Practices of participation in coastal area management: Experience from Kenya     

Hom Nath Gartaula   《Ocean & Coastal Management》2008,51(7):528-535

This paper explores a development intervention, discourses involved and people's encounter at the interfaces during interaction and negotiation processes in everyday project life. It aims to get insight in the participatory intervention; how participatory is it and what is the intention behind the concept? This ethnography of an ongoing program in Kenya concludes that creation of participatory projects is a strategy of development practitioners to have high-rated evaluation of the project for donor funding but, in practice, the concept of participation is used by actors according to their interest and need.  相似文献   

Similarity solution for the propagation of shock waves with varying energy in non-uniform medium     

Onkar Nath  A. D. P. Sinha 《Astrophysics and Space Science》1989,153(1):31-37

A model of self-similar propagation of shock waves driven by a flare energy release in a non-uniform atmosphere has been considered. The total energy content of the model is assumed to be increased with time within the inner expanding surface and shock front. Finally the variation of velocity, pressure, density, and energy of the model have been discussed. The gas is assumed to be grey and opaque.  相似文献   

The equilibrium state of shock-heated rotating atmosphere under the force of gravitation     

Onkar Nath 《Astrophysics and Space Science》1989,158(2):183-187

Equations are developed to describe the flow of a rotating atmosphere under force of gravitation heated by an arbitrary distribution of cylindrical shock waves. Solutions are obtained for the outer solar atmosphere with a steady mass motion in which the heat supplied by shock wave is balanced by the convective heat loss due to this motion. It is found that, for very large range of shock strength and frequencies, the temperature profile is similar to that predicted by the constant shock-strength hypothesis. This hypothesis is used as the basis of a model of the outer solar atmosphere starting near the solar atmosphere.  相似文献   

Exact solution of the problem of diffuse reflection and transmission by the method of Laplace transform and linear singular operators     

Rabindra Nath Das 《Astrophysics and Space Science》1978,58(2):419-425

The basic integro-differential equation is subjected to a one-sided finite Laplace transform to obtain linear integral equations of angular distribution of bounding faces. These linear integral equations have been transformed into linear singular integral equations which have been solved exactly to get the emergent distributions from the bounding faces by the theory of linear singular operators. Some solutions of linear singular integral equations have also been derived for future use in radiative transfer problems.  相似文献   

Heat and mass transfer in convective flow of an incompressible rarefied visco-elastic fluid in presence of transverse magnetic field     

H. L. Agrawal  R. Nath  P. C. Ram 《Astrophysics and Space Science》1983,95(2):439-451

Analytical study is performed to examine heat and mass transfer characteristics of natural convection flow of an incompressible, rarefied visco-elastic fluid past an infinite vertical porous plate with constant suction in the presence of transverse magnetic field under combined buoyancy force effects of thermal and mass diffusion. The effects of various parameters on mean velocity and mean skin-friction are shown graphically followed by a comparative study of Newtonian and non-Newtonian (visco-elastic). rarefied states.  相似文献   

Exact solution of a problem in radiative transfer by the laplace transform and the Wiener-Hopf technique when the incoming intensity at the surface is known     

Rabindra Nath Das 《Astrophysics and Space Science》1979,62(1):149-157

We consider the problem of determining the emergent intensity from the bounding face of a semi-infinite atmosphere having conservative scattering and the intensity at any optical depth by use of the Laplace transform in combination with the Wiener-Hopf technique when the incoming intensity at the bounding face of the atmosphere is known. The solution is exact.  相似文献   

Exact solution of a key equation in a finite stellar atmosphere by the method of Laplace transform and linear singular operators     

Rabindra Nath Das 《Astrophysics and Space Science》1980,67(2):335-342

The key equation which commonly appears for radiative transfer in a finite stellar atmosphere having ground reflection according to Lambert's law is considered in this paper. The exact solution of this equation is obtained for surface quantities in terms of theX-Y equations of Chandrasekhar by the method of Laplace transform and linear singular operators. This exact method is widely applicable for obtaining the solution for surface quantities in a finite atmosphere.  相似文献   

