Hairy root cultures of Catharanthus roseus var. Prabal were established by infecting the leaves with Agrobacterium rhizogenes agropine-type A4 strain. Two hundred and fifty independent root clones were evaluated for growth, morphology, number of integration of Ri T-DNA genes and alkaloid contents. On the basis of growth pattern, type of branching and number of lateral roots we were able to separate the hairy root clones into four categories. However based on the integration of the Ri T(L)-DNA and T(R)-DNA genes, there were only three different categories of independent hairy root clones-C1 (rolA&B(+)/ags(+)), C2 (rolA&B(-)/ags(+)) and C3 (rolA&B(+)/ags(-)). Southern hybridization analysis revealed both single and multiple copies of T-DNA integration in the root clones. The accumulation of considerable amounts of the root-specific alkaloids ajmalicine and serpentine was observed in the presence of both the T(L)-DNA and T(R)-DNA genes (C1) and the T(L)-DNA gene (C3) alone. Two rolA&B(-) but ags(+) clones (C2) accumulated much less or only very negligible amounts of ajmalicine. The possible role of the T(L)-DNA and T(R)-DNA genes on growth and alkaloid accumulation in these root clones is discussed.

Size distribution, water-soluble inorganic ions (WSII), and organic carbon (OC) and elemental carbon (EC) in size-segregated aerosols were investigated during a year-long sampling in 2010 over New Delhi. Among different size fractions of PM, PM was the dominant fraction (45%) followed by PM (20%), PM (15%), PM (10%), and PM (10%). All size fractions exceeded the ambient air quality standards of India for PM. Annual average mass size distributions of ions were specific to size and ion(s); Ca, Mg, K, NO, and Cl followed bimodal distribution while SO and NH ions showed one mode in PM. The concentrations of secondary WSII (NO, SO, and NH) increased in winters due to closed and moist atmosphere whereas open atmospheric conditions in summers lead to dispersal of pollutants. NHand Cawere dominant neutralization ions but in different size fractions. The summer-time dust transport from upwind region by S SW winds resulted in significantly high concentrations of PM and PM and PM. This indicted influence of dust generation in Thar Desert and its transport is size selective in nature in downwind direction. The mixing of different sources (geogenic, coal combustions, biomass burning, plastic burning, incinerators, and vehicular emissions sources) for soluble ions in different size fractions was noticed in principle component analysis. Total carbon (TC = EC + OC) constituted 8-31% of the total PM mass, and OC dominated over EC. Among EC, char (EC1) dominated over soot (EC2 + EC3). High SOC contribution (82%) to OC and OC/EC ratio of 2.7 suggested possible role of mineral dust and high photochemical activity in SOC production. Mass concentrations of aerosols and WSII and their contributions to each size fraction of PM are governed by nature of sources, emission strength of source(s), and seasonality in meteorological parameters.

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