Background:Village Health and Nutrition Day (VHND) was identified to provide primary care services (health, nutrition and sanitation) at village level under National Rural Health Mission.Aim:The study aimed to assess availability of health, nutrition and sanitation services, required instruments/equipment and medicines at VHND with client satisfaction from the VHND services.Materials and Methods:A cross-sectional study was conducted in three districts of Uttarakhand at Nainital, Tehri-Garhwal and Chamoli involving 24 villages in six blocks using multistage stratified sampling using predesigned pretested observation checklists (quantitative data). All the concerned functionaries of health, Integrated Child Development Services and Panchayati Raj Institution were interviewed (qualitative data) to understand the gap in services and remediation.Results:Of the 24 VHNDs observed, blood pressure measurement was done at 11 (45.83%) and weight at 13 (54.17%) sites in ante-natal care services; non-availability of blood pressure instrument and adult weighing machine were 45.83% and 41.66% sites, respectively. Immunization for children was provided at 22 sites; however, availability of other services were poor-vitamin A (three), growth monitoring of children (seven); supplementary nutrition (five); identification of households for construction of toilet (eight). Yet, one-third of clients provided three and four for satisfaction from VHND services on the scale score of 1–5.Conclusion:It was noted that none of the VHND site was providing all the stipulated services, though immunization was provided mostly. Anganwadi centers were lacking availability of various essential instruments and equipment. So regular orientation of village functionaries for ensuring all the VHND services with the availability of required logistic is recommended.

An elevated translocator protein (18 kDa, TSPO) density is observed during inflammation in the brain and peripheral organs making it a viable target for imaging.

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Permeability is a measure of the ability of a reservoir rock to transmit fluids, and is arguably the most important parameter within a simulation model. For the Mangala field, permeability has been measured extensively from core analyses, wireline logging and well test analyses. Implicit in each of these measurement techniques is a specific scale and measurement direction. It is thus not surprising that differences still remain even after correcting the measured permeabilities from various sources to an absolute permeability. This paper presents the detailed methodology that was used for the calculation of permeability from the various sources and discusses possible explanations for the differences in the numbers. In some of the lower reservoir units, Mangala core permeabilities are significantly higher than the permeabilities measured from well tests, and it is proposed that permeability "baffles" on a multi-meter scale may be causing this decrease in well test permeabilities. These "baffles" are related to depositional features (e.g. current bedding and channel pinch-outs) and are likely to be strongly directional, leading to a horizontal permeability anisotropy which has important implications for reservoir development. Introduction The Mangala field was discovered in January 2004 (Yashwant, et al, 2006) by targeting a simple, tilted fault-block trap formed within the rifted, Tertiary Barmer Basin (Figure-1 and Figure-2).