24. Sarhadi, A., Soltani, S., & Modarres, R. (2012). Probabilistic flood inundation mapping of ungauged rivers: Linking GIS techniques and frequency analysis.Journal of Hydrology, 458, 68-86. 25. Qi, H., Qi, P., & Altinakar, M. S. (2013).
Spellman. F, 2000, The Science of Water: Concepts and Applications, Second Edition, CRC Press, Page 76 Richards, K.S., 1978. Simulation of flow geometry in a riffle–pool stream. Earth Surface Processes and Landforms 3, 345–354. Thompson et al., 1998, D.M.
Rivers and streams are the main transporters of sediment and rock and they are known for their powerful erosional capabilities. Sediment and rock travel down gradient from location to location until they come to rest in a delta or they are deposited when the velocity of the water has become too slow to move the debris any further. Secondary streams, although known for moving less sediment or rock, still retain the power to erode and transport. Muddy Run, a secondary bedrock stream in Oneida Township, Huntingdon County, Pennsylvania, is one such example. Bedrock streams, instead of just flowing over the ground, cut down into the local bedrock (Seidl & Dietrich 1993).
September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1. Section 1: Geology Part I: Bedrock Knob The site visited on this day was informally known as the Bedrock Knob (NTS grid reference: 120 342).
His second hypothesis was that if iron did direct the yield in high nutrient, low chlorophyll waters and also absorb organic carbon into the depths of the ocean through the use of the biological pump then this could explain the observations made through ice cores he had collected. The ice cores had shown that carbon had a direct relationship with the climatic changes of the planet. Martin proposed, using his hypotheses, that fertilizing the ocean with iron in these HNLC waters could export atmospheric carbon dioxide into the oceanic sediment and seize it for many years. The Carbon Cycle in reference to the fertilization of the ocean can be simply explained by understanding that phytoplankton uses the carbon dioxide to grow. Carbon dioxide reaches the ocean surface and is photosynthesized by the phytoplankton which in turn grows into larger blooms.
Hydrologica l Processes, 10(2), 295-313. Smith, V. H., Joye, S. B., & Howarth, R. W. (2006). Eutrophication of freshwater and marine ecosystems. Limnology and Oceanography, 51(1), 351-355. .Smith, V. H., Tilman, G. D., & Nekola, J. C. (1999).
This study describes the bacterial adsorbents, their modification and mechanism for removal of copper. A brief description of Langmuir and Freundlich isotherm modelling is provided in this paper. Keywords: Bioremediation, biosorption, biosorbent, bacteria, heavy metals, copper. Introduction The intensive development of industry, agricultural practices and modern technologies are leading to the release of significant amount of contaminants to the environment (Ayres, 1992). Metals are inorganic form of contaminants whose extensive use has caused significant environmental pollution that mainly affects soil, watercourses, atmosphere and living systems (Kasassi et al., 2008).
Modeling Hydrology and Sediment Transport in Vegetative Filter Strips. J. of Hydrology. 214, (1999): 111-129 . (Muñoz-Carpena 1998) Skaggs, R. W., M. A. Breve, and J. W. Gilliam. 1995.
Stoner, M.G., & F.C. Ugolini, January 1968, "Arctic Pedogenesis: 2. Threshold-Controlled Subsurface Leaching Episodes." Soil Science, 145, p.46-50.
Available: http://www.nps.gov/olym/elwha /docs/eis96/elwha2.htm. --. Elwha River Restoration Project, Washington: Sediment Analysis and Modeling of the River Erosion Alternative, Elwha Technical Series, FN-95-9 (Aug. 1996). n. pag. Online.