a small number of biochars with respects to International Biochar Initiative (IBI) guidelines. However, it was demonstrated that these could be eliminated through employing pyrolysis processes which encompass higher temperatures (>500 °C) and ensuring the use of contaminant-free feedstocks. The variation in surface areas, carbonized fractions and surface functional groups achieved suggest that using the correct feedstock and process, biochar could be produced in Victoria (Australia) from common organic waste streams to the ends of acting as a sorbent, soil enhancer, and a waste management strategy.

Mine tailing storage represents an important environmental issue. The generation and dispersal of dust from mine tailings can contaminate air and surrounding soils. In addition, metals and soluble salts present in these wastes could pollute groundwater and surface water. The recovery of metals from mine tailings can contribute to minimize the environmental risk and to achieve a circular economy model. The main objective of the present work is to study the use of two carbon-based materials, a commercial activated carbon (AC) and a commercial charcoal (VC) in the leaching of zinc and copper from low-grade tailing waste. Experimental results obtained show that it is possible to achieve the recovery of more than 87 wt% of Zn after 6 h of leaching with different sulfuric acid solutions. The addition of carbon-based materials increases the extraction of Zn at high sulfuric acid concentrations (1 M) from 89% to 99%. The addition of VC significantly increases the extraction of Cu in leaching solution with high sulfuric acid concentration (1 M), from 41 to 61%. Future research will be necessary to optimize the properties of carbon-based materials and their recovery after leaching experiments in order to assess their potential for industrial application.

Biochars and hydrochars have a significant effect on soil properties linked to fertility or to carbon cycling and have been proposed as an amendment to increase soil productivity, particularly in acidic soils. Phytotoxic forms of aluminium (Al) are relatively abundant in acidic soils and, for a long period of time, liming has been used to correct this. Ca(OH)2, a pig manure (PM) and two biochars and two hydrochars prepared from pig manure were studied for their effects on Al fractions. Biochars were prepared at 450 °C (BPC450) and 600 °C (BPC600) and hydrochars were obtained using a pig manure solution (ratio 30:70) that was heated at 200 °C (HPC200) and 240 °C (HPC240). A treatment with an amount of Ca(OH)2 necessary to increase soil pH to the same pH value as the average in the treatments BPC450, BPC600, HPC200, HPC240 and PM was used for comparison. The fractionation of Al was studied, with the liming treatment allowing the differentiation between changes in fractionation driven by pH changes from other mechanisms. In relation to the control, all soil amendments presented high capacity of controlling toxic Al, similar to a traditional liming product (Ca(OH)2) and decreased the exchangeable Al extracted by NH4Cl. Both types of materials (biochars and hydrochars) lead to the formation of an increased number of organo-aluminium complexes (OAC). Biochars lead to the formation of OAC of low to medium stability, while hydrochars promoted the formation of OAC of high stability.

Biochar is a carbon-rich solid obtained from the pyrolysis of organic feedstock under limited oxygen and at relatively low temperatures [...]

Land degradation by old mining activities is a concern worldwide. However, many known technologies are expensive and cannot be considered for mining soil restoration. Biochar amendment of mining soils is becoming an interesting alternative to traditional technologies due to an improvement in soil properties and metal mobility reduction. Biochar effects depend on soil and biochar properties, which in turn vary with pyrolysis conversion parameters and the feedstock used. The objective of this study is to evaluate the effect of four biochars prepared from poultry and rabbit manure at two pyrolysis temperatures (450 and 600 °C) in the trace metal mobility, CO2 emissions, and enzymatic activity of 10 mining soils located in three historical mining areas of Spain (Zarandas-Andalusia, Mijarojos-Cantabria, and Portman-Murcia). For this reason, soils were amended with biochars at a rate of 10% (w/w), and different treatments were incubated for 180 days. For acid soils of the Zarandas-Andalusia area, biochar addition reduced the mobility of Ni, Zn, Cd, Pb, and Cr, respectively, by 91%, 81%, 29%, 67%, and 70%. Nevertheless, biochars did not exhibit the same efficiency in the other two areas where alkaline soils were predominant. CO2 emissions generally increased in the treated soils. The application of biochars produced at 600 °C reduced CO2 emissions, in some cases by more than 28%, being an adequate strategy for C sequestration in soil. The results showed that application of manure biochars can be an effective technique to reduce the mobility of metals in multi-contaminated acid soils, while reducing metal toxicity for soil microorganisms.

