63 citations as recorded by crossref.

1. Benzoic hydroxamate-based iron complexes as model compounds for humic substances: synthesis, characterization and algal growth experiments E. Orlowska et al. 10.1039/C5RA25256C
2. Iron isotopes reveal seasonal variations in the mechanisms for iron-bearing particle and colloid formation in the Lena River catchment, NE Siberia C. Hirst et al. 10.1016/j.gca.2023.09.016
3. Dissolved iron elution from mangrove ecosystem associated with polyphenols and a herbivorous snail K. Hinokidani & Y. Nakanishi 10.1002/ece3.5199
4. A Comparison between Four Analytical Methods for the Measurement of Fe(II) at Nanomolar Concentrations in Coastal Seawater M. Hopwood et al. 10.3389/fmars.2017.00192
5. Unprecedented Fe delivery from the Congo River margin to the South Atlantic Gyre L. Vieira et al. 10.1038/s41467-019-14255-2
6. Natural organic matter and iron export from the Tanner Moor, Austria F. Jirsa et al. 10.1016/j.limno.2012.09.006
7. Importance of Boreal Rivers in Providing Iron to Marine Waters E. Kritzberg et al. 10.1371/journal.pone.0107500
8. Distribution and chemical speciation of iron on the outer edge of the Changjiang diluted water plume of the East China Sea M. Sato et al. 10.1016/j.csr.2022.104646
9. Distribution and flux of dissolved iron in the peatland-draining rivers and estuaries of Sarawak, Malaysian Borneo X. Zhang et al. 10.5194/bg-17-1805-2020
10. Windsock behavior: climatic control on iron biogeochemistry in tropical mangroves T. Ferreira et al. 10.1007/s10533-021-00858-9
11. Iron and manganese speciation and cycling in glacially influenced high-latitude fjord sediments (West Spitsbergen, Svalbard): Evidence for a benthic recycling-transport mechanism L. Wehrmann et al. 10.1016/j.gca.2014.06.007
12. Distribution of dissolved iron in the Pearl River (Zhujiang) Estuary and the northern continental slope of the South China Sea R. Zhang et al. 10.1016/j.dsr2.2018.12.006
13. From the peat bog to the estuarine mixing zone: Common features and variances in riverine dissolved organic matter determined by non-targeted analysis A. Rathgeb et al. 10.1016/j.marchem.2017.06.012
14. Evaluation of physicochemical and heavy metals characteristics in surface water under anthropogenic activities using multivariate statistical methods, Garra River, Ganges Basin, India M. Ali Khan & J. Wen 10.4491/eer.2020.280
15. Determination of size-dependent metal distribution in dissolved organic matter by SEC-UV/VIS-ICP-MS with special focus on changes in seawater A. Rathgeb et al. 10.1002/elps.201500538
16. Complexation and reduction of iron by phenolic substances: Implications for transport of dissolved Fe from peatlands to aquatic ecosystems and global iron cycling X. Wan et al. 10.1016/j.chemgeo.2018.09.019
17. Seasonal Variations of Dissolved Iron Concentration in Active Layer and Rivers in Permafrost Areas, Russian Far East Y. Tashiro et al. 10.3390/w12092579
18. Particles as carriers of matter in the aquatic environment: Challenges and ways ahead for transdisciplinary research A. Thit et al. 10.1016/j.scitotenv.2022.155831
19. Pollution of River Mahaweli and farmlands under irrigation by cadmium from agricultural inputs leading to a chronic renal failure epidemic among farmers in NCP, Sri Lanka J. Bandara et al. 10.1007/s10653-010-9344-4
20. Bacterially mediated iron cycling and associated biogeochemical processes in a subtropical shallow coastal aquifer: implications for groundwater quality C. Lin et al. 10.1007/s10750-012-1184-z
21. Hydromorphic to subaqueous soils transitions in the central Grado lagoon (Northern Adriatic Sea, Italy) L. Vittori Antisari et al. 10.1016/j.ecss.2016.02.004
22. Geochemical interactions between iron and phenolics originated from peatland in Hani, China: implications for effective transport of iron from terrestrial systems to marine Y. Wu et al. 10.1007/s12665-015-5189-6
23. Deciphering the source of banded iron formations in the North China Craton C. Wang et al. 10.1016/j.precamres.2024.107298
24. Heavy metals in the midstream of the Ganges River: spatio-temporal trends in a seasonally dry tropical region (India) A. Singh & J. Pandey 10.1080/02508060.2014.921851
25. River-derived humic substances as iron chelators in seawater R. Krachler et al. 10.1016/j.marchem.2015.05.009
26. Fate of colloids during estuarine mixing in the Arctic O. Pokrovsky et al. 10.5194/os-10-107-2014
27. The role of peat decomposition stage on iron solubility and distribution in tidal swamps A. Fahmi et al. 10.1088/1755-1315/648/1/012174
28. Variable relationships between the hydrophobic fraction of dissolved organic matter and metals in Scottish freshwater before the estuarine mixing zone H. Sato et al. 10.1007/s10201-018-0569-8
29. Selective associations of organic matter components with ferrihydrite: Implications for Fe-organic matter preservation in tidal flat wetlands J. Wei et al. 10.1016/j.geoderma.2023.116574
30. Northern High-Latitude Organic Soils As a Vital Source of River-Borne Dissolved Iron to the Ocean R. Krachler & R. Krachler 10.1021/acs.est.1c01439
