Thesis (Ph. D.)--University of Wyoming, 2005. / Title from PDF title page (viewed on Nov. 13, 2007). Includes bibliographical references (p. 132-140).

This study is a qualitative study on the participants on the Ganga Arti. It does focus on the participants on how they attend, how they express their religious belief and why the ritual is important for them. The study has been done in Varanasi, India, on a period of three months. Also the study has been done on the two ghats Tulsi and Assi. It tries to explain how the ritual can be understand both thru the participants eyes and thru theory. That has been done with both interviews and participant observations. Thru the study it has shown how complex the ritual and ghat is for participants and the society. The study have shown how fieldwork can be done and which considerations can be done. It has also shown that people in Varanasi participant the ganga arti in different ways, the religious beliefs can be different and also how they show it.

Spatial and temporal patterns of dissolved organic matter (DOM) were characterized using a combination of spectroluorometric measurements and multivariate analysis techniques. The study was conducted over a four-year (2012-2016) period in multiple watersheds located in the Gulf-Atlantic Coastal Plain Physiographic region of the southeast USA as well as in the Indo-Gangetic Plain of India. Surface water samples were collected from five major lakes in the Mississippi, an estuarine region in the southeastern Louisiana, and from the coastal region in the eastern Mississippi Sound in the USA, and a large river (Ganges River) in India. Absorption and fluorescence measurements were performed to generate absorption spectra and excitation-emission matrices (EEMs). Using parallel factor analyses (PARAFAC), EEM models were developed to characterize the biogeochemistry of DOM in three studies in this project. Principal component analysis and regression analyses of DOM data indicated that the northern Mississippi lakes were majorly influenced by agricultural land use, estuarine region was affected by natural DOM export from forests and wetlands, while the coastal waters were affected by a mix of anthropogenic and natural inputs of DOM. Spatial analyses indicated that DOM derived from watershed with increased wetland coverage was humic and aromatic while the DOM derived from agricultural watersheds was bioavailable. Temporal patterns of DOM in the estuary indicated the influence of hydrologic conditions and summer temperatures, and revealed strong seasonality in DOM evolution in the watershed. During high discharge periods (spring), aromatic and humic DOM was exported from the watershed while strong photochemical degradation during summer resulted bioavailable DOM. Comparison between two river systems, a highly urbanized large river and a small pristine river, indicated the influence of anthropogenic inputs of DOM in the large river system. DOM was bioavailable during summer due to anthropogenic activities in the large river system while it varied with hydrological connectivity in a small river system during summer and winter. In conclusion, this study has improved my understandings of the DOM properties, which are critical for a comprehensive assessment of biogeochemical processes undergoing in important water bodies on which our society is heavily dependent upon.

The study investigates and evaluates chemical parameters in handpumped water along Assi, a tributary to Ganga, south of Varanasi, northern India. Assi is polluted from raw sewage, landfill runoff and outlets from industries. To find out if the stream affects the groundwater in its basin, regression analysis of the easily moving ions, nitrite, nitrate and chloride were done during spring and autumn 2008. Significant trends were found for nitrate, most of them in the after monsoon period. No other chemical parameter gave significant trends. Metals as manganese and hexavalent chromium was measured in the spring period. Levels were higher closer to the stream. Significant trends when tested with regression analyses could not be found and the hexavalent chromium do not exceed guideline values in the handpumps measured. Interviews made clear that one quarter of the users of handpumped water have bad water quality during the monsoon period. The mean value of TDS in these pumps were higher than for the pumps that have good water quality and exceeds 500 mg/l. The mean value for turbidity was higher than 5 NTU in these pumps and in pumped water with good quality lower than 5 NTU. High levels of turbidity did not seem to affect the experience of having a good water. Pumps with higher TDS-values shows higher risk for polluted surface runoff together with risk for a broken construction that can allow seepage into the pumped water. Assi gives a severe contribution of raw sewage to Ganga upstream the bathing area in Varanasi and the pollution in the stream seams to affect the groundwater in its basin.

Chemical weathering of silicate rock consumes atmospheric CO2 and supplies the oceans with cations, thereby controlling both seawater chemistry and climate. The rate of CO2 consumption is closely linked to the rate of CO2 outgassing from the planetary interior, providing a negative feedback loop essential to maintaining an equable climate on Earth. Reconstruction of past global temperatures indicates that a pronounced episode of global cooling began ~50 million years ago, coincident with the collision of India and Asia, and the subsequent exhumation of the Himalayas and Tibet. This has drawn attention to the possible links between exhumation, erosion, changes in silicate weathering rates, and climate. However, many of the present-day weathering processes operating on the continents remain debated and poorly constrained, hampering our interpretations of marine geochemical archives and past climatic shifts. To constrain the controls on silicate weathering, this thesis investigates the lithium (Li) isotopic composition of river waters, suspended sediments and bed load sediments in the Alaknanda river basin, forming the headwaters of the Ganges. Due to the large fractionation of Li isotopes in the Earth’s surface environment, Li is sensitive to small changes in silicate weathering processes. As a consequence of the pronounced gradients in climate (rainfall and temperature) and erosion across the basin, the river waters show large variations in their Li isotopic composition (δ7Li), ranging from +7.4 to +35.4‰, covering much of the observed global variation. This allows a detailed investigation of the controls on Li isotope fractionation, and by extension silicate weathering. The Li isotopic composition is modelled using a one-dimensional reactive transport model. The model incorporates the continuous input of Li from rock dissolution, removal due to secondary mineral formation, and hydrology along subsurface flow paths. Modelling shows that the Li isotopic variations can be described by two dimensionless variables; (1) the Damköhler number, ND, which relates the silicate dissolution rate to the fluid transit time, and (2) the net partition coefficient of Li during weathering, kp, describing the partitioning of Li between secondary clay minerals and water, which is primarily controlled by the stoichiometry of the weathering reactions. The derived values of the controlling parameters ND and kp, are investigated over a range of climatic conditions and on a seasonal basis, shedding light onto variations in the silicate weathering cycle. In a kinetically limited weathering regime such as the Himalayan Mountains, both climate and erosion exert critical controls the weathering intensity (the fraction of eroded rock which is dissolved) and the weathering progression (which minerals that are being weathered), and consequently the fractionation of Li isotopes and silicate weathering in general. Modelling of the Li isotopic composition provides an independent estimate of the parameters which control silicate weathering. These estimates are then used to constrain variables such as subsurface fluid flux, silicate dissolution rates, fluid transit times and the fraction of rock which is weathered to form secondary clay minerals. The simple one-dimensional reactive transport model therefore provides a powerful tool to investigate the minimum controls on silicate weathering on the continents.

