Tillage and nutrient management influence net global warming potential and greenhouse gas intensity in soybean-wheat cropping system

Conservation tillage has proven advantageous in improving soil health and productivity. However, the greenhouse gases (GHGs) emission and intensity from different conservation tillage and nutrient management systems under Indian conditions are less understood. Therefore, here, we compared the effect of tillage and nutrient management on GHGs emissions, net global warming potential (NGWP), and greenhouse gas intensity (GHGI) from a field experiment under five years in a soybean-wheat cropping system in the Vertisols. The tillage treatments comprised of reduced tillage (RT) and no tillage (NT). The three nutrient management treatments included application of 100% NPK (T1), 100% NPK + 1.0 Mg FYM-C ha-1 (T2), 100% NPK +2.0 Mg FYM-C ha-1 (T3). The results showed significantly higher SOC sequestration under NT (1388 kg ha-1 yr-1) followed byRT (1134 kg ha-1 yr-1) with application of FYM (2.0 Mg C ha-1) (T3) every year. Across tillage, integrated nutrient management(T2 and T3) lowered NGWP and GHGI compared to NPK (T1). The GHGI of NT system was less by 33% compared to RT. The results suggest that GHGs mitigation and sustained food production in the soybean-wheat system can be achieved in NT and RT with integrated use of organic and inorganic fertilizer as the major component of nutrient management.

Biodegradação do herbicida atrazina por Saccharomyces cerevisiae / Biodegradation of the atrazine herbicide by Saccharomyces cerevisiae

RESUMO Tendo em vista os vários problemas ambientais e de saúde que o uso crescente de agrotóxicos vem causando, é necessário a otimização de técnicas que visem a sua rápida degradação. A atrazina é um herbicida utilizado no controle de ervas daninhas, principalmente nas culturas de milho e cana-de-açúcar. Nesse sentido, o objetivo deste estudo foi verificar a eficiência da levedura Saccharomyces cerevisiae na degradação do herbicida atrazina em solo contaminado com diferentes concentrações do produto comercial. Foi igualmente testado o efeito da adição de palha de milho no experimento. A fim de determinar a quantidade de gás carbônico (CO2) liberado durante os ensaios, o qual reflete a atividade da microbiota do solo responsável pela degradação de compostos orgânicos, foi utilizada a técnica da respiração basal do solo. E, paralelamente a isso, para verificar a concentração de atrazina ao longo do experimento (tempo inicial, aos 7, 14 e 63 dias), foi utilizada a análise de cromatografia gasosa acoplada ao espectrômetro de massas (CG-MS). Por meio da análise estatística dos dados de respiração basal do solo, o fator de bioaumento com a levedura foi o mais significativo, seguido da adição de palha de milho. Verificou-se o declínio da concentração de atrazina por intermédio das análises cromatográficas. Assim, sugere-se que a biorremediação com S. cerevisiae tem potencial para elevar as taxas de degradação do herbicida no solo.

ABSTRACT Considering the various environmental and health problems that the increasing use of pesticides has been causing, it is necessary to optimize techniques aimed at their rapid degradation. Atrazine is a herbicide used to control weeds, especially in maize and sugarcane crops. Thus, the objective of this study was to verify the efficiency of the Saccharomyces cerevisiae yeast in the degradation of the herbicide atrazine in soil contaminated with different concentrations of the commercial product. The effect of addition of corn straw on the experiment was also tested. In order to determine the amount of carbon dioxide (CO2) released during the tests, which reflects the activity of the soil microorganism responsible for the degradation of organic compounds, the soil basal respiration technique was used. At the same time, the concentration of atrazine during the experiment (start time, at 7, 14, and 63 days) was analyzed by gas chromatography coupled to the mass spectrometer (CG-MS). Through the statistical analysis of the basal respiration data of the soil, the bioaugmentation factor with yeast was the most significant, followed by the addition of corn straw, and the decline in atrazine concentration was verified through chromatographic analyses. Thus, it is suggested that bioremediation with S. cerevisiae has the potential to increase the rates of degradation of the herbicide in the soil.

