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INTERFACIAL VELOCITY EFFECTS ON SEDIMENT OXYGEN DEMAND MEASUREMENT Raymond C. Whittemore, Research Engineer National Council of the Paper Industry for Air and Stream Improvement Tufts University Medford, Massachusetts 02155 The importance of organic bottom deposits on the oxygen balance of a river or estuary was recognized in 1925 [1]. Since that time research efforts attempting to define the mechanism of oxygen consumption, effects of pertinent environmental variables, and methods of measurement of sediment oxygen demand (SOD) have appeared in numerous journals. SOD remains of interest in receiving waters where bottom deposits are seasonal or historical (i.e., built up during years preceding treatment). Present and future water quality management decisions require an accurate assessment of the impact of these deposits on the oxygen balance. Bowman and Delfino [2) concluded that an acceptable SOD measurement technique should be consistent, reproducible, and efficient. They further state that laboratory experiments with undisturbed cores accommodate these three criteria and, therefore, represent a realistic approach to standardizing SOD measurements. There is, however, little evidence to suggest that laboratory experiments produce the same results as in-situ methods. The hydrodynamics and biology of the instream sediment interface cannot be consistently simulated with laboratory core methods. A standardized SOD measurement technique cannot be developed until this question of accuracy is resolved. The research to be described in this paper will focus on defining the hydrodynamic factors affecting SOD, particularly velocity at the sediment-water interface. Two different in-situ SOD devices were constructed and used in several rivers in the Northeast and Mid-Atlantic states during the period 1977-1980. EXPERIMENTAL PROCEDURES In-Situ Respirometer An in-situ respirometer was built for field work and is pictured in Figure 1. It consisted of an 18" diameter plexiglass cylinder 12" in height. A steel flange (30" outside diameter with an 18" diameter hole) was placed around the bottom. A 3" diameter steel cutting KCL SYRINGE 0, PROBE \ . DC STIRHifl mill, T SEDIMENT / ////// Figure 1. Schematic of an in-situ respirometer. 711
Object Description
Purdue Identification Number | ETRIWC198174 |
Title | Interfacial velocity effects on sediment oxygen demand measurement |
Author | Whittemore, Raymond C. |
Date of Original | 1981 |
Conference Title | Proceedings of the 36th Industrial Waste Conference |
Conference Front Matter (copy and paste) | http://earchives.lib.purdue.edu/u?/engext,32118 |
Extent of Original | p. 711-717 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital object copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Date Digitized | 2009-07-07 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Resolution | 300 ppi |
Color Depth | 8 bit |
Description
Title | page 711 |
Collection Title | Engineering Technical Reports Collection, Purdue University |
Repository | Purdue University Libraries |
Rights Statement | Digital copyright Purdue University. All rights reserved. |
Language | eng |
Type (DCMI) | text |
Format | JP2 |
Capture Device | Fujitsu fi-5650C |
Capture Details | ScandAll 21 |
Transcript | INTERFACIAL VELOCITY EFFECTS ON SEDIMENT OXYGEN DEMAND MEASUREMENT Raymond C. Whittemore, Research Engineer National Council of the Paper Industry for Air and Stream Improvement Tufts University Medford, Massachusetts 02155 The importance of organic bottom deposits on the oxygen balance of a river or estuary was recognized in 1925 [1]. Since that time research efforts attempting to define the mechanism of oxygen consumption, effects of pertinent environmental variables, and methods of measurement of sediment oxygen demand (SOD) have appeared in numerous journals. SOD remains of interest in receiving waters where bottom deposits are seasonal or historical (i.e., built up during years preceding treatment). Present and future water quality management decisions require an accurate assessment of the impact of these deposits on the oxygen balance. Bowman and Delfino [2) concluded that an acceptable SOD measurement technique should be consistent, reproducible, and efficient. They further state that laboratory experiments with undisturbed cores accommodate these three criteria and, therefore, represent a realistic approach to standardizing SOD measurements. There is, however, little evidence to suggest that laboratory experiments produce the same results as in-situ methods. The hydrodynamics and biology of the instream sediment interface cannot be consistently simulated with laboratory core methods. A standardized SOD measurement technique cannot be developed until this question of accuracy is resolved. The research to be described in this paper will focus on defining the hydrodynamic factors affecting SOD, particularly velocity at the sediment-water interface. Two different in-situ SOD devices were constructed and used in several rivers in the Northeast and Mid-Atlantic states during the period 1977-1980. EXPERIMENTAL PROCEDURES In-Situ Respirometer An in-situ respirometer was built for field work and is pictured in Figure 1. It consisted of an 18" diameter plexiglass cylinder 12" in height. A steel flange (30" outside diameter with an 18" diameter hole) was placed around the bottom. A 3" diameter steel cutting KCL SYRINGE 0, PROBE \ . DC STIRHifl mill, T SEDIMENT / ////// Figure 1. Schematic of an in-situ respirometer. 711 |
Resolution | 300 ppi |
Color Depth | 8 bit |
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