In recent times, there has been increased focus on a holistic approach to soil remediation with consideration of social, economic and environmental factors. Consequently, there is a demand from practitioners and regulators alike for suitable ways to measure ancillary outcomes, for example, effects on soil quality. Here we show that biochar, when applied to land to remediate lead (Pb)-contaminated soils, can lead to environmental improvements not realized by adding mined or manufactured phosphates. Here, we study a Pb-contaminated soil amended with two phosphate fertilizers (slow- and fast-release) and with biochars produced from poultry litter and from biosolids at three temperatures (300 °C, 400 °C and 500 °C). The results show that, unlike the fast-release P fertilizer, biochars did not result in an increase in the amount of leachable P that could be released into the environment. Biochars prepared at 500 °C presented a higher value of the integrative geometric mean of soil enzyme activity, compared to the P fertilizers. Overall, our research shows that biochars, particularly those prepared at the higher temperature tested, are a suitable alternative to P fertilizers as an integrative remediation strategy in Pb-contaminated soils, enabling soil biological restoration.

Charcoal briquettes are inexpensive solid fuels made from carbonized biomass. The potential of converting water hyacinth (Eichhornia crassipes) charcoal into briquettes with molasses as binder was investigated in this study. Dried water hyacinth was carbonized at a temperature between 350°C to 500°C in a fabricated fine biomass carbonizer. A solution containing 80% by weight molasses was used in the production of briquettes having different charcoal/molasses ratios of 40:60, 30:70, and 20:80. Each briquette was characterized in terms of bulk density, calorific value, compressive strength, proximate analysis and micro-structure by Scanning Electron Microscopy. Charcoal briquettes were tested for their flammable characteristics through their burning rates and ignition time. Altering the molasses to charcoal ratio affected the quality and characteristics of the briquettes. Volatile combustible matter and fixed carbon increased with increasing amount of binder while ash content decreased. The 30:70 charcoal/molasses ratio produced the highest calorific value (16.6 MJ/kg) and compressive strength (19.1 kg/cm2). The results have shown the potential of converting water hyacinth into an alternative fuel source.

Mercury intrusion porosimetry (MIP) is commonly used to determine soil pore size distributions (PSDs) in a wide, but incomplete, range of equivalent pore diameters. Mono‐ and multifractal analyses of soil PSDs are useful for analyzing the soil porous system. The main objective of this work was to characterize PSDs from tropical soils using the multifractal approach. Duplicate PSDs were measured by MIP for 54 horizons collected from 19 soil profiles in Minas Gerais, Brazil. Although 10 of the studied soils were Ferralsols (Oxisols or Latosols), other soil groups such as Nitisols, Acrisols, Alisols, Luvisols, Planosols, Cambisols, Andisols, and Leptosols also were sampled. Different patterns of PSDs were observed, depending on soil type, texture, and weathering intensity. Textural porosity (0.005–0.2 μm) was positively and significantly correlated to clay and Al2O3 contents and soil specific surface area. Comparison of multifractal analysis from Hg intrusion curves and N2 adsorption isotherms (NAIs) showed entropy dimension values and width of the singularity spectra smaller for the former than for the latter. Multifractal analysis of MIPs and NAIs allowed a thorough characterization of the complexity and heterogeneity of the soil pore space at different scales and was useful to provide new insights for portraying the soil pore system.

Biochar has been presented as a multifunctional material with short- and long-term agro-environmental benefits, including soil organic matter stabilization, improved nutrient cycling, and increased primary productivity. However, its turnover time, when applied to soil, varies greatly depending on feedstock and pyrolysis temperature. For sewage sludge-derived biochars, which have high N contents, there is still a major uncertainty regarding the influence of pyrolysis temperatures on soil carbon mineralization and its relationship to soil N availability. Sewage sludge and sewage sludge-derived biochars produced at 300 °C (BC300), 400 °C (BC400), and 500 °C (BC500) were added to an Oxisol in a short-term incubation experiment. Carbon mineralization and nitrogen availability (N-NH4+ and N-NO3−) were studied using a first-order model. BC300 and BC400 showed higher soil C mineralization rates and N-NH4+ contents, demonstrating their potential to be used for plant nutrition. Compared to the control, the cumulative C-CO2 emissions increased by 60−64% when biochars BC300 and BC400 were applied to soil. On the other hand, C-CO2 emissions decreased by 6% after the addition of BC500, indicating the predominance of recalcitrant compounds, which results in a lower supply of soil N-NH4+ (83.4 mg kg−1) in BC500, being 67% lower than BC300 (255.7 mg kg−1). Soil N availability was strongly influenced by total N, total C, C/N ratio, H, pore volume, and specific surface area in the biochars.