How different soil moisture levels affect the microbial activity / Como diferentes níveis de umidade do solo afetam a atividade microbiana de um solo de terras baixas usado para cultivo do arroz?

ABSTRACT: The lowland soils are characterized by high susceptibility to water saturation. This anaerobic condition is usually reported in paddy fields and alters the decomposition process of soil organic compounds. The aim of this study was to evaluate the soil microbial and enzymatic activity of a lowland soil at different soil moisture contents. A poorly drained Albaqualf cultivated with irrigated rice was used to evaluate microbial and enzymatic activity in treatments with different levels of soil moisture, being: i) 60% of field capacity (FC) (60%FC); ii) 100% of FC (100%FC); iii) flooded soil with a 2 cm water layer above soil surface, and iv) soil kept at 60%FC with late flood after 29 days the incubation. The greater soil microbial activity was observed in the 100%FC treatment, being 41% greater than 60%FC treatment and only 2% higher than flooded treatment. The enzymatic activity data by fluorescein diacetate (FDA) hydrolysis corroborated the higher CO2 release in treatments with higher soil moisture content. Differently from the results reported, the main methodologies to evaluate microbial activity still recommend maintenance of the soil with a moisture content close to 60% of the FC. However, in lowland soil with history of frequent paddy fields, the maintenance of moisture close to 60% of the FC can limit the microbial activity. The soil respiration technique can be used to evaluate the microbial activity in flooded soil conditions. However, further studies should be conducted to understand the effect of the cultivation history on the microbial community of these environments.

RESUMO: Os solos de várzea são caracterizados pela alta suscetibilidade à saturação por água. Esta condição anaeróbica é geralmente encontrada em solos arrozeiros e altera o processo de decomposição dos compostos orgânicos do solo. O objetivo deste estudo foi avaliar a atividade microbiana e enzimática de um solo de várzea sob diferentes teores de umidade no solo. Um Planossolo historicamente cultivado com arroz irrigado foi utilizado para avaliar a atividade microbiana e enzimática em tratamentos com diferentes níveis de umidade do solo, sendo: i) 60% de capacidade de campo (CC) (60%CC); ii) 100% da CC (100%CC); iii) solo inundado com uma camada de água de 2 cm acima da superfície do solo; e iv) solo mantido a 60%CC com inundação após 29 dias da incubação. A maior atividade microbiana do solo foi observada no tratamento 100%CC, sendo 41% maior que o tratamento 60%CC e 2% maior que tratamento inundado. Os dados da atividade enzimática pela hidrólise do diacetato de fluoresceína (FDA) corroboraram a maior liberação de CO2 nos tratamentos com maior umidade do solo. Diferentemente dos resultados encontrados, as principais metodologias para avaliação da atividade microbiana ainda recomendam manter o solo com umidade próxima a 60% da CC. No entanto, em solos de várzea com históricos de cultivos de arroz, a manutenção de umidade próxima a 60% da CC pode limitar a atividade microbiana. A técnica de respiração do solo pode ser usada para avaliar a atividade microbiana em condições de solo inundado. No entanto, mais estudos devem ser realizados para entender o efeito do histórico de cultivo na comunidade microbiana nesses ambientes.

Short-term effects of byproduct amendments and lime on physicochemical and microbiological properties of acidic soil from Jiaodong Peninsula of China / Efeitos de alterações de subprodutos e cal em solo ácido da Península de Jiaodong da China

ABSTRACT: The influences of byproduct amendments, containing silicon, calcium, magnesium and potassium, on acidic soil quality in Jiaodong Peninsula of China had been studied and compared with that of lime through monitoring physicochemical properties and enzyme activities of acidic soil over a 120-day period. Byproduct amendments (1125, 2250, 4500 and 9000 kg ha-1) and lime 2250 kg ha-1 was applied in the acidic soil. Results showed that both byproduct amendments and lime significantly increased the pH, EC and enzyme activities of soil. The by-product amendments inhibited microbial biomass carbon and soil respiration. Nevertheless, the lime-treated soil had a much more higher level of CO2 emission than the by-product amendments-treated soil. Compared to the by-product amendments-treated soil, the lime-treated soil had the higher pH, peroxidase activity, phenol oxidase activity and invertase activity. Therefore, lime might be a better choice over by-product amendments to improve chemical and biological properties of the acidic soil in Jiaodong Peninsula of China. For soils lacking available calcium and magnesium, the mixture of 4500 kg ha-1 amendments and 2250 kg ha-1 lime was recommend to treat the soil.

