Surface charging of thick porous water ice layers relevant for ion sputtering experiments
We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfac...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Galli, A. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016transfer abstract |
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| Schlagwörter: |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS - Mekaroonkamol, Parit ELSEVIER, 2023, Kidlington [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:126 ; year:2016 ; pages:63-71 ; extent:9 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.pss.2016.03.016 |
|---|
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ELV024912948 |
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| 520 | |a We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. | ||
| 520 | |a We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. | ||
| 650 | 7 | |a Jupiter satellites |2 Elsevier | |
| 650 | 7 | |a Surface charging |2 Elsevier | |
| 650 | 7 | |a Experimental techniques |2 Elsevier | |
| 650 | 7 | |a Ices |2 Elsevier | |
| 650 | 7 | |a Sputtering |2 Elsevier | |
| 700 | 1 | |a Vorburger, A. |4 oth | |
| 700 | 1 | |a Pommerol, A. |4 oth | |
| 700 | 1 | |a Wurz, P. |4 oth | |
| 700 | 1 | |a Jost, B. |4 oth | |
| 700 | 1 | |a Poch, O. |4 oth | |
| 700 | 1 | |a Brouet, Y. |4 oth | |
| 700 | 1 | |a Tulej, M. |4 oth | |
| 700 | 1 | |a Thomas, N. |4 oth | |
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10.1016/j.pss.2016.03.016 doi GBVA2016023000001.pica (DE-627)ELV024912948 (ELSEVIER)S0032-0633(16)30014-9 DE-627 ger DE-627 rakwb eng 620 620 DE-600 610 VZ 44.87 bkl Galli, A. verfasserin aut Surface charging of thick porous water ice layers relevant for ion sputtering experiments 2016transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. Jupiter satellites Elsevier Surface charging Elsevier Experimental techniques Elsevier Ices Elsevier Sputtering Elsevier Vorburger, A. oth Pommerol, A. oth Wurz, P. oth Jost, B. oth Poch, O. oth Brouet, Y. oth Tulej, M. oth Thomas, N. oth Enthalten in Elsevier Science Mekaroonkamol, Parit ELSEVIER ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS 2023 Kidlington [u.a.] (DE-627)ELV010254102 volume:126 year:2016 pages:63-71 extent:9 https://doi.org/10.1016/j.pss.2016.03.016 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_66 GBV_ILN_91 GBV_ILN_165 GBV_ILN_234 44.87 Gastroenterologie VZ AR 126 2016 63-71 9 045F 620 |
| spelling |
10.1016/j.pss.2016.03.016 doi GBVA2016023000001.pica (DE-627)ELV024912948 (ELSEVIER)S0032-0633(16)30014-9 DE-627 ger DE-627 rakwb eng 620 620 DE-600 610 VZ 44.87 bkl Galli, A. verfasserin aut Surface charging of thick porous water ice layers relevant for ion sputtering experiments 2016transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. Jupiter satellites Elsevier Surface charging Elsevier Experimental techniques Elsevier Ices Elsevier Sputtering Elsevier Vorburger, A. oth Pommerol, A. oth Wurz, P. oth Jost, B. oth Poch, O. oth Brouet, Y. oth Tulej, M. oth Thomas, N. oth Enthalten in Elsevier Science Mekaroonkamol, Parit ELSEVIER ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS 2023 Kidlington [u.a.] (DE-627)ELV010254102 volume:126 year:2016 pages:63-71 extent:9 https://doi.org/10.1016/j.pss.2016.03.016 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_66 GBV_ILN_91 GBV_ILN_165 GBV_ILN_234 44.87 Gastroenterologie VZ AR 126 2016 63-71 9 045F 620 |
| allfields_unstemmed |
10.1016/j.pss.2016.03.016 doi GBVA2016023000001.pica (DE-627)ELV024912948 (ELSEVIER)S0032-0633(16)30014-9 DE-627 ger DE-627 rakwb eng 620 620 DE-600 610 VZ 44.87 bkl Galli, A. verfasserin aut Surface charging of thick porous water ice layers relevant for ion sputtering experiments 2016transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. Jupiter satellites Elsevier Surface charging Elsevier Experimental techniques Elsevier Ices Elsevier Sputtering Elsevier Vorburger, A. oth Pommerol, A. oth Wurz, P. oth Jost, B. oth Poch, O. oth Brouet, Y. oth Tulej, M. oth Thomas, N. oth Enthalten in Elsevier Science Mekaroonkamol, Parit ELSEVIER ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS 2023 Kidlington [u.a.] (DE-627)ELV010254102 volume:126 year:2016 pages:63-71 extent:9 https://doi.org/10.1016/j.pss.2016.03.016 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_66 GBV_ILN_91 GBV_ILN_165 GBV_ILN_234 44.87 Gastroenterologie VZ AR 126 2016 63-71 9 045F 620 |