Os campos nativos do sul do Brasil são utilizados para o pastejo de bovinos e ovinos. Após o verão, no início da estação fria, a fitomassa excedente do pastejo seca, sendo comum sua queima para facilitar o rebrote da pastagem na primavera. No entanto, a queima da fitomassa mineraliza nutrientes e deixa o solo descoberto, potencializando a erosão hídrica. Este trabalho teve o objetivo de quantificar as perdas totais de água e solo e os teores de P, K e NH4+ na água da enxurrada, em campo nativo sobre um Latossolo Bruno aluminoférrico típico. Foram estudados os tratamentos: campo nativo sem queima e sem adubo; campo nativo sem queima e com superfosfato triplo; campo nativo com queima e sem adubo; e campo nativo com queima e com superfosfato triplo. Sobre as parcelas, com 11 m de comprimento, na direção do declive, e 3,5 m de largura, aplicou-se uma chuva simulada com intensidade de 75 mm h-1 e duração de 3 h. A queima influenciou a erosão hídrica e as perdas de nutrientes. A queima da fitomassa do campo nativo diminuiu os tempos de início e pico da enxurrada e a infiltração de água no solo, bem como aumentou a taxa máxima de enxurrada, as perdas de água e solo por erosão hídrica e os teores e as perdas totais de P, K e NH4+ na água de enxurrada, em relação à ausência da queima. A concentração de sedimentos na enxurrada foi maior no tratamento com queima da fitomassa do que no sem queima. O maior e o menor valor da concentração de sedimentos ocorreram em menor tempo de duração do escoamento superficial no tratamento com queima do que no tratamento sem queima, contribuindo para que a perda total de solo fosse 8,9 vezes maior com a queima do que sem a queima do campo. O teor e a perda total de P na água da enxurrada foram maiores no tratamento com adubo fosfatado do que no tratamento sem adubo, tanto no tratamento com queima da fitomassa quanto no sem queima. Para o K e o NH4+, os teores e as perdas totais foram maiores no tratamento com queima do que no sem queima. O modelo exponencial do tipo y = ae-bx ajustou-se aos teores de P, K e NH4+ na água da enxurrada, em relação ao tempo de ocorrência do escoamento superficial (p < 0,01).

O manejo do solo em cultivos perenes, como pomares, influencia a erosão hídrica. O presente estudo avaliou as perdas de solo e água sob chuva simulada em um Latossolo, em pomar de maçã, entre os meses de agosto de 2007 e abril de 2008, na estação experimental de fruticultura de clima temperado da Embrapa Uva e Vinho, em Vacaria (RS). O trabalho foi conduzido em parcelas experimentais de 3,5 x 11 m, sob chuvas com 1 h de duração e intensidade constante ao longo delas, com variação de 70 a 88 mm h-1 entre uma chuva e outra. Os sistemas de manejo estudados foram: 1) capina manual sob a copa das plantas e solo coberto com gramíneas e leguminosas no restante da área (ST); 2) aveia não dessecada, em que as sementes foram incorporadas ao solo, com capina manual em toda a área, dois meses antes do início dos testes de chuva (AN); 3) aveia dessecada quimicamente sete dias antes do início dos testes de chuva, em que as sementes foram incorporadas ao solo com enxada rotativa em toda a área, dois meses antes do início dos testes (AD); e 4) solo sem cobertura, em que a vegetação, após ter sido dessecada, foi removida da superfície do solo em toda a área com capina manual, um dia antes de iniciar os testes de chuva (SC). A forma de manejo da superfície do solo e o número de chuvas influenciaram a erosão hídrica; as perdas de solo variaram amplamente, enquanto as perdas de água apresentaram menor variação. Apesar da mobilização do solo para implantação de aveia, os tratamentos AN e AD com esse cultivo mostraram a mesma eficácia de controle da erosão em relação ao tratamento ST, em que o solo foi mobilizado apenas sob a copa das plantas. A eliminação da cobertura do solo no tratamento SC aumentou expressivamente as perdas de solo em relação aos tratamentos com cobertura; no que se refere às perdas de água, a diferença foi menor. O tempo de ocorrência do escoamento superficial influenciou a perda de solo; observou-se aumento dessa variável com o aumento do tempo de enxurrada até certo momento, a partir do qual diminuiu, independentemente do tratamento; a perda de água aumentou até certo momento e estabilizou. Houve relação inversa entre razão de perda de solo e razão de perda de água, independentemente do tipo de cobertura do solo e do sistema de manejo sob as macieiras. O modelo exponencial ajustou-se a essa relação.