RESUMO: As influências do emprego de subprodutos que contêm silício, cálcio, magnésio e potássio, sobre a qualidade do solo ácido na Península de Jiaodong da China, foram estudadas e comparadas com a da cal através do monitoramento das propriedades físico-químicas e atividades enzimáticas do solo ácido ao longo de um 120- período do dia. Os resultados mostraram que as alterações dos subprodutos e a cal aumentaram significativamente as atividades de pH, CE e enzimas do solo. As alterações dos subprodutos obviamente inibiram o carbono da biomassa microbiana e a respiração do solo, mas o solo tratado com cal apresentou um maior nível de emissão de CO2. Em comparação com as modificações do subproduto, o solo tratado tinha o maior pH, a atividade da peroxidase, a atividade da fenol oxidase e a atividade da invertease. Portanto, o cal pode ser uma escolha melhor em relação às alterações dos subprodutos para melhorar as propriedades químicas e biológicas do solo ácido na Península de Jiaodong da China.

Variação temporal do efluxo de CO2do solo em sistemas agroflorestais com palma de óleo na Amazônia Oriental / Temporal variation of soil CO2 efflux in oil palm-based agroforestry systems in eastern Amazon

The soil carbon dioxide (CO2) efflux dynamics and its controlling factors of Amazonian agroforestry systems are poorly understood. The objective of this study was to evaluate the temporal variation of soil CO2 efflux in oil palm-based agroforestry systems and the relation between efflux and biotic (microbial and total soil carbon, microbial respiration, fine roots, individual components of agroforestry systems (AFS)) and abiotic factors (soil moisture and temperature). The measurements were taken during the less rainy (December 2010) and rainy (May 2011) periods. The soil CO2 efflux was highest during the rainy season, probably due to increased microbial activity influenced by climatic factors coupled with biotic factors. The soil CO2 efflux correlated positively with soil moisture and microbial biomass carbon and negatively with soil temperature and metabolic quotient, but these correlations were weak. The soil CO2 efflux was sensitive to the type of agroforestry system and to rainfall seasonality.

A dinâmica do efluxo de dióxido de carbono (CO2) do solo e seus fatores controladores em sistemas agroflorestais da Amazônia são pouco compreendidas. O objetivo deste estudo foi avaliar a variação temporal do efluxo de CO2 do solo em sistemas agroflorestais onde a palma de óleo é a cultura principal e sua relação com fatores bióticos (carbono microbiano do solo, carbono total do solo, respiração microbiana do solo, raízes finas do solo, indivíduos componentes dos sistemas agroflorestais (SAFs) ) e abióticos (umidade e temperatura do solo). As medições foram realizadas nos períodos menos chuvoso (dezembro de 2010) e chuvoso (maio de 2011). O efluxo de CO2 do solo foi mais alto no período chuvoso, provavelmente, devido à maior atividade microbiana nesse período influenciada por fatores climáticos aliados a fatores bióticos. O efluxo de CO2do solo se correlacionou positivamente com umidade do solo e carbono da biomassa microbiana e negativamente com temperatura do solo e quociente metabólico, porém as correlações foram fracas. O efluxo de CO2do solo foi sensível ao tipo de sistema agroflorestal e a sazonalidade da precipitação.

