Vertical Distribution of TOC, TN and Other Important Soil Attributes and Their Relationship in Alfisol and Entisol of West Bengal

A study to assess the profile distribution of important soil attributes in Alfisols and Entisols of West Bengal was conducted during 2016-17. Purposefully selected random sampling was carried out to collect the soils from different locations of two study sites, viz., Kalinagar (25º27'33.9"N, 88º19'10.2"E) from Malda district and Durganagar (26º09'62.7"N, 89º53'51.7"E) from Cooch Behar district of West Bengal at 0-15, 15-30, 30-45 and 45-60 cm depths. Understanding of vertical distribution of soil fertility indicators like soil organic carbon (SOC), total nitrogen (TN) and other important properties in two different soil and climatic conditions will provide an insight regarding the behaviour of soil with the change in environmental conditions. Soil bulk density (BD), porosity, pH, SOC, TN, C:N ratio and texture were determined using standard laboratory procedures and computations. Obtained results were subjected to statistical analyses. Soils of Kalinagar sites were slightly acidic in nature while soils of Durganagar were neutral in nature. Kalinagar soils were silt clay loam in texture where Durganagar soils classified as loam to sandy loam. Soil BD values increased with depth in both Kalinagar (Alfisol) and Durganagar (Entisol). The porosity percentage progressively decreased with an increase in depth. Soils of Durganagar reported higher soil porosity at all the depths studied. An increase in soil pH with increasing depth was observed in both the sites. The mean total organic carbon (TOC) content recorded maximum in surface soil and its concentration decreased with the depth. Kalinagar soils observed 7.63% higher TOC (17.94 g kg-1) content than Durganagar (16.57 g kg-1) at surface depth (0-15 cm) and its accumulation at the lower depths was also maximum in former soil. Mean TN values were also found to decrease by increasing the depth. The accumulation of total nitrogen at the subsequent depths was relatively higher in Kalinagar than Durganagar. Increase in C:N ratio with increasing depth was noticed in Kalinagar site but the opposite trend was accorded in case of Durganagar. Accumulation of SOC and TN throughout the soil depth was found to be greater in Alfisol (Kalingar) due to higher clay and silt fractions as compared to Entisol (Durganagar). There was a significant positive relation of TOC with clay and silt (r = 0.285, p<0.05, r = 0.314, p<0.01, respectively) and of TN with clay and silt (r = 0.328, p<0.01, r = 0.262, p<0.05, respectively) irrespective of soil orders. Alfisols with high bulk density have a greater capacity to accumulate SOC and TN throughout the soil profile due to higher clay and silt fractions in comparison to Entisols with loose textural properties.

Effects of carbon, nitrogen and pH on the growth of Aspergillus parasiticus and aflatoxins production in water.

Mycotoxins are considered as the most hazardous fungal metabolites for human, animals and plant health. Recently, more attention has been paid on the occurrence of this group of fungi in different water sources throughout the globe. In this study, Aspergillus parasiticus ATCC strain was used as representative strain producing aflatoxins in drinking water. This study aimed to investigate the activation of fungi in drinking water and their ability to produce aflatoxins (B1, B2, G1, and G2) in water under different ratios of C:N using different concentrations of total organic carbon (TOC) and total nitrogen (TN). Glucose and ammonium sulphate were used for changing the levels of TOC and TN in the selected water media. Similarly, the effects of different water pH levels from 4.5 to 8.2 on the growth of this group of fungi and aflatoxins production were also investigated. The results indicate that the growth of fungi was highest, at C:N ratio of 1:1 as compared to other selected ratios. Furthermore, the findings indicate that the pH levels 5.5-6.5 showed best growth of fungi as compared to other pH levels. Aflatoxin concentrations were measured in the water samples using HPLC technique, but selected fungi were not able to produce aflatoxins in water at applied concentrations of TOC and TN mimicking the ratios and concentrations present in the natural aquatic environment.

Distribution of enteric bacteria in the sediments of Parangipettai and Cuddalore coast of India.

Distribution of major groups of enteric bacteria viz., Escherichia coli, Shigella spp., Salmonella spp., Vibrio parahaemolyticus and Vibrio cholerae was studied in the sediment samples collected from different depths of 5, 15, 25 and 35 m in Parangipettai and Cuddalore coast during March, 2009 to February, 2010. Among the bacterial population in Parangipettai, V. parahaemolyticus was found to be maximum with an occurrence of 55% followed by Shigella spp. (15%), V. cholerae (12%), Salmonella spp. (12%) and E. coli (6%). In Cuddalore, as an oddity, Vibrio cholerae emerged as dominant species with an incidence of 60% of the total. V. parahaemolyticus came next in the order with an incidence of 14%, followed by E.coli (11%), Shigella spp. (8%) and Salmonella spp. (7%). Similarly, monsoon and premonsoon seasons registered higher bacterial populations in both the regions. When the depth wise results were viewed, 5 and 15 m depths showed maximum (V. parahaemolyticus 3.7x 10 CFU g-1 in Parangipettai; V. cholera - 8.6x10 CFU g-1 in Cuddalore) bacterial population compared to subsequent depths. Cluster and MDS also showed distinct spatial and seasonal variations of bacterial populations in both the regions. Biota-Environment (BIO - ENV) method revealed the combinations of temperature, salinity and TOC as the best match influencing bacterial population.

