The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami
The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environm...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yamamoto, Mitsuo [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2020transfer abstract |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction - Aschauer, E. ELSEVIER, 2019, London |
|---|---|
| Übergeordnetes Werk: |
volume:233 ; year:2020 ; day:5 ; month:02 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.ecss.2019.106408 |
|---|
| Katalog-ID: |
ELV049212001 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV049212001 | ||
| 003 | DE-627 | ||
| 005 | 20230626023754.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 200518s2020 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.ecss.2019.106408 |2 doi | |
| 028 | 5 | 2 | |a /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica |
| 035 | |a (DE-627)ELV049212001 | ||
| 035 | |a (ELSEVIER)S0272-7714(18)31094-1 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 620 |a 670 |q VZ |
| 084 | |a 52.78 |2 bkl | ||
| 084 | |a 51.20 |2 bkl | ||
| 100 | 1 | |a Yamamoto, Mitsuo |e verfasserin |4 aut | |
| 245 | 1 | 4 | |a The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| 264 | 1 | |c 2020transfer abstract | |
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. | ||
| 520 | |a The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. | ||
| 650 | 7 | |a Kesennuma Bay |2 Elsevier | |
| 650 | 7 | |a Water quality environment |2 Elsevier | |
| 650 | 7 | |a Coastal area |2 Elsevier | |
| 650 | 7 | |a Fresh water |2 Elsevier | |
| 650 | 7 | |a Iron dynamics |2 Elsevier | |
| 650 | 7 | |a Tsunami |2 Elsevier | |
| 700 | 1 | |a Liu, Dan |4 oth | |
| 700 | 1 | |a Fukushima, Keitaro |4 oth | |
| 700 | 1 | |a Yokoyama, Katsuhide |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Academic Press |a Aschauer, E. ELSEVIER |t Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |d 2019 |g London |w (DE-627)ELV001620800 |
| 773 | 1 | 8 | |g volume:233 |g year:2020 |g day:5 |g month:02 |g pages:0 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.ecss.2019.106408 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 936 | b | k | |a 52.78 |j Oberflächentechnik |j Wärmebehandlung |q VZ |
| 936 | b | k | |a 51.20 |j Werkstoffoberflächeneigenschaften |q VZ |
| 951 | |a AR | ||
| 952 | |d 233 |j 2020 |b 5 |c 0205 |h 0 | ||
| author_variant |
m y my |
|---|---|
| matchkey_str |
yamamotomitsuoliudanfukushimakeitaroyoko:2020----:hifunefrswtrrmersrasucsnhcnetainoioiksnu |
| hierarchy_sort_str |
2020transfer abstract |
| bklnumber |
52.78 51.20 |
| publishDate |
2020 |
| allfields |
10.1016/j.ecss.2019.106408 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica (DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 DE-627 ger DE-627 rakwb eng 620 670 VZ 52.78 bkl 51.20 bkl Yamamoto, Mitsuo verfasserin aut The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier Liu, Dan oth Fukushima, Keitaro oth Yokoyama, Katsuhide oth Enthalten in Academic Press Aschauer, E. ELSEVIER Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction 2019 London (DE-627)ELV001620800 volume:233 year:2020 day:5 month:02 pages:0 https://doi.org/10.1016/j.ecss.2019.106408 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.78 Oberflächentechnik Wärmebehandlung VZ 51.20 Werkstoffoberflächeneigenschaften VZ AR 233 2020 5 0205 0 |
| spelling |
10.1016/j.ecss.2019.106408 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica (DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 DE-627 ger DE-627 rakwb eng 620 670 VZ 52.78 bkl 51.20 bkl Yamamoto, Mitsuo verfasserin aut The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier Liu, Dan oth Fukushima, Keitaro oth Yokoyama, Katsuhide oth Enthalten in Academic Press Aschauer, E. ELSEVIER Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction 2019 London (DE-627)ELV001620800 volume:233 year:2020 day:5 month:02 pages:0 https://doi.org/10.1016/j.ecss.2019.106408 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.78 Oberflächentechnik Wärmebehandlung VZ 51.20 Werkstoffoberflächeneigenschaften VZ AR 233 2020 5 0205 0 |
| allfields_unstemmed |
10.1016/j.ecss.2019.106408 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica (DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 DE-627 ger DE-627 rakwb eng 620 670 VZ 52.78 bkl 51.20 bkl Yamamoto, Mitsuo verfasserin aut The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier Liu, Dan oth Fukushima, Keitaro oth Yokoyama, Katsuhide oth Enthalten in Academic Press Aschauer, E. ELSEVIER Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction 2019 London (DE-627)ELV001620800 volume:233 year:2020 day:5 month:02 pages:0 https://doi.org/10.1016/j.ecss.2019.106408 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.78 Oberflächentechnik Wärmebehandlung VZ 51.20 Werkstoffoberflächeneigenschaften VZ AR 233 2020 5 0205 0 |
| allfieldsGer |
10.1016/j.ecss.2019.106408 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica (DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 DE-627 ger DE-627 rakwb eng 620 670 VZ 52.78 bkl 51.20 bkl Yamamoto, Mitsuo verfasserin aut The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier Liu, Dan oth Fukushima, Keitaro oth Yokoyama, Katsuhide oth Enthalten in Academic Press Aschauer, E. ELSEVIER Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction 2019 London (DE-627)ELV001620800 volume:233 year:2020 day:5 month:02 pages:0 https://doi.org/10.1016/j.ecss.2019.106408 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.78 Oberflächentechnik Wärmebehandlung VZ 51.20 Werkstoffoberflächeneigenschaften VZ AR 233 2020 5 0205 0 |