31. Synthetic iron complexes as models for natural iron-humic compounds: Synthesis, characterization and algal growth experiments E. Orlowska et al. 10.1016/j.scitotenv.2016.10.109
32. Iron and silicon isotope behaviour accompanying weathering in Icelandic soils, and the implications for iron export from peatlands S. Opfergelt et al. 10.1016/j.gca.2017.08.033
33. Distinguishing the influence of sediments, the Congo River, and water-mass mixing on the distribution of iron and its isotopes in the Southeast Atlantic Ocean H. Hunt et al. 10.1016/j.marchem.2022.104181
34. Salinity Effects on Iron Speciation in Boreal River Waters S. Herzog et al. 10.1021/acs.est.7b02309
35. Export of dissolved iron from river catchments in northeast Japan Y. Endo et al. 10.1007/s11355-020-00435-6
36. Natural iron fertilization of the coastal ocean by “blackwater rivers” R. Krachler et al. 10.1016/j.scitotenv.2018.11.423
37. Transport and reaction of iron and iron stable isotopes in glacial meltwaters on Svalbard near Kongsfjorden: From rivers to estuary to ocean R. Zhang et al. 10.1016/j.epsl.2015.05.031
38. Global and regional variations in tropical marine environments of Gondwana as revealed by a multi-stable isotope study, Middle Triassic (Anisian), Israel, Levant Basin A. Schneider-Mor et al. 10.1016/j.palaeo.2018.07.005
39. Sphagnum-dominated bog systems are highly effective yet variable sources of bio-available iron to marine waters R. Krachler et al. 10.1016/j.scitotenv.2016.03.012
40. Capacity of humic substances to complex with iron at different salinities in the Yangtze River estuary and East China Sea R. Yang et al. 10.1038/s41598-017-01533-6
41. Using FLOWFFF and HPSEC to determine trace metal–colloid associations in wetland runoff E. Neubauer et al. 10.1016/j.watres.2013.02.030
42. Ocean Acidification Effect on the Iron-Gallic Acid Redox Interaction in Seawater N. Pérez-Almeida et al. 10.3389/fmars.2022.837363
43. The Chemical Speciation of Fe(III) in Freshwaters S. Lofts et al. 10.1007/s10498-008-9040-5
44. β-O-4 type dilignol compounds and their iron complexes for modeling of iron binding to humic acids: synthesis, characterization, electrochemical studies and algal growth experiments E. Orlowska et al. 10.1039/C7NJ02328F
45. Inputs of glacially derived dissolved and colloidal iron to the coastal ocean and implications for primary productivity P. Statham et al. 10.1029/2007GB003106
46. The Importance of Dynamic Iron Deposition in Projecting Climate Change Impacts on Pacific Ocean Biogeochemistry E. Drenkard et al. 10.1029/2022GL102058
47. Characteristics and behavior of dissolved organic matter in the Kumaki River, Noto Peninsula, Japan T. Suzuki et al. 10.1007/s10201-014-0441-4
48. Climate-controlled variability of iron deposition in the Central Arctic Ocean (southern Mendeleev Ridge) over the last 130,000years C. März et al. 10.1016/j.chemgeo.2012.08.015
49. Review and synthesis: iron input, biogeochemistry, and ecological approaches in seawater C. Longhini et al. 10.1139/er-2018-0020
50. Effect of Fe (III) on Pseudokirchneriella subcapitata at circumneutral pH in standard laboratory tests is explained by nutrient sequestration J. Arbildua et al. 10.1002/etc.3609
51. Peculiarities of the Dynamics of Some Elements of Hydrochemical Regime in Small Water Bodies of Urban Territories: Coexisting Forms of Metals V. Zhezherya & P. Linnik 10.1615/HydrobJ.v58.i5.80
52. Towards the identification of humic ligands associated with iron transport through a salinity gradient K. Heerah & H. Reader 10.1038/s41598-022-19618-2
53. Organic iron complexes enhance iron transport capacity along estuarine salinity gradients of Baltic estuaries S. Herzog et al. 10.5194/bg-17-331-2020
54. Rain-fed streams dilute inorganic nutrients but subsidise organic-matter-associated nutrients in coastal waters of the northeast Pacific Ocean K. St. Pierre et al. 10.5194/bg-18-3029-2021
55. Relevance of peat-draining rivers for the riverine input of dissolved iron into the ocean R. Krachler et al. 10.1016/j.scitotenv.2010.02.018
56. Iron biogeochemistry across marine systems – progress from the past decade E. Breitbarth et al. 10.5194/bg-7-1075-2010
57. Behavior of Cu, Zn, Pb, Ni and Mn during mixing of freshwater with the Caspian Sea water A. Karbassi et al. 10.1016/j.desal.2007.06.035
58. Iron uptake kinetics by coastal micro- and macro-algae in relation to riverine and coastal organic matter M. Natsuike et al. 10.1016/j.ecss.2019.106580
59. The distribution of dissolved Fe and Al in the upper waters of the Eastern Equatorial Pacific L. Kaupp et al. 10.1016/j.dsr2.2010.08.009
60. Comparison of controlling mechanisms of flocculation processes in estuaries A. Biati & A. Karbassi 10.1007/BF03326182
61. Chemical Speciation and Bioavailability of Iron in Natural Waters - Linkage of Forest, River and Sea in View of Dynamics of Iron and Organic Matter M. NATSUIKE et al. 10.2965/jswe.39.197
62. Distinct drivers of two size fractions of operationally dissolved iron in a temperate river L. Logozzo et al. 10.1002/lno.12338
63. Flocculation of heavy metals during mixing of freshwater with Caspian Sea water A. Karbassi et al. 10.1007/s00254-007-0786-7