ABSTRACT
Aims: The present study investigated the effect of lowland rice soils of two regions viz. new alluvial and red-laterite on aggregate characterization and their associated organic carbon (SOC). Study Design: Randomized block design (RBD). Place and Duration of Study: New alluvial soils were collected from Jangipara block of Hooghly, West Bengal and Red-laterite soils were collected from Raghunathpur block of Purulia, West Bengal during 2017-18. Methodology: For each soil types (New alluvial and Red-laterite) five locations were identified and soil samples were collected from three depths i.e. 0-10, 10-20 and 20-30 cm. The aggregate characteristics i.e. water-stable aggregates (WSAs), mean weight diameter (MWD), aggregate stability and aggregate size fractions along with the distribution of carbon in those aggregate size fractions were critically studied. Results: The aggregate size as well as the stability decreased with increasing soil depth from 0 to 30 cm in both soils. New alluvial soils showed higher aggregate stability than red-laterite soils. Mean weight diameter (MWD) values of new alluvial soils were 34, 29 and 87% more than red-laterite soils at 0-10, 10-20 and 20-30 cm depth, respectively. Presence of higher amount of clay and organic matter in new alluvial made the difference in structural coefficient. The surface soil (0-10 cm) had more coarse aggregate (Cmac A >2000μ) fraction, however, microaggregates (<250μ) were dominant in lower depths in both soils. Water stable aggregates (WSA) in surface soils of new alluvial and red-laterite were 57 and 36%, respectively and were decreased with depth. Red-laterite produced higher micro aggregates as compared to new alluvial soils. Coarse macro aggregate fractions (>2000μ) retained maximum amount of soil organic carbon in both soils however, coarse micro aggregate associated carbon (Cmic AC<250μ) was captured in lower depths. New alluvial soils yielded aggregates with higher in diameter and stability coefficient that is due to higher amount of carbon stored in aggregates. Conclusion: The abundance of macro aggregate of New alluvial soils indicates better soil physical quality than Red-laterite soil which was dominated in higher micro aggregates leads to poor in structure and susceptible to water erosion.
ABSTRACT
El interés en estudios de biorremediación de suelos deteriorados por sobreexplotación y uso indiscriminado de agroquímicos se debe a que alteran la microflora, el sistema de autorregulación y la sustentabilidad en el largo plazo. Un Ultisol, suelo de baja fertilidad química y sometido a reducción de tamaño de agregados (<2,0 mm), solarizado para reducir la población microbiológica, fue inoculado con la bacteria Basillus subtilis en concentraciones de 106, 107, 108, 109 unidades formadoras de colonias (ufc). En 120 días se observó un incremento importante en magnitud de: estabilidad estructural, tamaño promedio de agregados, pH, fósforo disponible y una disminución del aluminio intercambiable. Estas variaciones en la respuesta estuvieron relacionadas con la actividad de los microorganismos en el suelo, y responden a la capacidad de solubilización de minerales por la bacteria, de producción de condiciones alcalinas y de biofilms, que unidos al aumento de biomasa de raíces de la planta, mucílagos y carbohidratos, coadyuvan en la formación de agregados estables y de mayor tamaño. Las propiedades físicas y químicas al final del experimento se estabilizaron en valores mayores a los encontrados en el suelo inicial, produciendo un efecto positivo general sobre el mismo, desde el punto de vista de la fertilidad global, al aumentar el fósforo disponible, disminuir la acidez intercambiable e incrementar la estabilidad y el tamaño promedio de agregados del suelo a corto plazo.
The interest about the studies of bioremediation in deteriorated soils under and over exploitation, indiscriminate use of agrochemicals that alter the microflora, the self regulation system and the sustainability in the long term. An Ultisol, with poor chemical properties and low fertility, because the reduction of aggregates size (< 2.0 mm). Solarize to reduce the microbiological population, it was inoculated with the bacteria Basillus subtilis in concentrations of 106, 107, 108, 109 colony forming units (cfu). In 120 days important increment in magnitude of: structural stability, size average of aggregates, pH, available phosphorus. Also diminish the interchangeable aluminum. These variations in the answer were related with the activity of the microorganisms in the soil, and it responds so that solubilisation capacity of minerals because the bacteria activity, production of alkaline conditions and biofilms too. Furthermore the increase of plant roots biomass, mucilages and carbohydrates cooperate in the formation of stable aggregates and bigger size of them. The physical and chemical properties at the end of the experiment were stabilized in bigger values than found in the initial soil. Confirming a positive general effect overall the soil, since the point of view of the global fertility, when increasing the available phosphorus, reduce the interchangeable acidity and increase the soil stability and average size aggregates in the short term.