O manejo do solo em cultivos perenes, como pomares, influencia a erosão hídrica. O presente estudo avaliou as perdas de solo e água sob chuva simulada em um Latossolo, em pomar de maçã, entre os meses de agosto de 2007 e abril de 2008, na estação experimental de fruticultura de clima temperado da Embrapa Uva e Vinho, em Vacaria (RS). O trabalho foi conduzido em parcelas experimentais de 3,5 x 11 m, sob chuvas com 1 h de duração e intensidade constante ao longo delas, com variação de 70 a 88 mm h-1 entre uma chuva e outra. Os sistemas de manejo estudados foram: 1) capina manual sob a copa das plantas e solo coberto com gramíneas e leguminosas no restante da área (ST); 2) aveia não dessecada, em que as sementes foram incorporadas ao solo, com capina manual em toda a área, dois meses antes do início dos testes de chuva (AN); 3) aveia dessecada quimicamente sete dias antes do início dos testes de chuva, em que as sementes foram incorporadas ao solo com enxada rotativa em toda a área, dois meses antes do início dos testes (AD); e 4) solo sem cobertura, em que a vegetação, após ter sido dessecada, foi removida da superfície do solo em toda a área com capina manual, um dia antes de iniciar os testes de chuva (SC). A forma de manejo da superfície do solo e o número de chuvas influenciaram a erosão hídrica; as perdas de solo variaram amplamente, enquanto as perdas de água apresentaram menor variação. Apesar da mobilização do solo para implantação de aveia, os tratamentos AN e AD com esse cultivo mostraram a mesma eficácia de controle da erosão em relação ao tratamento ST, em que o solo foi mobilizado apenas sob a copa das plantas. A eliminação da cobertura do solo no tratamento SC aumentou expressivamente as perdas de solo em relação aos tratamentos com cobertura; no que se refere às perdas de água, a diferença foi menor. O tempo de ocorrência do escoamento superficial influenciou a perda de solo; observou-se aumento dessa variável com o aumento do tempo de enxurrada até certo momento, a partir do qual diminuiu, independentemente do tratamento; a perda de água aumentou até certo momento e estabilizou. Houve relação inversa entre razão de perda de solo e razão de perda de água, independentemente do tipo de cobertura do solo e do sistema de manejo sob as macieiras. O modelo exponencial ajustou-se a essa relação.Soil management in perennial crops such as orchards can influence erosion. This study evaluated soil and water losses from an Oxisol under simulated rain, from August 2007 to April 2008, at the experimental station of Embrapa Uva e Vinho, in Vacaria (RS). On the 3.5 m x 11 m plots, rains of one hour were simulated at a constant intensity of 70 to 88 mm h-1. In the apple orchard, the following soil management systems were studied: i) manual weeding under apple trees and spontaneous grass and legume cover in the rest of the area (ST), ii) undesiccated oat cover, hoeing the seeds into the soil at weeding in the entire area, two months before the first rain test (NO), iii) oat cover chemically desiccated seven days before the first rain test, planted by a rotary hoe to incorporate seeds into the soil in the entire area, two months before the tests (DO); and iv) uncovered soil with removal of the previously desiccated spontaneous cover from the soil surface by weeding the entire area with a hoe, one day before each rain test (BS). The management systems related to the soil cover in the apple orchard and the rain tests influenced water erosion. Soil losses varied considerably in the treatments, more than water losses. Even with soil mobilization in the entire area for oat planting in the NO and DO treatments the control effectiveness of water erosion was equal to the ST treatment in which the soil was mobilized only under the trees. The removal of the soil cover from under apple trees greatly increased soil losses in relation to the cover maintenance, but had only little influence on water losses. The runoff duration influenced soil loss; an increase of this variable was observed with increasing runoff duration until a certain moment and, from then on, it decreased independently of the treatment; water loss increased until a certain moment and stabilized. An inverse relationship was observed between soil and water losses, independently of the soil management system under apple trees, adjusting to an exponential model.

