title: Long-term changes in streamflow following logging in western Oregon and associated fisheries implications

authors: Hicks, Brendan J.

subjects: streamflow

abstract: The long-term effect of logging on low summer streamflow was investigated with a data set of 36 years. Hydrologic records were analyzed for the period 1953 and 1988 from Watershed (WS) 1 (clear-cut logged and burned), WS 2 (unlogged control), and WS 3 (25 percent patch-cut logged and burned) in the H. J. Andrews Experimental Forest, western Cascade Range, Oregon. These records spanned 9–10 years before logging, and 21–25 years after logging and burning. Streamfiows in August were the lowest of any month, and were unaffected by occasional heavy rain that occurred at the beginning of summer. August streamfiows increased in WS 1 compared to WS 2 by 159 percent following logging in WS 1, but this increase lasted for only eight years following the start of logging in 1962. Water yield in August for 1970–1988 observed from WS 1 was 25 percent less than predicted from the control (WS 2, ANOVA, p=0.032).
Water yield in August increased by 59 percent after 25 percent of the area of WS 3 was patch-cut logged and burned in 1963. In contrast to WS 1, however, water yields from WS 3 in August were consistently greater than predicted for 16 years following the start of logging, through to 1978. For the 10 years, 1979–1988, water yield observed in August from WS 3 was not different than predicted from the control (WS 2, ANOVA, p-0.175).
The contrasting responses of WS 1 and 3 to logging are thought to be the result of differences in riparian vegetation caused by different geomorphic conditions. A relatively wide valley floor in WS 1 allowed the development of hardwoods in the riparian zone following logging, but the narrow valley of WS 3 and limited sediment deposits prevented establishment of riparian hardwoods.
Low streamflows during summer have implications for salmonid survival. Reduced streamflow reduces the amount of rearing habitat, thus increasing competition. Combined with high water temperatures, reduced streamflow can lead directly to salmonid mortality by driving salmonids from riffles and glides, and trapping them in drying pools. Low streamflow also increases oxygen depletion caused by leaves from riparian red alders.

text: Long-term changes in streamflow following logging in western Oregon and associated fisheries implications The long-term effect of logging on low summer streamflow was investigated with a data set of 36 years. Hydrologic records were analyzed for the period 1953 and 1988 from Watershed (WS) 1 (clear-cut logged and burned), WS 2 (unlogged control), and WS 3 (25 percent patch-cut logged and burned) in the H. J. Andrews Experimental Forest, western Cascade Range, Oregon. These records spanned 9–10 years before logging, and 21–25 years after logging and burning. Streamfiows in August were the lowest of any month, and were unaffected by occasional heavy rain that occurred at the beginning of summer. August streamfiows increased in WS 1 compared to WS 2 by 159 percent following logging in WS 1, but this increase lasted for only eight years following the start of logging in 1962. Water yield in August for 1970–1988 observed from WS 1 was 25 percent less than predicted from the control (WS 2, ANOVA, p=0.032).
Water yield in August increased by 59 percent after 25 percent of the area of WS 3 was patch-cut logged and burned in 1963. In contrast to WS 1, however, water yields from WS 3 in August were consistently greater than predicted for 16 years following the start of logging, through to 1978. For the 10 years, 1979–1988, water yield observed in August from WS 3 was not different than predicted from the control (WS 2, ANOVA, p-0.175).
The contrasting responses of WS 1 and 3 to logging are thought to be the result of differences in riparian vegetation caused by different geomorphic conditions. A relatively wide valley floor in WS 1 allowed the development of hardwoods in the riparian zone following logging, but the narrow valley of WS 3 and limited sediment deposits prevented establishment of riparian hardwoods.
Low streamflows during summer have implications for salmonid survival. Reduced streamflow reduces the amount of rearing habitat, thus increasing competition. Combined with high water temperatures, reduced streamflow can lead directly to salmonid mortality by driving salmonids from riffles and glides, and trapping them in drying pools. Low streamflow also increases oxygen depletion caused by leaves from riparian red alders.

year: 1991

title: Book Review: To Circumjack MacDiarmid: The Poetry and Prose of Hugh MacDiarmid by W. N. Herbert

authors: Riach, Alan

subjects: book review

abstract: This article reviews the book: “To Circumjack MacDiarmid: The Poetry and Prose of Hugh MacDiarmid”, by W. N. Herbert.

text: Book Review: To Circumjack MacDiarmid: The Poetry and Prose of Hugh MacDiarmid by W. N. Herbert This article reviews the book: “To Circumjack MacDiarmid: The Poetry and Prose of Hugh MacDiarmid”, by W. N. Herbert.

year: 1995

title: Ki te kapu o taku ringa - In the palm of my hand

authors: Hill, Rodrigo

subjects: Mātauranga Māori

abstract: This publication accompanies the launching of our exhibition 'Ki te Kapu o Taku Ringa - In the Palm of My Hand' at the Ōtorohanga Museum in June 2024.
The title is taken from a line of King Tāwhiao's song-poem 'Maioha mō Waikato'. Ejected from their homelands he and his Waikato brethren took refuge with their Maniapoto relations in Te Nehenehenui; parts of which are mentioned in the song-poem. Teh 'maioha' was composed expressing King Tāwhiao's love for his homelands, and his solastagic holding fast to those lands '...in the palm of his hand.'

text: Ki te kapu o taku ringa - In the palm of my hand This publication accompanies the launching of our exhibition 'Ki te Kapu o Taku Ringa - In the Palm of My Hand' at the Ōtorohanga Museum in June 2024.
The title is taken from a line of King Tāwhiao's song-poem 'Maioha mō Waikato'. Ejected from their homelands he and his Waikato brethren took refuge with their Maniapoto relations in Te Nehenehenui; parts of which are mentioned in the song-poem. Teh 'maioha' was composed expressing King Tāwhiao's love for his homelands, and his solastagic holding fast to those lands '...in the palm of his hand.'

year: 2024