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Featured researches published by Louis A. Kaplan.


Microbial Ecology | 1984

Benthic bacterial biomass supported by streamwater dissolved organic matter

Thomas L. Bott; Louis A. Kaplan; Frank T. Kuserk

Bacterial biomass in surface sediments of a headwater stream was measured as a function of dissolved organic carbon (DOC) flux and temperature. Bacterial biomass was estimated using epifluorescence microscopic counts (EMC) and ATP determinations during exposure to streamwater containing 1,788μg DOC/liter and after transfer to groundwater containing 693μg DOC/liter. Numbers of bacteria and ATP concentrations averaged 1.36×109 cells and 1,064 ng per gram dry sediment, respectively, under initial DOC exposure. After transfer to low DOC water, biomass estimates dropped by 53 and 55% from EMC and ATP, respectively. The decline to a new steady state occurred within 4 days from ATP assays and within 11 days from EMC measures. A 4°C difference during these exposures had little effect on generation times. The experiment indicated that 27.59 mg/hour of natural DOC supported a steady state bacterial biomass of approximately 10μg C/g dry weight of sediment (from EMC determinations). Steady state bacterial biomass estimates on sediments that were previously muffled to remove organic matter were approximately 20-fold lower. The ratio of GTP∶ATP indicated differences in physiological condition or community composition between natural and muffled sediments.


Journal of Environmental Monitoring | 2002

Monitoring dissolved organic carbon in surface and drinking waters

Christian Volk; Larry Wood; Bruce Johnson; Jeff Robinson; Hai Wei Zhu; Louis A. Kaplan

The presence of natural organic matter (NOM) strongly impacts drinking water treatment, water quality, and water behavior during distribution. Dissolved organic carbon (DOC) concentrations were determined daily over a 22 month period in river water before and after conventional drinking water treatment using an on-line total organic carbon (TOC) analyzer. Quantitative and qualitative variations in organic matter were related to precipitation and runoff, seasons and operating conditions. Following a rainfall event, DOC levels could increase by 3.5 fold over baseflow concentrations, while color, UV absorbance values and turbidity increased by a factor of 8, 12 and 300, respectively. Treated water DOC levels were closely related to the source water quality, with an average organic matter removal of 42% after treatment.


Organic Geochemistry | 1998

Isolation and analysis of lignin-derived phenols in aquatic humic substances : improvements on the procedures

Laurel J. Standley; Louis A. Kaplan

Abstract Procedures for the extraction of aquatic humic substances and analysis of their lignin-derived phenols were assessed and altered to simplify and shorten XAD-8 resin cleaning, reduce losses due to sorption, and optimize oxidative release of phenols without increasing their transformation. The revised cleaning procedures require 5 rather than 120xa0h and sorptive losses of humic acids were reduced 7%. Coefficients of variation for individual phenols in the final method ranged from 1 to 11%. The method was used to analyze lignin-derived phenols in White Clay Creek watershed humics, Suwannee River humics (IHSS), and Lake Washington sediments.


Compost Science & Utilization | 1995

Impact on Water Quality of High and Low Density Applications of Spent Mushroom Substrate to Agricultural Lands

Louis A. Kaplan; Laurel J. Standley; J. Denis Newbold

We studied the influence of spent mushroom substrate (SMS) land application on water resources. Four study sites, including mushroom farms with low or high density land applications of SMS, and two controls, an alfalfa field and a woodland, were instrumented with soilwater lysimeters and groundwater monitoring wells. Water samples were collected during the dormant season (winter) and growing season (spring). Samples were analyzed for a number of water quality parameters, including dissolved organic carbon (DOC), dissolved organic nitrogen (DON), ammonia, chloride, nitrate, nitrite, phosphate, sulfate, aluminum, cadmium, calcium, chromium, copper, iron, lead, magnesium, manganese, mercury, nickel, potassium, silicon, sodium, and zinc. Additional analyses were performed for pesticides commonly used in the cultivation of alfalfa or corn, or for insect control, including methomyl, dimethoate, hexazinone, atrazine, diuron and permethrin.All agricultural sites had elevated salt concentrations relative to the wo...


Limnology and Oceanography | 1997

Chemical composition of biodegradable dissolved organic matter in streamwater

Christian Volk; Catherine B. Volk; Louis A. Kaplan


Freshwater Biology | 1998

The role of micro-organisms in the ecological connectivity of running waters

Martin T. Pusch; Douglas Michael Fiebig; Ingrid Brettar; Heinrich Eisenmann; Bonnie K. Ellis; Louis A. Kaplan; Maurice A. Lock; Markus W. Naegeli; Walter Traunspurger


Limnology and Oceanography | 1982

Diel fluctuations of DOC generated by algae in a piedmont stream1

Louis A. Kaplan; Thomas L. Bott


Limnology and Oceanography | 1989

Diel fluctuations in bacterial activity on streambed substrata during vernal algal blooms: Effects of temperature, water chemistry, and habitat

Louis A. Kaplan; Thomas L. Bott


Environmental Science & Technology | 2000

Molecular Tracers of Organic Matter Sources to Surface Water Resources

Laurel J. Standley; Louis A. Kaplan; Darrell Smith


Limnology and Oceanography | 1992

Comparison of high-temperature and persulfate oxidation methods for determination of dissolved organic carbon in freshwaters

Louis A. Kaplan

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Thomas L. Bott

Academy of Natural Sciences of Drexel University

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Laurel J. Standley

Academy of Natural Sciences of Drexel University

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Christian Volk

Academy of Natural Sciences of Drexel University

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Catherine B. Volk

Academy of Natural Sciences of Drexel University

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George R. Aiken

United States Geological Survey

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J. Denis Newbold

Academy of Natural Sciences of Drexel University

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James Weishaar

United States Geological Survey

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Richard A. Larson

Academy of Natural Sciences of Drexel University

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