O tipo de cultura e a orientação de semeadura em relação ao declive do terreno podem modificar a proporção e o tamanho dos sedimentos transportados na enxurrada, além da relação do teor de C orgânico nos sedimentos e no solo erodido. Este trabalho teve o objetivo de determinar a proporção e o tamanho dos sedimentos transportados pela enxurrada sob taxa constante desta e o teor de C orgânico contido nos sedimentos e no solo erodido, sob duas formas de semeadura das culturas de aveia e ervilhaca. Quatro testes de chuva simulada foram aplicados entre março e novembro de 2006, durante o ciclo vegetativo das culturas, com intensidade constante de 64 mm h-1 e 1 h de duração de cada teste, em Lages, SC, num Cambissolo Húmico com declividade média de 11,9 cm m-1. Os tratamentos eram formados pela combinação de duas culturas e duas orientações de semeadura em relação ao declive. As culturas utilizadas foram aveia (Avena strigosa) e ervilhaca (Vicia sativa); as formas de semeadura eram: mecanizada em linhas em contorno ao declive e mecanizada em linhas paralelas ao declive (morro abaixo). As amostras de enxurrada para a coleta dos sedimentos foram obtidas sob taxa constante de enxurrada, aos 50 min de duração de cada teste de chuva. A aveia reduziu a quantidade de sedimentos na enxurrada em 46 % em relação à ervilhaca, e a semeadura em contorno, em 56 % em relação à semeadura morro abaixo. A proporção de sedimentos na enxurrada foi diminuída em 63 % entre o início e o final do ciclo das culturas. Na classe de menor tamanho dos sedimentos (< 0,038 mm), a aveia aumentou sua proporção em 17 % em relação à ervilhaca, e o contorno os aumentou em 10 % em relação à semeadura morro abaixo. O índice D50 dos sedimentos presentes na enxurrada foi de 0,043 mm na aveia e 0,119 mm na ervilhaca, e de 0,047 mm na semeadura em contorno e 0,117 mm na semeadura morro abaixo. A razão entre o teor de C orgânico dos sedimentos transportados pela enxurrada e o teor de C do solo na camada de 0-2,5 cm foi de 1,39 na aveia e 1,21 na ervilhaca, e de 1,43 na semeadura em contorno e 1,17 na semeadura morro abaixo.The crop type and seed row direction in relation to the land slope can modify the total amount and size of runoff-transported sediment. They may alter the relation between organic carbon levels in the sediments and the eroded soil. The current study aimed to quantify the sediment size and proportion transported at constant runoff rate and the organic carbon level in the sediments and the eroded soil, under oat and vetch sown in two row directions. Four simulated rainfalls were applied between March and November 2006, during the crop cycle, at a constant intensity of 64 mm h-1 for one hour, in Lages, Santa Catarina, Brazil, to an Inceptisol with a slope of 0.119 m m-1. The treatments consisted of the combination of two crops and two seed row directions in relation to the slope. Oat (Avena strigosa) and vetch (Vicia sativa) were sown mechanically in parallel downhill rows and contour rows of the slope. Runoff sediment was sampled in a set of sieves that collected the constant rate runoff flow for 50 min during each rain test. Oat cropping decreased the amount of runoff-transported sediment by 46 % in comparison to vetch cropping and the contour seed row reduced this by 56 % in relation to downhill seed row. The proportion of sediments in runoff decreased 63 % from the start to the end of the crop cycle. The proportion of the fine size sediment class (< 0.038 mm) was 17 % higher under oat than vetch, and the contour seed row increased the proportion by 10 % in comparison with the downhill seed row. The D50 sediment index in runoff was 0.043 mm in oat and 0.119 mm in vetch; it reached 0.047 mm in the contour and 0.117 mm in the downhill seed rows. The ratio between organic carbon level in sediments and in the 0-2.5 cm soil layer was 1.39 in oat, 1.21 in vetch, 1.43 in the contour and 1.17 in downhill seed rows.