Soil microbial biomass and activity in wetlands located in preserved and disturbed environments in the cerrado biome / Biomassa e atividade microbiana do solo em veredas situadas em ambientes conservados e antropizados no bioma cerrado

The veredas (a type of wetlands) are wet ecosystems usually associated with the presence of hydromorphic soils, which often occur in the vicinity of springs and watercourses of the Cerrado region in Brazil. This study aimed to assess microbiological and biochemical soil properties in wetlands (veredas) located in preserved and disturbed environments (in farming and grazing areas) in the Cerrado biome. Soil samples were collected at depths of 0-10 cm and 10-20 cm, along reference lines arranged according to their position in the landscape, in the upper, middle and lower positions of one of the slopes. The total soil organic carbon, microbial biomass carbon and nitrogen (Cmic and Nmic), microbial biomass C:N ratio, microbial quotient, basal respiration, metabolic quotient and fluorescein diacetate (FDA) hydrolytic activities in soil (as total soil heterotrophic enzymatic activity) were determined. The soils of veredas adjacent to agricultural and livestock environments showed changes in their biological properties compared to preserved ecosystems. Increased microbial biomass (Cmic and Nmic) is reported in veredas located nearby grazing areas under intensive and technified management, on the soil surface layer (0-10 cm), especially in the lower slope position, while in agricultural environments, under the same conditions of relief and depth, there is a relative decrease in microbial biomass carbon.

As veredas são ecossistemas úmidos, normalmente associados à presença de solos hidromórficos, que ocorrem com frequência nas proximidades das nascentes e cursos d'água da região do Cerrado. O objetivo deste trabalho foi avaliar atributos microbiológicos e bioquímicos do solo em áreas úmidas (veredas) localizadas em ambientes conservados e antropizados (em áreas agrícolas e pastagens), no bioma Cerrado. Amostras de solo foram coletadas nas profundidades de 0-10 cm e 10-20 cm, ao longo de linhas de referência dispostas, segundo sua posição no relevo, nas posições superior, média e inferior de uma das vertentes. Foram determinados o carbono orgânico total do solo, carbono e nitrogênio da biomassa microbiana (Cmic e Nmic), relação C:N da biomassa microbiana, quociente microbiano, respiração basal, quociente metabólico e atividade enzimática total do solo. Os solos de veredas vizinhas a ambientes agropecuários apresentaram variações em seus atributos biológicos, comparativamente a ecossistemas conservados. Em veredas adjacentes a pastagens sob manejo intensivo tecnificado, na camada superficial do solo (0-10 cm), ocorreu o incremento da biomassa microbiana (Cmic e Nmic), notadamente na posição inferior do relevo, enquanto em ambientes agrícolas, nas mesmas condições de relevo e profundidade, observou-se uma diminuição relativa do carbono da biomassa microbiana.

Efeitos de herbicidas na atividade da microbiota rizosférica e no crescimento da cana-de-açùcar / Herbicide effects on the atividadade rhizospheric microbial and growth of sugar cane

Objetivou-se neste trabalho avaliar os efeitos de herbicidas na atividade da microbiota rizosférica e no crescimento da cana-de-açúcar. Para isso, sete herbicidas (tembotrione, MSMA, diuron+hexazinone, sulfentrazone, trifloxysulfuron-sodiun, tebuthiuron e clomazone) foram aplicados em pós-emergência da cana-de-açúcar cultivada em vaso contendo 12 dm3 de substrato (solo + fertilizantes). Foram avaliados os efeitos desses produtos na evolução do CO2 do solo (C-CO2), no carbono da biomassa microbiana (CBM), no quociente metabólico (qCO2), na atividade da enzima fosfomonoesterase ácida do solo rizosférico em amostras de solo coletadas aos 44 dias após aplicação dos herbicidas (DAT) e os efeitos no crescimento aos 77 DAT. Inicialmente os herbicidas MSMA, clomazone, sulfentrazone e trifloxysulfuron-sodium causaram intoxicação à cultura. Todavia, apenas nas plantas tratadas com o trifloxysulfuron-sodium esses sintomas permaneceram visíveis no momento da colheita do experimento. Quanto aos efeitos dos herbicidas sobre a atividade da microbiota rizoférica da cana-de-açúcar, o sulfentrazone e tebuthiuron reduziram a C-CO2 e o MSMA, tebuthiuron e clomazone reduziram o CBM do solo. O clomazone foi o herbicida que causou o maior impacto na atividade da microbiota, pois aumentou o valor do qCO2. Por outro lado, o sulfentrazone reduziu os valores dessa variável, contribuindo para o equilíbrio da microbiota no solo. Não houve influência dos herbicidas na atividade da fosfomonoesterase ácida do solo rizosférica da cana-de-açúcar.

