This report presents a model of manganese and iron flux from sediments. The reaction kinetics for iron and manganese in the overlying water column are also developed. As shown below, the chemistry of iron and manganese are sufficiently similar so that a common model formulation can be used. The model is an extension of the nutrient and oxygen sediment flux model developed previously for application to Chesapeake Bay. It has subsequently been applied to freshwater lake sediments as well. Thus the model developed in this report is a comprehensive model for nutrients, oxygen and sulfide, and now iron and manganese
In recent years, reaction transport models have gained importance in the study of diagenesis, which ...
Iron and manganese in bottom sediments studied along the sublatitudinal transect from Kandalaksha to...
We studied the concentration of a series of transition metals including Mn and Fe in an estuarine fi...
The effect of benthic oxygenic photosynthesis on sediment-water fluxes of manganese and iron was stu...
A steady state diagenetic model is developed which accounts for changes in both the pore water and s...
Eutrophication is a process, when aquatic bodies are affected by high nutrients loads, which is foll...
Water column data and porewater profiles are used to study the chemical evolution with time and with...
International audiencePore water and solid phase geochemical profiles of sediment cores collected al...
The role of redox processes in determining the chemistry of iron and manganese is considered systema...
Phytoplankton in the oceans are responsible for about half of the photosynthetic fixation of carbon ...
A computer-generated chemical equilibrium model has been developed to predict the unusual seasonal v...
A steady state, coupled, non-linear model has been developed for early diagenetic processes in pelag...
Our laboratory flume experiments demonstrate that advective porewater flows produce biogeochemical r...
Suspended matter and sediments from the North Sea were analysed for Al, Fe and Mn. A seasonal variat...
Processes controlling the distribution and mobility of Fe and Mn in Lake Sammamish, Wash-ington, a s...
In recent years, reaction transport models have gained importance in the study of diagenesis, which ...
Iron and manganese in bottom sediments studied along the sublatitudinal transect from Kandalaksha to...
We studied the concentration of a series of transition metals including Mn and Fe in an estuarine fi...
The effect of benthic oxygenic photosynthesis on sediment-water fluxes of manganese and iron was stu...
A steady state diagenetic model is developed which accounts for changes in both the pore water and s...
Eutrophication is a process, when aquatic bodies are affected by high nutrients loads, which is foll...
Water column data and porewater profiles are used to study the chemical evolution with time and with...
International audiencePore water and solid phase geochemical profiles of sediment cores collected al...
The role of redox processes in determining the chemistry of iron and manganese is considered systema...
Phytoplankton in the oceans are responsible for about half of the photosynthetic fixation of carbon ...
A computer-generated chemical equilibrium model has been developed to predict the unusual seasonal v...
A steady state, coupled, non-linear model has been developed for early diagenetic processes in pelag...
Our laboratory flume experiments demonstrate that advective porewater flows produce biogeochemical r...
Suspended matter and sediments from the North Sea were analysed for Al, Fe and Mn. A seasonal variat...
Processes controlling the distribution and mobility of Fe and Mn in Lake Sammamish, Wash-ington, a s...
In recent years, reaction transport models have gained importance in the study of diagenesis, which ...
Iron and manganese in bottom sediments studied along the sublatitudinal transect from Kandalaksha to...
We studied the concentration of a series of transition metals including Mn and Fe in an estuarine fi...