Renewing carbon and re-establishing it again in the soil is one of the valuable means to cope with climate change. There are many technologies for carbon apprehension and storage, but the most important one gaining attention is biochar technology. So, to carbonize and return different biological materials back to the farmland, a comprehensive study was proposed to characterize and evaluate the carbon (C) mineralization of biochars produced from different animal manures and crop straws. Six types of biochars were prepared from animal manures (poultry litter, swine and cattle manures) and crop straws (rice, soybean, and corn straws). The biochars were analyzed for chemical characteristics (elemental variables, thermal decomposition, cation exchange capacity, pH, electrical conductivity, specific surface area, and surface functional groups) and an incubation experiment was conducted to evaluate C mineralization from soil biochar mixture. Biochars produced from crop straws resulted to have more C as compared to the biochars produced from animal manures. Concentration of nitrogen was low, while P, K, Ca, and Mg were found reasonably higher in all biochars except swine manure biochar. The plant-derived biochars presented lower CO₂emissions when incorporated to soil at 1 and 2% of C. Varying but all the biochars prepared represented an alkaline pH. Biochars prepared from the crop straws resulted to have more C, alkaline in nature, high CEC, low CO₂emissions, can sequester C and more suitable to enhance the soil fertility in comparison to biochars produced from other sources.

High copper (Cu) soil contents, due to the continuous vineyard application of Cu fungicides throughout the years, may impair the growth of the shoot and modify the structure of the root system. The current study aimed to investigate the threshold levels of available Cu in the soil causing toxicity effects in young grapevine plants of 'Red Niagara' cultivated in clay soils. Grapevine plantlets were cultivated in pots containing vineyard devoted soils with increasing contents of available Cu (25, 80, 100 and 165 mg kg-1), for 53 days. Photosynthesis and transpiration rates, and the quantum yield of photosystem II (Fv/Fm) were evaluated during the cultivation period. At the end of the experiment, the plant nutrient and leaf chlorophyll were determined, along with the anatomical analysis of the root system structure and plant dry matter determination. Higher levels of available Cu in the soil increased the apoplastic, symplastic and total fraction of the metal in the roots, reducing the other nutrients, especially in the shoots. Photosynthesis, transpiration rates and Fv/Fm were also reduced. Higher levels of Cu led to anatomical changes in the roots, that increased diameter, number of layers in the cortex, vascular cylinder and total root areas. It also resulted in reduced dry matter production by grapevines.

As aplicações sucessivas de dejeto líquido de suínos no solo podem aumentar os teores e alterar as formas de Cu e Zn no solo. O presente trabalho teve como objetivo estimar o acúmulo de Cu e Zn e suas formas em solo submetido a aplicações sucessivas de dejeto líquido de suínos, em sistema plantio direto com rotação de culturas. O trabalho foi desenvolvido em um Argissolo Vermelho distrófico arênico na área experimental do Departamento de Engenharia Agrícola da Universidade Federal de Santa Maria (RS). Os tratamentos consistiram na aplicação de 0, 20, 40 e 80 m³ ha-1 de dejeto líquido de suínos. Foram realizadas 17 aplicações de dejetos de maio de 2000 até o momento da coleta do solo, em outubro de 2006. Amostras de solo foram coletadas nas camadas de 0-2, 2-4, 4-6, 6-8, 8-10, 10-12, 12-14, 14-16, 16-18, 18-20, 20-25, 25-30, 30-35, 35-40, 40-50 e 50-60 cm, secas ao ar, passadas em peneiras de 2 mm e moídas em grau de ágata. Em seguida, foram preparadas e analisados os teores pseudototais após extração pelo método 3050B da EPA, disponíveis por meio da extração com HCl 0,1 mol L-1, além do fracionamento químico do Cu e do Zn. Nos dejetos de suínos foram determinados os teores pseudototais de Cu e Zn. As aplicações sucessivas de dejeto líquido de suínos no solo aumentaram os teores de Cu e Zn das camadas superficiais, com migração até 12 e 10 cm de profundidade, respectivamente. O Cu e Zn adicionados são acumulados no solo em formas biodisponíveis, sendo preferencialmente ligados às frações orgânica e mineral, respectivamente. Successive applications of pig slurry in the soil can increase the levels and change the forms of copper (Cu) and zinc (Zn). The objective of this study was to evaluate Cu and Zn accumulation and forms in the soil of areas with successive pig slurry applications under no tillage crop rotation. The experiment was carried out in a Typic Hapludalf in the experimental area of the Department of Agricultural Engineering of the Federal University of Santa Maria, Santa Maria (RS), Brazil. Pig slurry was applied at rates of 0, 20, 40 and 80 m³ ha-1. A total of 17 applications were applied to the soil surface between May 2000 and October 2006. The soil samples were collected in the layers 0-2, 2-4, 4-6, 6-8, 8-10, 10-12, 12-14, 14-16, 16-18, 18-20, 20-25, 25-30, 30-35, 35-40, 40-50, and 50-60 cm. The soil was dried, ground, sieved (2 mm) and the pseudo-total levels, available (HCl 0.1 mol L-1) and chemical fractions of Cu and Zn were determined. The pseudo-total contents of copper and zinc in the slurry were analyzed. Successive applications of pig slurry increased the pseudo-total content of copper and zinc in soil (surface layers), with migration to 12 and 10 cm depths, respectively. The Cu and Zn applied were accumulated in the soil in bioavailable forms, and preferentially associated with the organic and mineral fraction, respectively

After flooding in rice crops, the Fe³⁺ ions from iron oxide minerals are reduced to Fe²⁺ in the anaerobic conditions, making it soluble. The excess of Fe²⁺ in soil solution can be toxic to plants, resulting in decreasing rice yield. Pyrolyzed materials from rice crop residues, such as rice husk, can be an environmentally friendly option to reduce iron availability in soil solution, provided they have appropriate chemical and physical characteristics regarding iron adsorption. In this study, rice husk biochar (RHB) and rice husk ashes (RHA1 and RHA2) were characterized regarding physical and chemical characteristics and the iron adsorption capacity. The different oxygenation conditions in obtaining the materials resulted in chemical and physical differences (e.g., biochar carbon content of 46% and ashes of 16% and 0.93%), but there were no significant differences related to iron adsorption capacity in aqueous solution. The iron adsorption capacity of the biochar was 5.53 mg Fe²⁺ g⁻¹ and of the ashes was 6.74 and 7.22 mg Fe²⁺ g⁻¹ for the two materials tested, which demonstrates potential of these materials to mitigate iron toxicity in flooded rice crops.

Pig slurry application as soil manure can alter the chemical properties of the soil and affect its acidity, modifying the environment for crop growth and development. The objective of this study was to evaluate the chemical properties related to soil acidity subjected to successive applications of pig slurry. The experiment was conducted in May 2000, in an experimental area of the Federal University of Santa Maria (UFSM) under no-tillage and lasted until January 2008. Nineteen surface applications of 0, 20, 40, and 80 m³ ha-1 of pig slurry were performed, during a period of 100 months and the soil sampled in the end (layers 0-2, 2-4, 4-6, 6-8, 8-10, 10-12, 12-14, 14-16, 16-18, 18-20, 20-25, 25-30, 30-35, 35-40, 40-50 and 50-60 cm). The application of pig slurry increased soil pH values, an effect that could reach the depth of 8 cm without affecting the potential acidity values. The applications also resulted in accumulation of Ca and Mg exchangeable levels in the surface layers, increasing base saturation and reducing Al saturation. Long-term applications induced an increase in organic matter in the deeper layers. However, the effect of this residue on the potential CEC was less significant and restricted to the surface layers.