The objective of this study was to evaluate the effects of herbicides used in their recommended doses, on the activity of the microbiota and sugar cane growth. For this, seven herbicides (tembotrione, MSMA, hexazinone + diuron, sulfentrazone, trifloxysulfuron-sodiun, and tebuthiuron cloamzone) were applied in pots containing 12 dm3 substrate (soil + fertilizer) at 50 days after sugarcane planting. The effects of these products on the evolution of soil CO2 (CO2-C), in the microbial biomass carbon (MBC), metabolic quotient (qCO2), enzyme activity in the rhizosphere acid phosphomonoesterase in rhizosphere soil samples collected at 44 days after herbicide application (DAT) and the growth effects at 77 DAT. Initially herbicides MSMA, clomazone, sulfentrazone and trifloxysulfuron-sodium caused poisoning in culture. However, only plants treated with trifloxysulfuron-sodium, these symptoms remained visible at harvest of the experiment. The effects of herbicides on microbial activity rizoferica of sugar cane, sulfentrazone and tebuthiuron reduced CO2-C and MSMA herbicide clomazone and reduced the CBM soil. The herbicide clomazone was that caused the greatest impact on microbial activity because of the increased value qCO2. Moreover, the sulfentrazone reduced values of that variable, contributing to the balance of microflora in the soil. No influence of herbicides on the activity of acid phosphomonoesterase rhizospheric on the sugarcane soil.

Mild salinization stimulated glyphosate degradation and microbial activities in a riparian soil from Chongming Island, China.

An incubation experiment was conducted to investigate the effects of simulated saltwater treatment with different percentages of artificial seawater on degradation dynamics of herbicide glyphosate and microbial activities in a riparian soil in Chongming Island, China. The results showed that 10% seawater treatment showed significantly enhancing effects on degradation efficiency of glyphosate with the lowest residual concentration among all the treatments. However, glyphosate degradation was markedly decreased in the riparian soil with 20% and 50% seawater treatments. The half-lives for 20% and 50% seawater treatments were prolonged by 12.1 and 39.0%, respectively, as compared to control. Microbial investigation indicated that 10% seawater treatment significantly stimulated microbial activities in the glyphosate-spiked riparian soil throughout the incubation period. At 42 day of incubation experiment, flourescein diacetate (FDA) hydrolysis rate, microbial adenosine triphosphate (ATP), and basal soil respiration (BSR) in the glyphosate-spiked riparian soil with 10% seawater were 59.2, 42.5 and 31.8% higher than those with no saltwater treatment, respectively. In contrast, saltwater treatment with 50% seawater significantly inhibited microbial activities. Especially, FDA hydrolysis rate, microbial ATP and BSR were decreased by 66.4, 58.6 and 66.8%, respectively, as compared to control. The results indicate that levels of simulated saltwater can exert variable effects on herbicide degradation dynamics and microbial parameters in the riparian soil.

Soil CO2 efflux in central Amazonia: environmental and methodological effects / Efluxo de CO2 do solo na Amazônia central: efeitos ambiental e metodológico