Agregação e proteção física da matéria orgânica em planossolo háplico sob diferentes sistemas de manejo / Aggregation and physical protection of organic matter in albaqualf under different manegement systems

Identificar os mecanismos de estabilização da matéria orgânica (MO) que atuam com maior eficiência em solos hidromórficos é essencial para compreender e avaliar a dinâmica da MO nestes agroecossistemas. O objetivo deste estudo foi avaliar a agregação, o teor de carbono orgânico total (COT) do solo e de carbono nas frações físicas da MO, em Planossolo Háplico Eutrófico solódico, sob diferentes sistemas de manejo; além de caracterizá-la por Infravermelho com Transformada de Fourier (FTIR). O presente estudo foi realizado na Estação Experimental de Terras Baixas da Embrapa Clima Temperado, Capão do Leão, RS. A área experimental foi implantada em 2003. Em novembro de 2007, foram amostradas duas camadas (0,000 - 0,025 m e de 0,025 - 0,075 m) de solo em áreas sob preparo convencional (PC), plantio direto (PD) e campo nativo (CN). A qualidade estrutural na camada superficial do solo sob PC e PD foi afetada nas classes de agregados de 4,76 a 0,50 mm. O PC e o PD apresentaram reduções nos teores de COT do solo, carbono da fração grosseira, fração leve livre (FLL) e fração leve oclusa (FLO). Em curto período de tempo (quatro anos), os sistemas de manejo não influenciaram a fração pesada (FP). As proporções das frações físicas da MO em relação ao COT aumentaram na ordem FLL

To identify the mechanisms of stabilization of organic matter (OM) that act more efficiently in hydromorphic soils is essential to understand and to assess OM dynamics in these ecosystems. The aim of this study was to evaluate the aggregation, the total organic carbon (TOC) in the soil and in the physical fractions of OM, to characterize them by Fourier Transform Infrared (FTIR), and to identify the mechanisms of protection in an Albaqualf soil under different management systems. This study was conducted at the Lowlands Experimental Station of Embrapa Temperate Climate, in Capão of Leão municipality, Rio Grande do Sul State. The experimental area was established in 2003. In November 2007, soil was sampled in two layers (0.000 - 0.025 m and 0.025 - 0.075 m depth) under conventional tillage (CT), no tillage (NT) and native pasture (CN) areas. The structural soil quality under CT and NT, in the surface layer, was affected in the aggregate of diameter classes from 4.76 to 0.50 mm. The CT and the NT showed reductions in levels of soil TOC, C from the coarse fraction, free light fraction (FLF) and occluded light fraction (OLF). In a short period of time (four years), the management systems did not affect the heavy fraction (HF). The proportions of physical fractions of OM in relation to the COT increased in the order FLL

Recuperação de carbono obtida por três métodos em frações da matéria orgânica de latossolo, sob consórcio milho-forrageiras, no cerrado / Carbon recovery obtained by three methods in organic matter fractions of latosol under maize-grass intercropping in the cerrado

A dinâmica da matéria orgânica do solo (MOS) pode ser melhor compreendida após identificadas suas frações lábeis (> 53 µm) e estáveis (< 53 µm). Diante da importância crescente do uso de técnicas de fracionamento físico da MOS, torna-se necessário avaliar se a recuperação de carbono nessas frações é influenciada pelos métodos utilizados para sua determinação. O objetivo deste trabalho foi avaliar os teores de carbono, por três métodos, em diferentes frações da matéria orgânica, num Latossolo Vermelho-Amarelo distrófico sob consórcio milho-forrageiras e em sistema solteiro. Foram determinados os teores de carbono das frações: (i) particulada da matéria orgânica (COP) e naquela (ii) associada aos minerais da matéria orgânica (COM). Determinou-se ainda, o teor de (iii) carbono orgânico total do solo (COT) na matéria orgânica não fracionada. Três métodos de determinação do carbono orgânico do solo foram utilizados: (i) Walkley & Black modificado, (ii) Mebius modificado, e (iii) combustão via seca, em analisador elementar (CHN). Foram utilizadas amostras de solos de três sistemas de manejo dispostos em delineamento em blocos casualizados, com três repetições para determinação do carbono orgânico do solo: (i) milho solteiro; (ii) milho consorciado com capim colonião (Panicum maximum cv. Aruana); e (iii) milho consorciado com braquiária (Brachiaria humidicola). As amostras de solo foram coletadas na profundidade de 0 ­ 5 cm. O método Walkley & Black apresentou menores valores de COT em relação ao CHN nos sistemas de manejo milho/braquiária e milho solteiro, e mostrou valores de COP semelhantes àqueles obtidos pelo CHN nos sistemas de manejo milho solteiro e milho/braquiária. Valores de COT, COP e COM obtidos pela metodologia de Mebius modificado foram semelhantes àqueles obtidos pelo analisador elementar, para todos os sitemas de manejo. O COP, quando avaliado pelas metodologias de Mebius e CHN, mostrou-se significativamente mais sensível às alterações de manejo em relação ao COT e COM.

