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Michael H. Bothner

Researcher at United States Geological Survey

Publications -  70
Citations -  2829

Michael H. Bothner is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Sediment & Bay. The author has an hindex of 28, co-authored 70 publications receiving 2681 citations. Previous affiliations of Michael H. Bothner include Woods Hole Oceanographic Institution.

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Transport of sludge-derived organic pollutants to deep-sea sediments at deep water dump site 106

TL;DR: Findings clearly indicate that organic pollutants derived from dumped sludge are transported through the water column and have accumulated on the deep-sea floor.
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Metal concentrations in surface sediments of boston harbor—Changes with time

TL;DR: In this paper, the concentrations of metals in surface sediments of Boston Harbor have decreased during the period 1977-1993, which is supported by analysis of surface sediment collected at monitoring stations in the outer harbor between 1977 and 1993; and historical data from a contaminated-sediment database.
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Insights on geochemical cycling of U, Re and Mo from seasonal sampling in Boston Harbor, Massachusetts, USA

TL;DR: In this article, the removal of redox-sensitive metals from continental margin sediments underlying oxic bottom water is investigated, and it is shown that removing redox sensitive metals from seafloor sediments plays a key role in marine budgets of these metals.
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The use (and misuse) of sediment traps in coral reef environments: theory, observations, and suggested protocols

TL;DR: In this article, a review of the state-of-the-art of sediment trap dynamics in shallow-water environ- ments that characterize coral reefs is presented, followed by the first synthesis of near-bed sediment trap data collected with concurrent hydrodynamic information in coral reef environments.
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Rate of mercury loss from contaminated estuarine sediments

TL;DR: The concentration of mercury in contaminated estuarine sediments of Bellingham Bay, Washington was found to decrease with a half-time of about 1.3 yr after the primary anthropogenic source of mercury was removed.