Soil respiration plays a significant role in the carbon cycle of Amazonian rainforests. Measurements of soil respiration have only been carried out in few places in the Amazon. This study investigated the effects of the method of ring insertion in the soil as well as of rainfall and spatial distribution on CO2 emission in the central Amazon region. The ring insertion effect increased the soil emission about 13-20 percent for sandy and loamy soils during the firsts 4-7 hours, respectively. After rainfall events below 2 mm, the soil respiration did not change, but for rainfall greater than 3 mm, after 2 hours there was a decrease in soil temperature and respiration of about 10-34 percent for the loamy and sand soils, with emissions returning to normal after around 15-18 hours. The size of the measurement areas and the spatial distribution of soil respiration were better estimated using the Shuttle Radar Topographic Mission (SRTM) data. The Campina reserve is a mosaic of bare soil, stunted heath forest-SHF and tall heath forest-THF. The estimated total average CO2 emissions from the area was 3.08±0.8 µmol CO2 m-2 s-1. The Cuieiras reserve is another mosaic of plateau, slope, Campinarana and riparian forests and the total average emission from the area was 3.82±0.76 µmol CO2 m-2 s-1. We also found that the main control factor of the soil respiration was soil temperature, with 90 percent explained by regression analysis. Automated soil respiration datasets are a good tool to improve the technique and increase the reliability of measurements to allow a better understanding of all possible factors driven by soil respiration processes.

Respiração do solo possui um importante papel no ciclo do carbono em florestas tropicais Amazônicas. Entretanto poucas medidas de respiração do solo foram feitas. Neste estudo são apontados os efeitos na metodologia de instalação dos anéis no solo, bem como os efeitos da precipitação e a distribuição espacial da emissão de CO2 na Amazônia central. Os efeitos da inserção de anéis no solo aumentaram de 13 a 20 por cento para o solo arenoso e argiloso, o efeito durou de 4 a 7 horas, respectivamente. Já os efeitos na precipitação, notamos que os eventos abaixo de 2 mm a respiração do solo permaneceu indiferente, mas para precipitação acima de 3 mm, 2 horas depois, houve uma diminuição da temperatura e respiração em 10 a 34 por cento para o solo argilosos e arenosos, retornando a emissão normal após 15 a 18 horas. Para estimar a distribuição espacial da respiração do solo e o tamanho correto das áreas medidas, foram utilizadas as imagens do Shuttle Radar Topographic Mission (SRTM). Considerando que a Reserva de Campina é um mosaico de solo desnudo, floresta alagável de baixa e alta estatura (SHF e THF). A emissão total média de CO2 para a área foi de 3.08±0.8 µmol CO2 m-2 s-1. Já a Reserva do Cuieiras possui outro mosaico de florestas de platôs, encostas, Campinaranas e riparias, sendo a emissão média total desta área foram de 3.82±0.76 µmol CO2 m-2 s-1. Encontramos também que a respiração do solo foi controlada pela temperatura do solo, sendo uma correlação de 90 por cento encontrada pela análise de regressão. Dados obtidos com sistema automático de respiração do solo é uma grande oportunidade de melhoramento da técnica e o aumento da confiança nas medidas em relação aos possíveis fatores que controlam os processos de emissão de CO2 do solo.

Conservation tillage, optimal water and organic nutrient supply enhance soil microbial activities during wheat (Triticum Aestivum L.) cultivation

The field experiments were conducted on sandy loam soil at New Delhi, during 2007 and 2008 to investigate the effect of conservation tillage, irrigation regimes (sub-optimal, optimal and supra-optimal water regimes), and integrated nutrient management (INM) practices on soil biological parameters in wheat cultivation. The conservation tillage soils has shown significant (p<0.05) increase in soil respiration (81.1 percent), soil microbial biomass carbon (SMBC) (104 percent) and soil dehydrogenase (DH) (59.2 percent) compared to the conventional tillage soil. Optimum water supply (3-irrigations) enhanced soil respiration over sub-optimum and supra-optimum irrigations by 13.32 percent and 79 percent respectively. Soil dehydrogenase (DH) activity in optimum water regime has also increased by 23.33 percent and 8.18 percent respectively over the other two irrigation regimes. Similarly, SMBC has also increased by 12.14 percent and 27.17 percent respectively in soil with optimum water supply compared to that of sub-optimum and supra-optimum water regime fields. The maximum increase in soil microbial activities is found when sole organic source (50 percent Farm Yard Manure+25 percent biofertilizer+25 percent Green Manure) has been used in combination with the conservation tillage and the optimum water supply. Study demonstrated that microbial activity could be regulated by tillage, water and nitrogen management in the soil in a sustainable manner.