| allfieldsGer |
10.1016/j.pss.2016.03.016 doi GBVA2016023000001.pica (DE-627)ELV024912948 (ELSEVIER)S0032-0633(16)30014-9 DE-627 ger DE-627 rakwb eng 620 620 DE-600 610 VZ 44.87 bkl Galli, A. verfasserin aut Surface charging of thick porous water ice layers relevant for ion sputtering experiments 2016transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. Jupiter satellites Elsevier Surface charging Elsevier Experimental techniques Elsevier Ices Elsevier Sputtering Elsevier Vorburger, A. oth Pommerol, A. oth Wurz, P. oth Jost, B. oth Poch, O. oth Brouet, Y. oth Tulej, M. oth Thomas, N. oth Enthalten in Elsevier Science Mekaroonkamol, Parit ELSEVIER ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS 2023 Kidlington [u.a.] (DE-627)ELV010254102 volume:126 year:2016 pages:63-71 extent:9 https://doi.org/10.1016/j.pss.2016.03.016 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_66 GBV_ILN_91 GBV_ILN_165 GBV_ILN_234 44.87 Gastroenterologie VZ AR 126 2016 63-71 9 045F 620 |
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10.1016/j.pss.2016.03.016 doi GBVA2016023000001.pica (DE-627)ELV024912948 (ELSEVIER)S0032-0633(16)30014-9 DE-627 ger DE-627 rakwb eng 620 620 DE-600 610 VZ 44.87 bkl Galli, A. verfasserin aut Surface charging of thick porous water ice layers relevant for ion sputtering experiments 2016transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. Jupiter satellites Elsevier Surface charging Elsevier Experimental techniques Elsevier Ices Elsevier Sputtering Elsevier Vorburger, A. oth Pommerol, A. oth Wurz, P. oth Jost, B. oth Poch, O. oth Brouet, Y. oth Tulej, M. oth Thomas, N. oth Enthalten in Elsevier Science Mekaroonkamol, Parit ELSEVIER ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS 2023 Kidlington [u.a.] (DE-627)ELV010254102 volume:126 year:2016 pages:63-71 extent:9 https://doi.org/10.1016/j.pss.2016.03.016 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_66 GBV_ILN_91 GBV_ILN_165 GBV_ILN_234 44.87 Gastroenterologie VZ AR 126 2016 63-71 9 045F 620 |
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English |
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Enthalten in ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS Kidlington [u.a.] volume:126 year:2016 pages:63-71 extent:9 |
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Enthalten in ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS Kidlington [u.a.] volume:126 year:2016 pages:63-71 extent:9 |
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ENDOLOOP-ASSISTED TRANSORAL OUTLET REDUCTION: A PILOT CASE-CONTROL STUDY OF A NEW THERAPEUTIC INTERVENTION FOR WEIGHT REGAIN AFTER ROUX-EN-Y GASTRIC BYPASS |
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surface charging of thick porous water ice layers relevant for ion sputtering experiments |
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Surface charging of thick porous water ice layers relevant for ion sputtering experiments |
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We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. |
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We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. |
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We use a laboratory facility to study the sputtering properties of centimeter-thick porous water ice subjected to the bombardment of ions and electrons to better understand the formation of exospheres of the icy moons of Jupiter. Our ice samples are as similar as possible to the expected moon surfaces but surface charging of the samples during ion irradiation may distort the experimental results. We therefore monitor the time scales for charging and discharging of the samples when subjected to a beam of ions. These experiments allow us to derive an electric conductivity of deep porous ice layers. The results imply that electron irradiation and sputtering play a non-negligible role for certain plasma conditions at the icy moons of Jupiter. The observed ion sputtering yields from our ice samples are similar to previous experiments where compact ice films were sputtered off a micro-balance. |
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Surface charging of thick porous water ice layers relevant for ion sputtering experiments |
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