Trend in chemical composition of precipitation during 2005–2009 at a rural station of Bhubaneswar, eastern India     

Namrata Das  Saroj Sundar Baral  Parth Sarathi Mahapatra  Trupti Das  Gautam Roy Chaudhury  Surendra Nath Das 《Theoretical and Applied Climatology》2012,110(1-2):55-63

Precipitation samples collected during 2005–2009 from a rural forest station of Bhubaneswar were analyzed for their chemical composition. The samples were collected through a wet-only (WO) collector and two bulk (B1 and B2) collectors. The ions were evenly balanced indicating good data quality. The overall pH of rainwater was slightly acidic and ~47% of all rain events during the period were acidic (pH?<?5.6). Multilinear regression analysis showed relation between the free acidity (H⁺) and other components in rainwater. Enrichment factors (EF) of the major components with respect to their sources such as marine and crustal were calculated. Maximum EF was observed for NO ₃ ^? for both marine and crustal sources for all the three collectors. Source apportionments were also carried for the ions. Trend analysis showed continuous increase in most of the ions over years during the study period driven by anthropogenic emissions. Statistical/factorial analysis established correlation among different ions.  相似文献   

Heavy minerals of the Barakar Formation,Talchir Gondwana Basin,Orissa     

Rabindra Nath Hota  Wataru Maejima 《Journal of the Geological Society of India》2009,74(3):375-384

Heavy mineral analysis has been carried out in the Barakar Formation of the Talchir Gondwana Bbasin, Orissa. The characteristic heavy minerals are garnet, zircon, tourmaline, rutile, biotite, chlorite, pyroxenes, hornblende, staurolite, sillimanite, apatite, epidote, sphene, spinel and siderite including opaques and leucoxene. These heavy minerals are divisible into four groups on the basis of principal component analysis and suggest derivation of Barakar sediments from pegmatite, acid and basic igneous as well as low- and high-rank metamorphic rocks lying to the south of the Talchir Gondwana Basin. Though the heavy mineral suites of all the sandstone samples are by and large similar, differences have been noticed in the frequencies of many heavy minerals in vertical succession. Cyclic nature and vertical fluctuation of heavy mineral frequencies can be ascribed to variation of the relief of the source area, sudden release of some of the minerals in the source region and/or existence of favourable geochemical condition to escape partial dissolution.  相似文献   

A study of lightning activity over land and oceanic regions of India     

Asha Nath  G. K. Manohar  K. K. Dani  P. C. S. Devara 《Journal of Earth System Science》2009,118(5):467-481

Monthly variations of lightning activity over typical land and oceanic regions of India were examined using satellite data (OTD) for a 5-year period (1995–1999). It is noted that the nature of variation between surface air maximum temperature (T _max), thunderstorm days (Th_n), and lightning flash count over ER and WR showed remarkable correspondence and sensitivity with each other on monthly time scale. As we move out of winter season and enter the monsoon season, via pre-monsoon season, the WR undergoes cooling relative to the ER in the range 0.1–1.2°C. As a result, WR experiences reduction of thunder days and lowering in flash count. This decrease in T _max, Th_n, and flash count over WR may also be associated with relatively small values of T _θw and CAPE in comparison with similar values over ER during the monsoon season. Our observation of associated reduction in Th_n and lightning count per 1°C cooling in surface air maximum temperature suggests reduction of ∼3.5 thunderstorms per station and 73 flashes. Comparison of lightning flashes between pairs of coastal, oceanic, arid-zone, hilly, and island stations reveals distinct relationship between climate regime and intensity of lightning activity. We may conclude the results of this study by saying that the overhead lightning activity is a clear reflection of the status of the underlying ground-earth properties. A close and continuous monitoring of lightning activity may be considered as a need of present day scientific studies.  相似文献