Field measurements of soil CO2 efflux in Heteropogon contortus do minated grassland of semi-arid eco-system.

Seasonal changes in soil respiration (SR), soil temperature (ST) and soil moisture (SM) were compared between a barren land with no vegetation (control) and grassland dominated by Heteropogon contortus (L.) of a semi-arid eco-system during 2005-2006. A statistically significant (p<0.001) seasonal change in SR was observed between the two sites. The variation characteristics of soil CO2 efflux rates were observed during wet periods along precipitation gradients and it was consistently higher in grasslands than in control. A maximum soil CO2 efflux of 13.35 ± 0.33 Amol m-2 s-1 in grassland and 7.33 ± 0.8 Amol m-2 s-1 in control was observed during rainy season-II, i.e., from October to December, a minimum of 1.27 ± 0.2 Amol m-2 s-1 in grassland and 0.67 ± 0.5 Amol m-2 s-1 in control during summer season, i.e., from March to June. A positive significant relation observed between soil respiration and soil moisture (r2 above 0.8) and no significant relation was observed between soil CO2 efflux and soil temperature (r2 below 0.3). In water-limited semi-arid ecosystem, rewetting of the soil due to precipitation events triggered the increased pulses of soil respiration especially in grassland when compared to the barren land. The observed soil respiration rates during summer and after the subsequent precipitation events strongly indicated that the soil water-deficit conditions reduce the efflux both in barren land (control) and in grassland of semi-arid eco-system.

Changes in some soil properties at different incubation periods after tobacco waste application.

In this study, changes in organic carbon (OC), basal soil respiration (BSR), nitrate nitrogen (NO3-N), electrical conductivity (EC) and aggregate stability (AS) of a clay loam soil due to tobacco waste (TOW) application were monitored for 240 days. After incorporating 5% TOW into soil according to oven dry weight basis, soil samples were incubated at field capacity for 20, 40, 80, 140 and 240 days under a greenhouse condition. TOW application significantly increased all soil properties over the control treatment. Soil OC and AS values had significant positive correlations each other and with the other soil properties. Soil OC, BSR and AS values significantly increased from 0.12%, 0.03 μg CO2-C g-1 dry soil 24 hr and 20.7% in control treatment to 1.13%, 3.7 μg CO2-C g-1 dry soil 24 hr and 54.4% in TOW treatment, respectively, in 20 days. While the highest NO3-N (1780 ppm) was found in 40 days, the highest EC (3.35 dS m-1) was in 240 days after TOW application. Disaggregation occurred in all treatments after 20 days of incubation due to probably the more substrate demands of microorganisms in soil.

Soil properties and root biomass responses to prescribed burning in young corsican pine (Pinus nigra Arn.) stands.

Fire is an important tool in the management of forest ecosystems. Although both prescribed and wildland fires are common in Turkey, few studies have addressed the influence of such disturbances on soil properties and root biomass dynamics. In this study, soil properties and root biomass responses to prescribed fire were investigated in 25-year-old corsican pine (Pinus nigra Arn.) stands in Kastamonu, Turkey. The stands were established by planting and were subjected to prescribed burning in July, 2003. Soil respiration rates were determined every two months using soda-lime method over a two- year period. Fine (0-2 mm diameter) and small root (2-5 mm diameter) biomass were sampled approximately bimonthly using sequential coring method. Mean daily soil respiration ranged from 0.65 to 2.19 g C m-2 d-1 among all sites. Soil respiration rates were significantly higher in burned sites than in controls. Soil respiration rates were correlated significantly with soil moisture and soil temperature. Fine root biomass was significantly lower in burned sites than in control sites. Mean fine root biomass values were 4940 kg ha-1 for burned and 5450 kg ha-1 for control sites. Soil pH was significantly higher in burned sites than in control sites in 15-35 cm soil depth. Soil organic matter content did not differ significantly between control and burned sites. Our results indicate that, depending on site conditions, fire could be used successfully as a tool in the management of forest stands in the study area.

