Biological Nitrogen Removal Database

A manually curated data resource for microbial nitrogen removal


Groundwater Water systems


Experimental setup


Influent:Groundwater flow

Denitrification system:Chemoautotrophic hydrogenotrophic denitrification

Denitrifying reactor:Continuous flow fixed film reactor

Medium:Microporous polyethylene membranes

Culture taken from:nan

Organism (s) cultured:nan

Respiration:Anaerobic

Electron donor:Hydrogen

Electron acceptor:Nitrate


Experimental Information


Input NO3-N (mg/l):nan

Nitrate removal rate (mg NO3-N/l/h):nan

Denitrification rate (gNO3-N removed/m3/day):nan

Microorganisms identified:nan

Molecular tools:nan


Information about Article


Major findings:Results on the behavioral gas transfer studies using porous membranes in groundwater flow systems suggest that porous membranes can be applied effectively in experiments for enhancing in-situ bioremediation of groundwater.

Authors:Fang et al., 2002

Title:Passive Dissolution of Hydrogen Gas Into Groundwater Using Hollow-Fiber Membranes

Pubmed link:Link

Full research link:Link

Abstract:A new hollow-fiber membrane remediation system has recently been developed to passively supply groundwater with dissolved hydrogen (H2) to stimulate the biodegradation of chlorinated solvents. Understanding the mass transfer behavior of membranes under conditions of creeping flow is critical for the design of such systems. Therefore, the objectives of this research were to evaluate the gas transfer behavior of hollow-fiber membranes under conditions typical of groundwater flow and to assess the effect of membrane configuration on gas transfer performance. Membrane gas transfer was evaluated using laboratory-scale glass columns operated at low flow velocities (8.6–12,973 cm/d). H2 was supplied to the inside of the membrane fibers while water flowed on the outside and normal to the fibers (i.e. cross-flow). Membrane configuration (single fiber and fabric) and membrane spacing for the fabric modules did not affect gas transfer performance. Therefore, the results from all of the experiments were combined to obtain the following dimensionless Sherwood number (Sh) correlation expressed as a function of Reynolds number (Re) and Schmidt number (Sc): Sh=0.824Re0.39Sc0.33 (0.0004<Re<0.6). This correlation is useful for predicting the rate of transfer of any gas from clean membranes to flowing water at low Re. This correlation provides a basis for estimating the membrane surface area requirements for groundwater remediation as illustrated by a simple example.