نتایج جستجو برای: sediment bypass tunnel

تعداد نتایج: 122364  

2014
Menachem M. Meller Amber B. Courville Anne E. Sumner

The prevalence of class III obesity (BMI ≥ 40 kg/m(2)) in black women is 18%. As class III obesity leads to hip joint deterioration, black women frequently present for orthopedic care. Weight loss associated with bariatric surgery should lead to enhanced success of hip replacements. However, we present a case of a black woman who underwent Roux-en-Y gastric bypass with the expectation that weig...

Journal: :Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) 2012

2003
Haim Tsoar Eugene Berman

Most aeolian sediment transport models and experiments have been conducted on flat horizontal surfaces. Very little numerical or analytical research has been carried out for aeolian sand transport on slopes. The current work presents numerical modelling of saltating sand for a climbing dune which has a slope angle of 20”. The model utilised wind fields predicted from the FAA complex terrain mod...

2016
Emily Denise Melton Dimitry Y Sorokin Lex Overmars Olga Chertkov Alicia Clum Manoj Pillay Natalia Ivanova Nicole Shapiro Nikos C Kyrpides Tanja Woyke Alla L Lapidus Gerard Muyzer

Desulfurivibrio alkaliphilus strain AHT2(T) is a strictly anaerobic sulfidogenic haloalkaliphile isolated from a composite sediment sample of eight hypersaline alkaline lakes in the Wadi al Natrun valley in the Egyptian Libyan Desert. D. alkaliphilus AHT2(T) is Gram-negative and belongs to the family Desulfobulbaceae within the Deltaproteobacteria. Here we report its genome sequence, which cont...

2015
C. Seabird McKeon Björn G. Tunberg Cora A. Johnston Daniel J. Barshis Alex Ford

Community composition of the infaunal bivalve fauna of the St. Lucie Estuary and southern Indian River Lagoon, eastern Florida was sampled quarterly for 10 years as part of a long-term benthic monitoring program. A total of 38,514 bivalves of 137 taxa were collected and identified. We utilized this data, along with sediment samples and environmental measurements gathered concurrently, to assess...

2016
James T. Morris Donald C. Barber John C. Callaway Randy Chambers Scott C. Hagen Charles S. Hopkinson Beverly J. Johnson Patrick Megonigal Scott C. Neubauer Tiffany Troxler Cathleen Wigand

A mixing model derived from first principles describes the bulk density (BD) of intertidal wetland sediments as a function of loss on ignition (LOI). The model assumes that the bulk volume of sediment equates to the sum of self-packing volumes of organic and mineral components or BD = 1/[LOI/k1 + (1-LOI)/k2], where k1 and k2 are the self-packing densities of the pure organic and inorganic compo...

2008
Louis J. Thibodeaux Kalliat T. Valsaraj Kenneth Fountain Cynthia L. Price

This report describes a series of investigations conducted examining a number of specific factors that control air emissions associated with the dredging of Indiana Harbor and Canal (IHC) and associated IHC Confined Disposal Facility (CDF) operations. Three primary objectives were addressed: (1) measurement of Henry’s Law constants and sediment-water desorption constants for various chemicals i...

2006
J. Belnap S. L. Phillips J. E. Herrick J. R. Johansen

Recently disturbed and ‘control’ (i.e. less recently disturbed) soils in the Mojave Desert were compared for their vulnerability to wind erosion, using a wind tunnel, before and after being experimentally trampled. Before trampling, control sites had greater cyanobacterial biomass, soil surface stability, threshold friction velocities (TFV; i.e. the wind speed required to move soil particles), ...

2013
F. Falcini E. Foufoula-Georgiou V. Ganti C. Paola V. R. Voller

[1] Models for the overall topographic evolution of erosional and depositional systems can be grouped into two broad classes. The first class is local models in which the sediment flux at a point is expressed as a linear or nonlinear function of local hydrogeomorphic measures (e.g., water discharge and slope). The second class is nonlocal models, where the sediment flux at a point is expressed ...

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