The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021

Increased groundwater demand is causing aquifer declines that impact viability of groundwater-dependent ecosystems (GDEs) like springs and phreatophyte communities. To understand which springs and phreatophyte communities may be stressed by groundwater level declines in Oregon and Nevada, we assesse...

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Main Authors: Laurel Saito, Zach Freed, Sarah Byer, Michael Schindel
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-12-01
Series:Frontiers in Environmental Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fenvs.2022.1007114/full
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author Laurel Saito
Zach Freed
Sarah Byer
Michael Schindel
author_facet Laurel Saito
Zach Freed
Sarah Byer
Michael Schindel
author_sort Laurel Saito
collection DOAJ
description Increased groundwater demand is causing aquifer declines that impact viability of groundwater-dependent ecosystems (GDEs) like springs and phreatophyte communities. To understand which springs and phreatophyte communities may be stressed by groundwater level declines in Oregon and Nevada, we assessed groundwater level trends in nearby monitoring wells. Very few springs and phreatophyte communities were near monitoring wells with adequate data. Less than 1% of >50,000 springs in Nevada and Oregon were within 800 m of analyzed wells, and only 52 springs were near a shallow (<30 m below ground surface) well. Among springs near analyzed wells, 56% in Nevada and 29% in Oregon were near wells with declining groundwater level trends, and percentages were similar among springs that were within 800 m of analyzed shallow wells. Less than 22% of all phreatophyte communities in Nevada and Oregon were near analyzed wells, and only 9.6% were within 800 m of a shallow well. Of phreatophyte communities near analyzed wells, 48% and 57% were near wells with declining trends in Nevada and Oregon, respectively. Differences among GDE types could reflect more groundwater development where phreatophytes exist. Differences between states in proportion of springs near wells with declining trends could be due to more surface water capture in Oregon or increased pressure for groundwater development in Nevada. State-specific policies and administration of groundwater rights and monitoring affect data availability and trends observed in the two states. More groundwater level data are essential for understanding impacts of groundwater withdrawals to GDEs.
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spelling doaj.art-3376ca4d024a4c2898646515b0f5ba172022-12-22T02:59:27ZengFrontiers Media S.A.Frontiers in Environmental Science2296-665X2022-12-011010.3389/fenvs.2022.10071141007114The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021Laurel Saito0Zach Freed1Sarah Byer2Michael Schindel3Nevada Business Unit, The Nature Conservancy, Reno, NV, United StatesOregon Business Unit, The Nature Conservancy, Bend, OR, United StatesNevada Business Unit, The Nature Conservancy, Reno, NV, United StatesOregon Business Unit, The Nature Conservancy, Bend, OR, United StatesIncreased groundwater demand is causing aquifer declines that impact viability of groundwater-dependent ecosystems (GDEs) like springs and phreatophyte communities. To understand which springs and phreatophyte communities may be stressed by groundwater level declines in Oregon and Nevada, we assessed groundwater level trends in nearby monitoring wells. Very few springs and phreatophyte communities were near monitoring wells with adequate data. Less than 1% of >50,000 springs in Nevada and Oregon were within 800 m of analyzed wells, and only 52 springs were near a shallow (<30 m below ground surface) well. Among springs near analyzed wells, 56% in Nevada and 29% in Oregon were near wells with declining groundwater level trends, and percentages were similar among springs that were within 800 m of analyzed shallow wells. Less than 22% of all phreatophyte communities in Nevada and Oregon were near analyzed wells, and only 9.6% were within 800 m of a shallow well. Of phreatophyte communities near analyzed wells, 48% and 57% were near wells with declining trends in Nevada and Oregon, respectively. Differences among GDE types could reflect more groundwater development where phreatophytes exist. Differences between states in proportion of springs near wells with declining trends could be due to more surface water capture in Oregon or increased pressure for groundwater development in Nevada. State-specific policies and administration of groundwater rights and monitoring affect data availability and trends observed in the two states. More groundwater level data are essential for understanding impacts of groundwater withdrawals to GDEs.https://www.frontiersin.org/articles/10.3389/fenvs.2022.1007114/fullgroundwater level trendsgroundwater-dependent ecosystemsstressorsgroundwater pumpingspringsphreatophytes
spellingShingle Laurel Saito
Zach Freed
Sarah Byer
Michael Schindel
The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
Frontiers in Environmental Science
groundwater level trends
groundwater-dependent ecosystems
stressors
groundwater pumping
springs
phreatophytes
title The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
title_full The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
title_fullStr The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
title_full_unstemmed The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
title_short The vulnerability of springs and phreatophyte communities to groundwater level declines in Oregon and Nevada, 2002–2021
title_sort vulnerability of springs and phreatophyte communities to groundwater level declines in oregon and nevada 2002 2021
topic groundwater level trends
groundwater-dependent ecosystems
stressors
groundwater pumping
springs
phreatophytes
url https://www.frontiersin.org/articles/10.3389/fenvs.2022.1007114/full
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