Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Rudolf F, Krachler"'
Publikováno v:
Environmental Science & Technology
In peatlands, bacterial tyrosinases (TYRs) are proposed to act as key regulators of carbon storage by removing phenolic compounds, which inhibit the degradation of organic carbon. Historically, TYR activity has been blocked by anoxia resulting from p
Autor:
Rudolf F. Krachler, Regina Krachler
Publikováno v:
Environmental sciencetechnology. 55(14)
Organic soils in the Arctic-boreal region produce small aquatic humic ligands (SAHLs), a category of naturally occurring complexing agents for iron. Every year, large amounts of SAHLs-loaded with iron mobilized in river basins-reach the oceans via ri
Publikováno v:
Science of The Total Environment. 656:952-958
The present study elucidates the role of natural iron fertilization of the coastal ocean by so-called “blackwater rivers”. Areas of marsh, fen, peatland, boreal forest etc. are characterized by organic-rich soils. From those soils, humic substanc
Autor:
Regina, Krachler, Rudolf F, Krachler, Gabriele, Wallner, Peter, Steier, Yasin, El Abiead, Hubert, Wiesinger, Franz, Jirsa, Bernhard K, Keppler
Publikováno v:
The Science of the total environment. 556
Iron is a micronutrient of particular interest as low levels of iron limit primary production of phytoplankton and carbon fluxes in extended regions of the world's oceans. Sphagnum-peatland runoff is extraordinarily rich in dissolved humic-bound iron
Autor:
Amir Blazevic, Regina Krachler, Bernhard K. Keppler, Wolfgang Kandioller, Franz Jirsa, Annette Rompel, Myrvete Tafili-Kryeziu, Ewelina Orlowska, Wolfgang Linert, Rudolf F. Krachler
Publikováno v:
Angewandte Chemie (Weinheim an Der Bergstrasse, Germany)
'Angewandte Chemie International Edition ', vol: 55, pages: 6417-6422 (2016)
Angewandte Chemie (International Ed. in English)
'Angewandte Chemie International Edition ', vol: 55, pages: 6417-6422 (2016)
Angewandte Chemie (International Ed. in English)
Humic substances (HS) are important iron chelators responsible for the transport of iron from freshwater systems to the open sea, where iron is essential for marine organisms. Evidence suggests that iron complexed to HS comprises the bulk of the iron
Autor:
Bernhard K. Keppler, Regina Krachler, Thilo Hofmann, Rudolf F. Krachler, Frank von der Kammer, Shahram Ayromlou, Franz Jirsa, Altan Süphandag
Publikováno v:
Science of The Total Environment. 408:2402-2408
Peat bogs have the ability to produce strong chelate ligands (humic and fulvic acids) which enhance the weathering rates of iron-silicate minerals and greatly increase the solubility of the essential trace metal iron in river water. Fluvial networks
Autor:
Dieter Mader, Franz Jirsa, Daniel Kogelnig, Regina Krachler, Rudolf F. Krachler, Barbara Mitteregger, Anja Stojanovic
Publikováno v:
Geochemistry. 69:223-234
General geochemical parameters of water, superficial sediments, and suspended particulate matter (SPM) were determined from small shallow saline lakes (soda ponds) as well as from lake Neusiedlersee in eastern Austria. Additionally, instrumental neut
Autor:
Regina, Krachler, Rudolf F, Krachler, Gabriele, Wallner, Stephan, Hann, Monika, Laux, Maria F, Cervantes Recalde, Franz, Jirsa, Elisabeth, Neubauer, Frank, von der Kammer, Thilo, Hofmann, Bernhard K, Keppler
Publikováno v:
Marine Chemistry
The speciation of iron(III) in oxic seawater is dominated by its hydrolysis and sedimentation of insoluble iron(III)-oxyhydroxide. As a consequence, many oceanic areas have very low iron levels in surface seawater which leads to iron deficiency since
Autor:
Christof Plessl, Thilo Hofmann, Frank von der Kammer, Rudolf F. Krachler, Franz Jirsa, Altan Süphandag, Bernhard K. Keppler, Regina Krachler, Margret Vogt
Publikováno v:
Global Biogeochemical Cycles. 26
[1] Primary production in large areas of the open ocean is limited by low iron concentrations. Rivers are potential sources of iron to the ocean, however, riverine iron is prone to intense flocculation and sedimentation in the estuarine mixing zone.
To date, little is known about the pH-stimulated mineralization of organic matter in aquatic environments. In this study, we investigated biodegradation processes in alkaline waters. Study site is a large shallow soda lake in Central Europe (Neusiedl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f45537940ad0455d4a96abdf1123972f
https://doi.org/10.5194/bgd-6-491-2009
https://doi.org/10.5194/bgd-6-491-2009