Temporal changes in hydraulic conductivity of sand porous media biofilters during wastewater infiltration due to biomat formation

Deborah N Huntzinger, John E. McCray, Kathryn S. Lowe, Robert L. Siegrist

Research output: Contribution to journalArticle

43 Citations (Scopus)

Abstract

Porous media biofilters (PMBs) are commonly used to treat domestic wastewater. Biomats develop at the infiltrative surface of PMBs due to continued wastewater application and create an impedance to flow. The goal of this research is to quantify the temporal evolution of normalized biomat hydraulic conductivity (Kbm/bbm) and effective hydraulic conductivity (Ke). Ke is the overall hydraulic conductivity of the infiltrative zone, including biomat and unsaturated media below the biomat. Research was conducted using eight one-dimensional (1D) sand columns with gravel-free and gravel-laden infiltrative surfaces. The columns were loaded at design rates of 100-200 cm/d for 20 weeks of column operation. The Ke values for these continuously loaded columns were determined from analyses of bromide-tracer tests, falling-head permeability tests, and volumetric water content measurements during biomat development. The reduction in the Ke due to biomat formation is due to two factors: reduced hydraulic conductivity of the thin biomat, and a reduced hydraulic conductivity of the subsoil due to development of a biomat-induced unsaturated flow regime. Unsaturated hydraulic conductivities of the subsoil below the biomat (K ss) were estimated from capillary curves and water content measurements. For observed final biomat thicknesses (less than 1 cm), the biomat hydraulic conductivity, Kbm, is three orders of magnitude smaller than the unsaturated hydraulic conductivity (Kss). However, the relatively large thickness of the vadose zone causes the Kss to be an important contributor to the overall Ke value. For these columns, the final Ke values were approximately two orders of magnitude smaller than the original value. Because the exact thickness of the biomat (bbm) is unknown during the flow experiments, the hydraulic conductance of the biomat zone is presented using a normalized hydraulic conductivity function (Kbm/bbm). A similar K bm/bbm is reached regardless of wastewater loading rate. An exponential relationship exists between the volume of wastewater applied to the column and both Ke and Kbm/bbm.

Original languageEnglish (US)
Pages (from-to)230-243
Number of pages14
JournalJournal of Hydrology
Volume311
Issue number1-4
DOIs
StatePublished - Sep 15 2005
Externally publishedYes

Fingerprint

biofilters
porous media
hydraulic conductivity
infiltration (hydrology)
wastewater
porous medium
infiltration
sand
unsaturated hydraulic conductivity
subsoil
gravel
water content
unsaturated flow
unsaturated medium
vadose zone
impedance
bromides
tracer techniques
permeability
fluid mechanics

Keywords

  • Biomat
  • Hydraulic conductivity
  • Infiltration
  • Porous media biofilters
  • Wastewater

ASJC Scopus subject areas

  • Soil Science
  • Earth-Surface Processes

Cite this

Temporal changes in hydraulic conductivity of sand porous media biofilters during wastewater infiltration due to biomat formation. / Huntzinger, Deborah N; McCray, John E.; Lowe, Kathryn S.; Siegrist, Robert L.

In: Journal of Hydrology, Vol. 311, No. 1-4, 15.09.2005, p. 230-243.

Research output: Contribution to journalArticle

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