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Restoration increases transient storages in boreal headwater streams
Author(s) -
Marttila Hannu,
Turunen Jarno,
Aroviita Jukka,
Tammela Simo,
Luhta PirkkoLiisa,
Muotka Timo,
Kløve Bjørn
Publication year - 2018
Publication title -
river research and applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.679
H-Index - 94
eISSN - 1535-1467
pISSN - 1535-1459
DOI - 10.1002/rra.3364
Subject(s) - streams , siltation , environmental science , stream restoration , hydrology (agriculture) , sediment , large woody debris , debris , transient (computer programming) , habitat , geology , riparian zone , ecology , geomorphology , geotechnical engineering , oceanography , computer network , computer science , biology , operating system
Bed siltation can drastically alter the physical conditions of headwater streams and is therefore a stressor for stream ecosystems. We studied 32 headwater streams that represented near‐natural (reference; N = 11), sediment‐impacted ( N = 12), or wood‐ ( N = 4) or stone‐restored ( N = 5) streams to quantify how extensive siltation and restoration with either large woody debris (LWD) or boulder structures influence transient storage conditions. We carried out repeated stream tracer experiments, field measurements of habitat characteristics, and numerical simulations to determine the effects of siltation and restoration on total transient storage. Compared with reference streams, impacted streams had a smaller storage zone cross‐sectional area ( A s / A ) ratio and fraction of median travel time due to transient storage ( F 200 ), whereas restored streams had transient storage conditions similar to near‐natural conditions. Both of the two restoration methods had positive but differing impacts on bed sediment and transient storage properties. The LWD restoration created diverse total transient storage conditions, whereas boulder restoration decreased fine sediment cover. Addition of both LWD and boulders could thus aid the recovery of headwater streams from excessive sediment input and increase transient storage and in‐stream habitat complexity.