Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories
Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help charact...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Varricchione, Jeffrey T. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Anmerkung: |
© Eawag 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Aquatic sciences - Basel : Springer, 1920, 67(2005), 4 vom: 26. Okt., Seite 434-453 |
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| Übergeordnetes Werk: |
volume:67 ; year:2005 ; number:4 ; day:26 ; month:10 ; pages:434-453 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00027-005-0784-3 |
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| Katalog-ID: |
SPR000288659 |
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| 100 | 1 | |a Varricchione, Jeffrey T. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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| 520 | |a Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. | ||
| 700 | 1 | |a Thomas, Steven A. |4 aut | |
| 700 | 1 | |a Minshall, G. Wayne |4 aut | |
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10.1007/s00027-005-0784-3 doi (DE-627)SPR000288659 (SPR)s00027-005-0784-3-e DE-627 ger DE-627 rakwb eng Varricchione, Jeffrey T. verfasserin aut Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. Thomas, Steven A. aut Minshall, G. Wayne aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 26. Okt., Seite 434-453 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:26 month:10 pages:434-453 https://dx.doi.org/10.1007/s00027-005-0784-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 26 10 434-453 |
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10.1007/s00027-005-0784-3 doi (DE-627)SPR000288659 (SPR)s00027-005-0784-3-e DE-627 ger DE-627 rakwb eng Varricchione, Jeffrey T. verfasserin aut Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. Thomas, Steven A. aut Minshall, G. Wayne aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 26. Okt., Seite 434-453 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:26 month:10 pages:434-453 https://dx.doi.org/10.1007/s00027-005-0784-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 26 10 434-453 |
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10.1007/s00027-005-0784-3 doi (DE-627)SPR000288659 (SPR)s00027-005-0784-3-e DE-627 ger DE-627 rakwb eng Varricchione, Jeffrey T. verfasserin aut Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. Thomas, Steven A. aut Minshall, G. Wayne aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 26. Okt., Seite 434-453 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:26 month:10 pages:434-453 https://dx.doi.org/10.1007/s00027-005-0784-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 26 10 434-453 |
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10.1007/s00027-005-0784-3 doi (DE-627)SPR000288659 (SPR)s00027-005-0784-3-e DE-627 ger DE-627 rakwb eng Varricchione, Jeffrey T. verfasserin aut Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. Thomas, Steven A. aut Minshall, G. Wayne aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 26. Okt., Seite 434-453 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:26 month:10 pages:434-453 https://dx.doi.org/10.1007/s00027-005-0784-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 26 10 434-453 |
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10.1007/s00027-005-0784-3 doi (DE-627)SPR000288659 (SPR)s00027-005-0784-3-e DE-627 ger DE-627 rakwb eng Varricchione, Jeffrey T. verfasserin aut Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories 2005 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Eawag 2005 Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. Thomas, Steven A. aut Minshall, G. Wayne aut Enthalten in Aquatic sciences Basel : Springer, 1920 67(2005), 4 vom: 26. Okt., Seite 434-453 (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:67 year:2005 number:4 day:26 month:10 pages:434-453 https://dx.doi.org/10.1007/s00027-005-0784-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 67 2005 4 26 10 434-453 |
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Varricchione, Jeffrey T. @@aut@@ Thomas, Steven A. @@aut@@ Minshall, G. Wayne @@aut@@ |
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We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. 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Varricchione, Jeffrey T. |
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Varricchione, Jeffrey T. Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
| abstract |
Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. © Eawag 2005 |
| abstractGer |
Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. © Eawag 2005 |
| abstract_unstemmed |
Abstract. We investigated the vertical, lateral, and seasonal distribution of hyporheic invertebrates at five stream sites in Idaho (unglaciated areas) and seven sites in Montana (glaciated areas), U.S.A. Conservative tracer releases and transient storage zone analyses were conducted to help characterize study sites. Hyporheic invertebrates and substrate were sampled by freeze-coring with electro-shocking, and mini-piezometers were used to measure other hyporheic conditions, including vertical hydraulic gradient (VHG). Wells were installed at some Montana sites (range: 5–175 m lateral to the channel) and shallow pits were excavated at some Idaho sites (5 m lateral to the channel) to sample hyporheic invertebrates in these saturated sediments regions. Environmental conditions varied widely among sites and between surface and hyporheic zones at each site, and most hyporheic habitat measures differed significantly between glaciated and unglaciated streams. In-channel invertebrate density and taxa richness generally decreased with increasing depth into the streambed, regardless of geographic location, history of glaciation, or season. Although hyporheic invertebrate mean density and (to a lesser extent) richness values at individual depth layers (e.g., 10–20 cm, 20–30 cm) mostly were greater in the glaciated region than the unglaciated region, density and richness between 10–50 cm did not differ significantly between the two regions. Hydrologic variables (VHG; $ A_{S} $/A [ratio of transientstorage- zone- to channel- cross-sectional areas]; $ TT_{S} $ [turnover time of storage]; and $ R_{h} $ [hydraulic retention factor]) provided the best explanation for differences in sub-channel invertebrate density and richness patterns. The observation that benthic invertebrates occurred in freeze-core, well, and open-pit samples contributes to existing evidence that aquatic invertebrates occupy habitats that extend considerable distances from the active channel. © Eawag 2005 |
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4 |
| title_short |
Vertical and seasonal distribution of hyporheic invertebrates in streams with different glacial histories |
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https://dx.doi.org/10.1007/s00027-005-0784-3 |
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Thomas, Steven A. Minshall, G. Wayne |
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10.1007/s00027-005-0784-3 |
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2024-07-03T15:07:29.660Z |
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| score |
7.401698 |