نتایج جستجو برای: deep water sediments

تعداد نتایج: 764487  

1995
C. Christiansen

The yearly nutrient supply from land and atmosphere to the study area in SW Kattegat is 10 900 tons of N and 365 tons of P. This is only few percent of the supply from adjacent marine areas, as the yearly transport through the study area is 218 000 tons of N and 18 250 tons of P. Yearly net deposition makes up 1340 tons of N (on average 2.5 g m yr) and 477 ton of P (on average 0.9 g m yr). Shal...

2006
Ulrich Wand Alfred Wegener Vladimir A. Samarkin Georgia Horst-Michael Nitzsche Hans-Wolfgang Hubberten

We found unprecedentedly high abundances of microbially produced CH4 in the anoxic deep waters of Lake Untersee, an oligotrophic, perennially ice-covered Antarctic freshwater lake. The maximum CH4 concentration (approaching 21.8 6 1.4 mmol L21) is one of the highest observed so far in a natural aquatic ecosystem. Although surficial lake sediments are the predominant source of CH4 in Lake Unters...

Journal: :Eos, Transactions American Geophysical Union 2012

2014
Jacobo Martín Pere Puig Pere Masqué Albert Palanques Anabel Sánchez-Gómez

The offshore displacement of commercial bottom trawling has raised concerns about the impact of this destructive fishing practice on the deep seafloor, which is in general characterized by lower resilience than shallow water regions. This study focuses on the flanks of La Fonera (or Palamós) submarine canyon in the Northwestern Mediterranean, where an intensive bottom trawl fishery has been act...

2016
David J. Burdige Tomoko Komada

This Article is brought to you for free and open access by the Ocean, Earth & Atmospheric Sciences at ODU Digital Commons. It has been accepted for inclusion in OEAS Faculty Publications by an authorized administrator of ODU Digital Commons. For more information, please contact [email protected]. Repository Citation Burdige, David J. and Komada, Tomoko, "Using Ammonium Pore Water Profiles ...

2016
Khan Z. Jadoon Samir Al-Mashharawi Sherif M. Hanafy Gerard T. Schuster Thomas M. Missimer

Wadi aquifers in Saudi Arabia historically have been recharged primarily by channel loss (infiltration) during floods. Historically, seasonal groundwater levels fluctuated from land surface to about 3 m below the surface. Agricultural irrigation pumping has lowered the water table up to 35 m below the surface. The geology surrounding the fluvial system at Wadi Qidayd consists of pelitic Precamb...

2011
Christiane Hasemann Thomas Soltwedel

The unexpected high species richness of deep-sea sediments gives rise to the questions, which processes produce and maintain diversity in the deep sea, and at what spatial scales do these processes operate? The idea of a small-scale habitat structure at the deep-sea floor provides the background for this study. At small scales biogenic structures create a heterogeneous environment that influenc...

Journal: :Environmental science & technology 2012
Laura Ruhl Avner Vengosh Gary S Dwyer Heileen Hsu-Kim Grace Schwartz Autumn Romanski S Daniel Smith

The combustion of coal to generate electricity produces about 130 million tons of coal combustion residues (CCRs) each year in the United States; yet their environmental implications are not well constrained. This study systematically documents the quality of effluents discharged from CCR settling ponds or cooling water at ten sites and the impact on associated waterways in North Carolina, comp...

2000
K.-C. Emeis U. Struck T. Leipe F. Pollehne H. Kunzendorf C. Christiansen

Three major depositional basins (the Gdansk, Bornholm and Eastern Gotland basins) of the Baltic Proper, which together account for .50% of the depositional areas in the entire Baltic Sea, have accumulated increased amounts of sediment and organic carbon during the last 50 years, as is shown in Pb-dated sediment cores. The shallow Arkona Basin has had constant accumulation rates and rate increas...

2012
Sarah Sokoll Moritz Holtappels Phyllis Lam Gavin Collins Michael Schlüter Gaute Lavik Marcel M. M. Kuypers

A pronounced deficit of nitrogen (N) in the oxygen minimum zone (OMZ) of the Arabian Sea suggests the occurrence of heavy N-loss that is commonly attributed to pelagic processes. However, the OMZ water is in direct contact with sediments on three sides of the basin. Contribution from benthic N-loss to the total N-loss in the Arabian Sea remains largely unassessed. In October 2007, we sampled th...

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