Biochar effects on soil microbial abundance and community structure are keys for understanding the biogeochemical cycling of nutrients and organic matter turnover, but are poorly understood, in particular in tropical areas. We conducted a greenhouse experiment in which we added biochars produced from four different feedstocks [sewage sludge (B1), deinking sewage sludge (B2), Miscanthus (B3) and pine wood (B4)] at a rate of 3% (w/w) to two tropical soils (an Acrisol and a Ferralsol) planted with proso millet (Panicum milliaceum L.). The interactive effect of the addition of earthworms was also addressed. For this purpose we utilized soil samples from pots with or without the earthworm Pontoscolex corethrurus, which is a ubiquitous earthworm in tropical soils. Phospholipid fatty acid (PLFA) measurements showed that biochar type, soil type and the presence of earthworms significantly affected soil microbial community size and structure. In general, biochar addition affected fungal but not bacterial populations. Overall, biochars rich in ash (B1 and B2) resulted in a marked increase in the fungi to bacteria ratio, while this ratio was unaltered after addition of biochars with a high fixed carbon content (B3 and B4). Our study remarked the contrasting effect that both, biochar prepared from different materials and macrofauna, can have on soil microbial community. Such changes might end up with ecosystem-level effects.

Proper and effective management of soil nutrients requires assessment of their variability at the field scale. We compare the effects of lime amendment rate on the spatial variability of three macronutrient forms (NH4+-N, Olsen P, and Mehlich-1 K) in a paddy soil at three different dates during the growth period of a rice crop. The field work was carried out near Corrientes, Argentina. Lime treatments were 0, 625, and 1250 kg ha−1 dolomite, and each liming dose was applied to a 1.7 ha field. Ninety-three soil samples per treatment were first collected in aerobic conditions and then two more times after flooding, at bunch formation and flowering. Soil NH4+-N increased along time, whereas P was highest at bunch formation and K steadily decreased along the rice growth period. Dolomite addition increased macronutrient availability at the first and second samplings, but its effects at the third sampling depended on the element. The three soil nutrients analyzed displayed strong patterns of spatial dependence for the three lime treatments and at the three periods studied. The areas with relative high or low macronutrient concentrations within each field were not stable throughout the rice growth period. Seasonality in the spatial distribution of macronutrients may be of agronomic value for site specific management.

Phytoremediation of soils contaminated with cadmium was tested after liming (CaO) or biochar addition, using red amaranth (Amaranthus tricolor L.) as test plant species. Two biochars with contrasting characteristics were prepared from two feedstocks and added to the soil at a rate of 3% (w:w): Eucalyptus pyrolysed at 600°C (EB) and poultry litter at 400°C (PLB). Liming was carried out in two treatments (CaO1) and (CaO2) to the same pH as the treatments EB and PLB respectively. Total plant mass increased in soils amended with PLB and with a mixture of PLB and EB; however this was not sufficient to increase the efficiency of phytoextraction. Bioavailable and mobile fractions of Cd diminished after liming or biochar addition. Our study infers that, both the amount of Cd immobilized and the main mechanism responsible for this immobilization varies according to biochar properties.

The effect of organic matter addition on Ba availability to Helianthus annuus L., Raphanus sativus L., and Ricinus communis L. grown on a Neossolo Litólico Chernossólico fragmentário (pH 7.5), contaminated with scrap residue was evaluated. Four rates (0, 20, 40, and 80 Mg ha−1, organic carbon basis) of peat or sugar cane filter, with three replicates, were tested. Plant species were grown until the flowering stage. No effect of organic matter addition to soil on dry matter yield of oilseed radish shoots was observed, but there was an increase in sunflower and castor oil plant shoots when sugar cane filter cake was used. The average Ba transferred from roots to shoots was more than 89% for oilseed radish, 71% for castor oil plants, and 59% for sunflowers. Organic matter treatments were not efficient in reducing Ba availability due to soil liming.

Soil microbes play a key role in nutrient cycling and carbon sequestration. Global change can alter soil microbial population composition and behavior. Biochar addition has been explored in the last years as a way to mitigate global warming. However, responses of microbial communities to biochar addition in particular in relation to abiotic disturbances are seldom documented. An example of these disturbances, which is predicted to be exacerbated with global warming, is regional drought. It has been known that fungal-based food webs are more resistant to drought than their bacterial counterparts. Our study found that biochar addition can increase the resistance of both the bacterial and fungal networks to drought. Contrary to expected, this result was not related to a change in the dominance of fungal or bacteria. In general, soil amended with biochar was characterized by a faster recovery of soil microbial properties to its basal values. Biochar addition to the soil also suppressed the Birch effect, a result that has not been previously reported.