Seismic Lines Are Associated With Enhanced Ground Layer Evapotranspiration in Peatlands.

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Title: Seismic Lines Are Associated With Enhanced Ground Layer Evapotranspiration in Peatlands.
Authors: Bayatvarkeshi, Maryam1 (AUTHOR) mbayatva@uwaterloo.ca, Ketcheson, Scott2 (AUTHOR), Korsah, Percy1 (AUTHOR), Schmidt, Megan1 (AUTHOR), Tabassum, Nazia1 (AUTHOR), Strack, Maria1 (AUTHOR)
Source: Ecohydrology. Sep2025, Vol. 18 Issue 6, p1-17. 17p.
Subject Terms: *Evapotranspiration, *Peatlands, *Anthropogenic effects on nature, *Water balance (Hydrology), *Ecological impact, Water vapor transport
Geographic Terms: Canada, Alberta
Abstract: Evapotranspiration, the combined water loss through both evaporation from the ground surface and transpiration through the vegetation canopy, makes up a substantial portion of the water balance in peatlands in the western boreal region of Canada. Geologic exploration for petroleum resources has created a network of linear clearings, known as seismic lines, that have altered the local hydro‐climatological conditions within the ecosystems that they cross, including peatlands. Accordingly, understanding the interaction between human activities and hydrological fluxes in peatlands is crucial for identifying the processes sensitive to these types of disturbances, especially in a region with a subhumid climate. This study aims to assess the effect of seismic lines on evapotranspiration from the understory at different sites in northern Alberta. Actual evapotranspiration (AET) was measured using weighing lysimeters and chamber techniques, and potential evapotranspiration (PET) was calculated based on the Penman and Priestley–Taylor equation. Understory AET on the seismic lines was 59% and 33% higher than in the adjacent ecosystem, based on lysimeter and chamber measurements, respectively. Furthermore, we also observed that the soil temperature, available photosynthetically active radiation (PAR) and plant community composition were the primary drivers of the AET measured using chambers, while wind speed and PAR controlled the AET measured by lysimeters. We estimated that ground layer PET on the line was 51% higher than off the line. These variations affected the Priestley–Taylor coefficient of evaporability (α) values so that the α value on the seismic line (0.73) was higher than off the line (0.61). Accounting for transpiration from trees, it was determined that the AET from seismic lines exceeds the AET from adjacent areas by 31%. Considering the ubiquitous nature and high spatial density of seismic lines in the boreal region, these changes to a dominant water loss mechanism will have a considerable impact on hydrological fluxes and result in an altered water budget, with potential implications at the watershed scale. [ABSTRACT FROM AUTHOR]
Copyright of Ecohydrology is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Seismic Lines Are Associated With Enhanced Ground Layer Evapotranspiration in Peatlands.
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  Data: <searchLink fieldCode="AR" term="%22Bayatvarkeshi%2C+Maryam%22">Bayatvarkeshi, Maryam</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> mbayatva@uwaterloo.ca</i><br /><searchLink fieldCode="AR" term="%22Ketcheson%2C+Scott%22">Ketcheson, Scott</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Korsah%2C+Percy%22">Korsah, Percy</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Schmidt%2C+Megan%22">Schmidt, Megan</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Tabassum%2C+Nazia%22">Tabassum, Nazia</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Strack%2C+Maria%22">Strack, Maria</searchLink><relatesTo>1</relatesTo> (AUTHOR)
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  Data: <searchLink fieldCode="JN" term="%22Ecohydrology%22">Ecohydrology</searchLink>. Sep2025, Vol. 18 Issue 6, p1-17. 17p.
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  Data: *<searchLink fieldCode="DE" term="%22Evapotranspiration%22">Evapotranspiration</searchLink><br />*<searchLink fieldCode="DE" term="%22Peatlands%22">Peatlands</searchLink><br />*<searchLink fieldCode="DE" term="%22Anthropogenic+effects+on+nature%22">Anthropogenic effects on nature</searchLink><br />*<searchLink fieldCode="DE" term="%22Water+balance+%28Hydrology%29%22">Water balance (Hydrology)</searchLink><br />*<searchLink fieldCode="DE" term="%22Ecological+impact%22">Ecological impact</searchLink><br /><searchLink fieldCode="DE" term="%22Water+vapor+transport%22">Water vapor transport</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22Canada%22">Canada</searchLink><br /><searchLink fieldCode="DE" term="%22Alberta%22">Alberta</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: Evapotranspiration, the combined water loss through both evaporation from the ground surface and transpiration through the vegetation canopy, makes up a substantial portion of the water balance in peatlands in the western boreal region of Canada. Geologic exploration for petroleum resources has created a network of linear clearings, known as seismic lines, that have altered the local hydro‐climatological conditions within the ecosystems that they cross, including peatlands. Accordingly, understanding the interaction between human activities and hydrological fluxes in peatlands is crucial for identifying the processes sensitive to these types of disturbances, especially in a region with a subhumid climate. This study aims to assess the effect of seismic lines on evapotranspiration from the understory at different sites in northern Alberta. Actual evapotranspiration (AET) was measured using weighing lysimeters and chamber techniques, and potential evapotranspiration (PET) was calculated based on the Penman and Priestley–Taylor equation. Understory AET on the seismic lines was 59% and 33% higher than in the adjacent ecosystem, based on lysimeter and chamber measurements, respectively. Furthermore, we also observed that the soil temperature, available photosynthetically active radiation (PAR) and plant community composition were the primary drivers of the AET measured using chambers, while wind speed and PAR controlled the AET measured by lysimeters. We estimated that ground layer PET on the line was 51% higher than off the line. These variations affected the Priestley–Taylor coefficient of evaporability (α) values so that the α value on the seismic line (0.73) was higher than off the line (0.61). Accounting for transpiration from trees, it was determined that the AET from seismic lines exceeds the AET from adjacent areas by 31%. Considering the ubiquitous nature and high spatial density of seismic lines in the boreal region, these changes to a dominant water loss mechanism will have a considerable impact on hydrological fluxes and result in an altered water budget, with potential implications at the watershed scale. [ABSTRACT FROM AUTHOR]
– Name: AbstractSuppliedCopyright
  Label:
  Group: Ab
  Data: <i>Copyright of Ecohydrology is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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RecordInfo BibRecord:
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      – Type: doi
        Value: 10.1002/eco.70102
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 17
        StartPage: 1
    Subjects:
      – SubjectFull: Evapotranspiration
        Type: general
      – SubjectFull: Peatlands
        Type: general
      – SubjectFull: Anthropogenic effects on nature
        Type: general
      – SubjectFull: Water balance (Hydrology)
        Type: general
      – SubjectFull: Ecological impact
        Type: general
      – SubjectFull: Water vapor transport
        Type: general
      – SubjectFull: Canada
        Type: general
      – SubjectFull: Alberta
        Type: general
    Titles:
      – TitleFull: Seismic Lines Are Associated With Enhanced Ground Layer Evapotranspiration in Peatlands.
        Type: main
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          Name:
            NameFull: Bayatvarkeshi, Maryam
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            NameFull: Ketcheson, Scott
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            NameFull: Korsah, Percy
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            NameFull: Schmidt, Megan
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            NameFull: Tabassum, Nazia
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            NameFull: Strack, Maria
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          Dates:
            – D: 01
              M: 09
              Text: Sep2025
              Type: published
              Y: 2025
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