Soil organic matter alterations can be better understood when it is fractionated for the identification of its labile (> 53 µm) and stable (< 53 µm) fractions. Because of the increasing and important use of soil organic matter fractionation techniques, it becomes necessary to evaluate if the carbon recovery in these fractions is influenced by methods used for its determination. The aim of this work was to evaluate the content of organic carbon in soil organic matter fractions, by three different methods, under maize-grass intercropping and sole maize in a dystrophic Red-Yellow Latosol (Oxisol). The following carbon contents were determined from the fractions: (i) of the particulate soil organic matter (POM) and from that (ii) of mineral-associated soil organic matter (MOC). The content of total organic carbon (TOC) was also determined in the non-fractionated soil organic matter. Three methods for the determination of soil organic carbon were used: (i) Walkley & Black modified, (ii) Mebius modified, and (iii) dry combustion in a CHN elemental analyzer. The experimental design was a randomized block design with three replications. Soil samples were collected from three management systems: (i) sole corn; (ii) maize-Panicum maximum intercropping; and (iii) maize- Brachiaria humidicola intercropping. Soil samples were collected from the depth of 0 ­ 5 cm. Lower TOC were found in the Walkley & Black method in relation to the CHN elemental analyzer, under the management systems sole maize and maize-Panicum maximum intercropping. However, the Walkley & Black method showed similar POM in relation to CHN analyzer method, under the management systems sole maize and maize-Brachiaria humidicola intercropping. TOC, POM and MOC obtained from the Mebius modified method were similar to those obtained from the elemental analyzer, under the three management systems. The POM when evaluated by the Mebius and CHN methods, showed to be more sensible to soil management alterations.

Montaje y validación del método de análisis poscombustión y detección por infrarrojo no dispersivo para determinación de carbono orgánico total (cot) en agua / Assembly and validation by the method of combustion analysis and ondispersive innfrared detection for determining total organic carbon (toc) in water

La técnica de análisis por combustión y detección por infrarrojo no dispersivo (IRND) fue validada para la determinación de materia orgánica en agua, cuantificada como carbono orgánico total (COT). Previamente se optimizó la eliminación del carbono inorgánico (CI) de la muestra con un tiempo óptimo de 1,5 min y una relación ácido de 5%. Se estableció un rango dinámico lineal (RDL) entre 3 y 20 mg/L de COT, en el cual la recta de regresión cumplió con los parámetros que acreditaron su linealidad según el análisis por el método de los mínimos cuadrados, mostrando un coeficiente de correlación de 0,9994. La sensibilidad expresada por la pendiente de la recta de regresión indicó una variación de aproximadamente 5 unidades en la respuesta del detector por cada mg/L de COT. Los límites de detección y cuantificación obtenidos a partir de la recta de regresión fueron 0,517 y 1,722 mg/L de COT, respectivamente. La precisión de la técnica, teniendo como meta un 5% en coeficiente de variación (CV), fue mejor en el agua potable y en concentraciones cercanas a ésta (aprox. 7 mg/L de COT), mientras que las mayores desviaciones se presentaron en concentraciones cercanas a los límites inferior y superior del RDL. Las recuperaciones de concentraciones conocidas sobre muestras reales adicionadas fueron del 85% con baja adición y del 83% con adición alta, valores que sugieren una reevaluación del desempeño de la técnica con respecto a su exactitud, no obstante se alcanzó la meta de recuperación comprendida entre el 70 y el 130%. La técnica así establecida es por tanto apta para el análisis de aguas crudas, potables y residuales y es viable su utilización en el seguimiento a procesos de oxidación avanzada aplicados en el tratamiento de agua para consumo humano.

The technique of combustion analysis and detection by non-dispersive infrared (NDIR) was validated for the determination of organic matter in water, quantified as total organic carbon (TOC). Previously optimized the elimination of inorganic carbon (IC) of the sample with an optimum time sparge of 1.5 min and an acid ratio of 5%. It established a linear dynamic range (LDR) between 3 and 20 mg/L of TOC, in which the regression line that met the parameters credited its linearity as analyzed by the method of least squares, showing a correlation coefficient of 0,9994. The sensitivity expressed by the slope of the regression line indicated a variation of about 5 units in the detector response for each mg/L of TOC. The detection and quantification limits obtained from the regression line were 0.517 and 1.722 mg/L of TOC, respectively. The precision of the technique, aiming at 5% coefficient of variation (CV) was better in the drinking water at concentrations close to it (about 7 mg/L of TOC), whereas larger deviations were presented at concentrations near the lower and upper limits of LDR. The recoveries of known concentrations of actual samples of 85% additions were low addition and 83% with high added values that suggest a reevaluation of the performance of the technique with respect to its accuracy, however the goal was reached between recovery 70 to 130%. The technique is well established thereby capable of analyzing raw water, drinking and waste and feasible to use in monitoring advanced oxidation processes applied in the treatment of drinking water.