Soil respiration and root biomass responses to burning in calabrian pine (Pinus brutia) stands in Edirne, Turkey.

In this study, soil properties and root biomass responses to prescribed fire were investigated in 25-30 year-old calabrian pine (Pinus brutia Ten.) stands in Edirne, Turkey. The stands were established by planting and were subjected to prescribed burning in July, 2005. Soil respiration rates were determined every two months using the soda-lime method over a two-year period. Fine (>2 mm diameter) and small root (>2-5 mm diameter) biomass were sampled approximately bimonthly using the sequential coring method. Soil respiration rates in burned sites were significantly higher than in control sites during the summer season but there was no significant difference in the other seasons. Soil respiration rates were correlated significantly with soil moisture and soil temperature. Fine and small root biomass were significantly lower in burned sites than in control sites. Mean fine root biomass values were 3204 kg ha-1 for burned and 3772 kg ha-1 for control sites. Annual soil CO2 releases totaled 515 g C m-2 for burned and 418 g C m-2 for control sites. Our results indicate that, depending on site conditions, fire could be used successfully as a tool in the management of calabrian pine stands in the study area.

In vitro study on the influence of methyl parathion on soil bacterial activity.

A study was conducted to find out the effect of different concentrations of Methyl parathion, an organophosphorus pesticide on soil bacterial population, soil respiratory activity and dehydrogenase activity, under laboratory conditions for a definite time period. The higher concentration (100 ppm) of Methyl parathion application, considerably reduced bacterial count, CO2 evolution and enzyme activity in soil but the microbial activities seemed to recover several weeks following pesticide application.

Efluxo de CO2 do solo em floresta de transição Amazônia Cerrado e em área de pastagem

The objective of this paper was (a) to estimate the CO2 soil efflux in a Mature Transitional Tropical Forest Amazonia and a area of Pasture in the north of the Mato Grosso; (b) to analyzer the influence of the soil humidity and temperature, and accumulated litter. The measurements had been carried through with device of CO2 absorption for infra-red ray (EGM/WMA-2 PP System, Hitchin Hertz, UK) in may/2005 to april/2006. The average values of the CO2 efflux of the ground in the Forest and the area of 5,45 and 4,94 µmolm-2s-1 Pasture µmolm-2s-1, respectively. In the dry season the behavior of the CO2 efflux of the ground was similar in the Mature Transitional Tropical Forest Amazonian and in the area of Pasture, and in the wet season the ecosystems had presented distinct behaviors, and the CO2 efflux of the ground in the area of Pasture was superior to the one in the Transitional Forest. It is essential that if it evaluates the influence of other factors in the CO2 efflux in ecosystems located in one same ecótono for the attainment of new answers that contribution to clarify doubt atmospheric CO2 emission to them the worldwide level.

O objetivo deste trabalho foi (a) estimar o efluxo de CO2 do solo em uma Floresta de Transição Amazônica Cerrado e em uma área de Pastagem localizadas no norte do Mato Grosso, e (b) verificar a influência da umidade e temperatura do solo, e serrapilheira acumulada no efluxo de CO2. As medições foram realizadas com aparelho de absorção de CO2 por infravermelho (EGM/WMA-2 PP System, Hitchin Hertz, UK) de maio/2005 a abril/2006. Os valores médios do efluxo de CO2 do solo na Floresta e na área de Pastagem foram de 5,45 e 4,95 µmolm-2s-1, respectivamente. Uma resposta satisfatória do efluxo de CO2 do solo e a serrapilheira acumulada, ocorreu somente na estação seca. Na estação seca o comportamento do efluxo de CO2 do solo foi semelhante na Floresta de Transição Amazônica Cerrado e na área de Pastagem, e na estação úmida os ecossistemas apresentaram comportamentos distintos, e o efluxo de CO2 do solo na área de Pastagem foi superior ao na Floresta de Transição. É essencial que se avalie a influência de outros fatores no efluxo de CO2 em ecossistemas localizados em um mesmo ecótono para a obtenção de novas respostas que contribuíam para esclarecer as dúvidas da emissão de CO2 em nível mundial.