| allfieldsSound |
10.1016/j.ecss.2019.106408 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica (DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 DE-627 ger DE-627 rakwb eng 620 670 VZ 52.78 bkl 51.20 bkl Yamamoto, Mitsuo verfasserin aut The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami 2020transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier Liu, Dan oth Fukushima, Keitaro oth Yokoyama, Katsuhide oth Enthalten in Academic Press Aschauer, E. ELSEVIER Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction 2019 London (DE-627)ELV001620800 volume:233 year:2020 day:5 month:02 pages:0 https://doi.org/10.1016/j.ecss.2019.106408 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 52.78 Oberflächentechnik Wärmebehandlung VZ 51.20 Werkstoffoberflächeneigenschaften VZ AR 233 2020 5 0205 0 |
| language |
English |
| source |
Enthalten in Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction London volume:233 year:2020 day:5 month:02 pages:0 |
| sourceStr |
Enthalten in Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction London volume:233 year:2020 day:5 month:02 pages:0 |
| format_phy_str_mv |
Article |
| bklname |
Oberflächentechnik Wärmebehandlung Werkstoffoberflächeneigenschaften |
| institution |
findex.gbv.de |
| topic_facet |
Kesennuma Bay Water quality environment Coastal area Fresh water Iron dynamics Tsunami |
| dewey-raw |
620 |
| isfreeaccess_bool |
false |
| container_title |
Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |
| authorswithroles_txt_mv |
Yamamoto, Mitsuo @@aut@@ Liu, Dan @@oth@@ Fukushima, Keitaro @@oth@@ Yokoyama, Katsuhide @@oth@@ |
| publishDateDaySort_date |
2020-01-05T00:00:00Z |
| hierarchy_top_id |
ELV001620800 |
| dewey-sort |
3620 |
| id |
ELV049212001 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV049212001</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626023754.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">200518s2020 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.ecss.2019.106408</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV049212001</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0272-7714(18)31094-1</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">620</subfield><subfield code="a">670</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.78</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">51.20</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Yamamoto, Mitsuo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Kesennuma Bay</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Water quality environment</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Coastal area</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Fresh water</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Iron dynamics</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Tsunami</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Dan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fukushima, Keitaro</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yokoyama, Katsuhide</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Academic Press</subfield><subfield code="a">Aschauer, E. ELSEVIER</subfield><subfield code="t">Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction</subfield><subfield code="d">2019</subfield><subfield code="g">London</subfield><subfield code="w">(DE-627)ELV001620800</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:233</subfield><subfield code="g">year:2020</subfield><subfield code="g">day:5</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.ecss.2019.106408</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.78</subfield><subfield code="j">Oberflächentechnik</subfield><subfield code="j">Wärmebehandlung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">51.20</subfield><subfield code="j">Werkstoffoberflächeneigenschaften</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">233</subfield><subfield code="j">2020</subfield><subfield code="b">5</subfield><subfield code="c">0205</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| author |
Yamamoto, Mitsuo |
| spellingShingle |
Yamamoto, Mitsuo ddc 620 bkl 52.78 bkl 51.20 Elsevier Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| authorStr |
Yamamoto, Mitsuo |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV001620800 |
| format |
electronic Article |
| dewey-ones |
620 - Engineering & allied operations 670 - Manufacturing |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
620 670 VZ 52.78 bkl 51.20 bkl The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami Elsevier |
| topic |
ddc 620 bkl 52.78 bkl 51.20 Elsevier Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami |
| topic_unstemmed |
ddc 620 bkl 52.78 bkl 51.20 Elsevier Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami |
| topic_browse |
ddc 620 bkl 52.78 bkl 51.20 Elsevier Kesennuma Bay Elsevier Water quality environment Elsevier Coastal area Elsevier Fresh water Elsevier Iron dynamics Elsevier Tsunami |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
d l dl k f kf k y ky |
| hierarchy_parent_title |
Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |
| hierarchy_parent_id |
ELV001620800 |
| dewey-tens |
620 - Engineering 670 - Manufacturing |
| hierarchy_top_title |
Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV001620800 |
| title |
The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| ctrlnum |
(DE-627)ELV049212001 (ELSEVIER)S0272-7714(18)31094-1 |
| title_full |
The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| author_sort |
Yamamoto, Mitsuo |
| journal |
Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |
| journalStr |
Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
600 - Technology |
| recordtype |
marc |
| publishDateSort |
2020 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Yamamoto, Mitsuo |
| container_volume |
233 |
| class |
620 670 VZ 52.78 bkl 51.20 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Yamamoto, Mitsuo |
| doi_str_mv |
10.1016/j.ecss.2019.106408 |
| dewey-full |
620 670 |
| title_sort |
influence of freshwater from terrestrial sources on the concentrations of iron in kesennuma bay, japan, after the 2011 tsunami |
| title_auth |
The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| abstract |
The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. |
| abstractGer |
The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. |
| abstract_unstemmed |
The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U |
| title_short |
The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami |
| url |
https://doi.org/10.1016/j.ecss.2019.106408 |
| remote_bool |
true |
| author2 |
Liu, Dan Fukushima, Keitaro Yokoyama, Katsuhide |
| author2Str |
Liu, Dan Fukushima, Keitaro Yokoyama, Katsuhide |
| ppnlink |
ELV001620800 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth |
| doi_str |
10.1016/j.ecss.2019.106408 |
| up_date |
2024-07-06T20:56:49.955Z |
| _version_ |
1803864674094022656 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV049212001</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626023754.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">200518s2020 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.ecss.2019.106408</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000000892.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV049212001</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0272-7714(18)31094-1</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">620</subfield><subfield code="a">670</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">52.78</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">51.20</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Yamamoto, Mitsuo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The influence of freshwater from terrestrial sources on the concentrations of iron in Kesennuma Bay, Japan, after the 2011 tsunami</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2020transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The earthquake and tsunami that took place off the Pacific Coast of Tohoku, Japan, in 2011 caused serious damage to the coastal areas of the Tohoku and Kanto regions. Samples have been collected either monthly or bi-monthly since the tsunami to facilitate an investigation of how the coastal environment in Kesennuma Bay, Miyagi Prefecture, northeastern Japan, was affected by the tsunami. In this study, information about iron (Fe), nitrogen (N), and phosphorus (P) concentrations, and salinity, chlorophyll, and turbidity, was examined to gain insights into the Fe dynamics in the bay. The Fe, nitrate-nitrogen and nitrite-nitrogen (NO2–N + NO3–N), and phosphate (PO4–P) concentrations were monitored from June 2011 to July 2013. The results showed that the Fe concentrations before and after March 2012 follow different patterns, and the Fe concentrations in surface seawater 1 year after the tsunami reflected the influence of freshwater inputs. Various forms of Fe, N, and P were monitored after March 2014. Total Fe was significantly correlated with precipitation (represented by an index) and salinity, especially at the river mouths. Comparison of the N:P:Fe ratios at all the sites from March 2014 to November 2016 showed that Fe was abundant, and the ratios differed between the surface water and bottom water. The present study indicates that Fe in Kesennuma Bay is influenced by factors such as the balance between freshwater inputs and ocean water, and the water depth. Further, freshwater from terrestrial areas was the main influence on the Fe concentrations close to the river mouths.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Kesennuma Bay</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Water quality environment</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Coastal area</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Fresh water</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Iron dynamics</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Tsunami</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Dan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fukushima, Keitaro</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Yokoyama, Katsuhide</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Academic Press</subfield><subfield code="a">Aschauer, E. ELSEVIER</subfield><subfield code="t">Strain and stress analyses on thermally annealed Ti-Al-N/Mo-Si-B multilayer coatings by synchrotron X-ray diffraction</subfield><subfield code="d">2019</subfield><subfield code="g">London</subfield><subfield code="w">(DE-627)ELV001620800</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:233</subfield><subfield code="g">year:2020</subfield><subfield code="g">day:5</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.ecss.2019.106408</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">52.78</subfield><subfield code="j">Oberflächentechnik</subfield><subfield code="j">Wärmebehandlung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">51.20</subfield><subfield code="j">Werkstoffoberflächeneigenschaften</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">233</subfield><subfield code="j">2020</subfield><subfield code="b">5</subfield><subfield code="c">0205</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.4005365 |