| contributor author | Ben L. O’Connor | |
| contributor author | Miki Hondzo | |
| contributor author | Judson W. Harvey | |
| date accessioned | 2017-05-08T21:41:26Z | |
| date available | 2017-05-08T21:41:26Z | |
| date copyright | December 2009 | |
| date issued | 2009 | |
| identifier other | %28asce%29ee%2E1943-7870%2E0000101.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl/handle/yetl/59494 | |
| description abstract | Traditionally, dissolved oxygen (DO) fluxes have been calculated using the thin-film theory with DO microstructure data in systems characterized by fine sediments and low velocities. However, recent experimental evidence of fluctuating DO concentrations near the sediment-water interface suggests that turbulence and coherent motions control the mass transfer, and the surface renewal theory gives a more mechanistic model for quantifying fluxes. Both models involve quantifying the mass transfer coefficient | |
| publisher | American Society of Civil Engineers | |
| title | Incorporating Both Physical and Kinetic Limitations in Quantifying Dissolved Oxygen Flux to Aquatic Sediments | |
| type | Journal Paper | |
| journal volume | 135 | |
| journal issue | 12 | |
| journal title | Journal of Environmental Engineering | |
| identifier doi | 10.1061/(ASCE)EE.1943-7870.0000093 | |
| tree | Journal of Environmental Engineering:;2009:;Volume ( 135 ):;issue: 012 | |
| contenttype | Fulltext | |