Cette thèse se propose de définir les temps caractéristiques des processus d’altération à l'échelle de profil d'altération (bassin versant de Rio Icacos à Porto Rico) et de transfert sédimentaire subséquent dans les plaines alluviales (bassins du Gange et du Brahmapoutre). Cette problématique est abordée par l’analyse des nucléides des séries de désintégration radioactives de l’uranium-238. L’étude du système d’altération sphéroïdale développée sur le site de Porto Rico a permis de développer une méthode numérique de type quasi-Newton afin de résoudre le système d'équations qui rend compte du comportement des nucléides et du taux de formation de la saprolite et des couronnes d’altération.Pour les bassins du Gange et du Brahmapoutre, les sédiments ont été collectés sur différents affluents et à son exutoire. La variation des déséquilibres 238U-234U-230Th dans les sédiments, différente pour les sédiments en suspension et les sédiments à grains grossiers d’amont en aval, semble être une caractéristique générale des rivières himalayennes coulant dans la plaine Indo-gangétique. Par ce travail de thèse, nous avons montré l’utilité d’inclure l’analyse du 226Ra à l’analyse des autres nucléides de la chaîne de décroissance radioactive de l’238U (l’238U -234U-230Th 230Th) pour déterminer un taux d’altération dans un système bien défini. Néanmoins, l’étude du système du Brahmapoutre montre que la méthode proposée demande à être affinée car le transfert sédimentaire est un processus plus complexe dû à la variabilité minéralogique, granulométrique et à la dynamique sédimentaire (locale) des échantillons récoltés. / This thesis proposes to define the time-scales of weathering processes on a spheroidal weathering profile, (Rio Icacos watershed, Puerto Rico ) and the transfer time of sediments within alluvial plains (Ganges and Brahmaputra basins). This issue is addressed through the analysis of the nuclides of the 238U decay chain. The study of a spheroidal weathering system developed on the site of Puerto Rico permit to develop a limited memory quasi-Newton algorithm in order to solve the system of equations that reflects the behavior of nuclides and the rate of formation of the saprolite and the rindlet zone. For the Ganges and Brahmaputra basins, sediments were collected from different tributaries and their outlets. The variation of 238U - 234U - 230Th disequilibria in the sediments, with different variation trends for suspended and coarse-grained sediments, is probably a general feature of all Himalayan rivers flowing across the Indo-Gangetic plain. For this work, we have shown the usefulness of including the analysis of 226Ra analysis of other nuclides in the chain of radioactive decay of 238U (238U - 234U - 230Th) to determine the weathering rate in a well-defined system. Nevertheless, the study of the Brahmaputra system shows that proposed method needs to be refined as the sediment transfer is a complex process due to the mineralogical variability, size and (local) dynamics of sediments samples collected.

Bangladesh and India share 54 transboundary rivers. Despite that, the transboundary water management between these two countries is heavily concentrated on the Ganges river basin, in which, mode of cooperation is still based on physical sharing of water. The study is developed on the argument that Bangladesh and India need a shift of focus in their current mode of transboundary water management from physical sharing of water to sharing of benefits derived from the use (and non-use) water in order to foster transboundary water cooperation in the Ganges river basin. Based on a single-case study, the research work aims to explore the scope of benefit-sharing in the transboundary water cooperation in the Ganges river basin and how benefit-sharing can be facilitated between these two countries. The findings show that the water negotiation in the Ganges basin would become much more complicated in the future, primarily due to the growing gap between the demand and the availability of water. The adverse impact of climate change will further deteriorate the situation. Besides, the changing nature of India’s domestic politics and the growing internal conflict between its provincial states will weaken the Indian central government’s authority to manage transboundary water resources jointly. Therefore, in the future, Bangladesh and India would find it difficult to elicit a positive-sum outcome from any water negotiation in Ganges river if they still focus on the volumetric allocation of water. The study suggests that inland navigation and water transit, multipurpose storage dam projects and joint management of the Sundarbans can be the potential areas for benefit-sharing in the Ganges basin. The study stresses the importance of shifting the policy outlook and developing institutional arrangements between Bangladesh and India to introduce and facilitate benefit-sharing in the Ganges river basin that will help to share benefits equitably, hence foster cooperation.

No description available.

The aim is to propose solutions to the new bridge construction due to its unsatisfactory compared to the existing bridge reconstruction project . There are three studies bridging and selected variant trapezoidal plate further processed static opinion. The design was judged by the ultimate limit states and usability. Partial assessments were made for the anchoring system, anchorage area , unravels notched bars and store design to support .