In-stream large woody debris loading and riparian forest seral stage associations in the southern Appalachian Mountains

1996 ◽  
Vol 26 (7) ◽  
pp. 1218-1227 ◽  
Author(s):  
Craig W. Hedman ◽  
David H. Van Lear ◽  
Wayne T. Swank
Keyword(s):  
Riparian Forest ◽  
Woody Debris ◽  
American Chestnut ◽  
Eastern Hemlock ◽  
Large Woody Debris ◽  
Growth Stages ◽  
Old Growth ◽  
Wide Range ◽  
Carry Over ◽  
Stream Systems

Large woody debris (LWD) is an important ecological component of mountain streams. However, the relation of LWD loading and riparian forest composition is poorly understood in the southern Appalachians. In this study, 500-m reaches of 11 riparian forest–stream systems representing a 300-year sere were inventoried and measured to obtain quantitative estimates and descriptions of in-stream LWD. Loading volumes ranged from 7.1 to 31.2 m3/100 m of stream, or between 3.6 and 13.2 kg/m2. LWD loadings were highly variable during midseral stages of plant community succession, primarily because of the wide range in loading of American chestnut (Castaneadentata (Marsh.) Borkh.). Loadings increased linearly in late-successional through old-growth systems over a 165-year interval. Eastern hemlock (Tsugacanadensis (L.) Carrière) and American chestnut were the most dominant carry-over LWD species in midsuccessional stream systems. Loading of eastern hemlock LWD increased from midsuccessional through old-growth stages as the species became dominant in the riparian forest. Without carry-over debris, LWD loadings would be extremely low in midsuccessional stream systems. American chestnut was a major component of LWD in midsuccessional stream systems, despite the fact that it has been unavailable for recruitment for decades.

Riparian aquatic interaction simulator (RAIS): a model of riparian forest dynamics for the generation of large woody debris and shade

2002 ◽  
Vol 162 (2-3) ◽  
pp. 299-318 ◽  
Author(s):  
Jeffrey J. Welty ◽  
Timothy Beechie ◽  
Kathleen Sullivan ◽  
David M. Hyink ◽  
Robert E. Bilby ◽  
...  
Keyword(s):  
Forest Dynamics ◽  
Riparian Forest ◽  
Woody Debris ◽  
Large Woody Debris

Volumosina, a new Nearctic genus for the rare old-growth forest fly Herniosina voluminosa Marshall (Diptera: Sphaeroceridae)

2017 ◽  
Vol 149 (4) ◽  
pp. 444-460 ◽  
Author(s):  
Jindřich Roháček ◽  
Stephen A. Marshall
Keyword(s):  
Natural History ◽  
New Genus ◽  
Woody Debris ◽  
Morphological Characters ◽  
Large Woody Debris ◽  
New Combination ◽  
Old Growth ◽  
History Data ◽  
Old Growth Forest

AbstractVolumosinanew genus (Diptera: Sphaeroceridae: Limosininae) is described to accomodate the enigmatic Nearctic species Herniosina voluminosa Marshall, 1987 and its relationships are discussed. Based on morphological characters Volumosina is treated as part of the Limosina genus group along with Apteromyia Vimmer, 1929, Gigalimosina Roháček, 1983, Herniosina Roháček, 1983, and Limosina Macquart, 1835 but its position within the group remains unresolved. Volumosina voluminosa (Marshall, 1987) new combination is recorded from Canada and redescribed with new distributional and natural history data suggesting that it is an old-growth specialist associated with large woody debris. The gigantism of the male aedeagal complex of V. voluminosa is discussed.

Stream channel configuration, landform, and riparian forest structure in the Cascade Mountains, Washington

2000 ◽  
Vol 57 (4) ◽  
pp. 699-707 ◽  
Author(s):  
Byron W Rot ◽  
Robert J Naiman ◽  
Robert E Bilby
Keyword(s):  
Plant Community ◽  
Riparian Forest ◽  
Woody Debris ◽  
Basal Area ◽  
Old Growth ◽  
Tree Diameter ◽  
Riparian Tree ◽  
Channel Configuration ◽  
Riparian Plant ◽  
Channel Type

The hierarchical relationship of five key elements, valley constraint, riparian landform, riparian plant community, channel type, and channel configuration, are described for 21 sites in mature to old-growth riparian forests of the western Cascades Mountains, Washington, U.S.A. Channel type (bedrock, plane-bed, and forced pool-riffle) was closely related to channel configuration (especially large woody debris (LWD) volume, density, and LWD-formed pools) at the smallest spatial scale and valley constraint at the largest. Valley constraint significantly influenced off-channel habitat (r2 = 0.71) and LWD volume within forced pool-riffle channels (r2 = 0.58). Riparian plant community composition was differentiated by four landform classes: three alluvial landforms based on height above the channel and one based on hillslope. Just above the active channel, floodplain landforms contained more deciduous stems than conifer and greater conifer basal area than deciduous. Conifers dominated other landforms. The diameter of in-channel LWD increased with the age of the riparian forest (r2 = 0.34). In old-growth forests, LWD diameter was equivalent to or greater than the average riparian tree diameter for all sites. In younger forests, the mixed relationship between LWD and riparian tree diameter may reflect a combination of LWD input from the previous old-growth stand and LWD input from the existing stand.

scholarly journals Simulating the Effects of Forest Management on Large Woody Debris in Streams in Northern Idaho

2007 ◽  
Vol 22 (2) ◽  
pp. 81-87 ◽  
Author(s):  
Mark Teply ◽  
Dale McGreer ◽  
Dennis Schult ◽  
Patrick Seymour
Keyword(s):  
Riparian Forest ◽  
Woody Debris ◽  
Timber Harvest ◽  
Forest Harvesting ◽  
Large Woody Debris ◽  
Growth And Yield ◽  
Directional Bias ◽  
Riparian Management ◽  
Significant Difference ◽  
Northern Idaho

Abstract Existing models for simulating large woody debris (LWD) loads of forest streams were adapted for forest conditions in northern Idaho. Effects of riparian management prescriptions implemented for streams within a habitat conservation planning area for bull trout and other sensitive species were evaluated based on riparian and instream LWD conditions observed along 58 randomly selected stream segments. A wood budgeting system presented by Welty et al. (2002. Riparian aquatic interaction simulator (RAIS): A model of riparian forest dynamics for the generation of large woody debris and shade. For. Ecol. Manage. 162:299–318) was employed through use of observed starting instream LWD loads and generalized depletion rates. LWD recruitment estimates were based on locally relevant growth and yield simulators, taper equations, and adjustments for tree fall directional bias. LWD loading, expressed as the number of qualifying pieces per 1,000 ft of stream, was examined under two scenarios: a no-harvest scenario and a harvest scenario. Results indicated no significant difference in the frequency distribution of simulated LWD loading between the no-harvest and harvest scenarios over a 100-year prediction period. Examination of our assumptions indicated that LWD loading was likely underestimated and less variable than would be expected. However, these assumptions had equal effects on each scenario, enabling us to confidently interpret the effects of timber harvest. The nature and extent of riparian forest harvesting evaluated in this simulation is similar to levels being considered elsewhere in the region. Therefore, simulation techniques demonstrated here could be applied elsewhere in the region for evaluating the potential effects of riparian management on fisheries resources.

Characteristics and Function of Large Woody Debris in Streams Draining Old-Growth, Clear-Cut, and Second-Growth Forests in Southwestern Washington

1991 ◽  
Vol 48 (12) ◽  
pp. 2499-2508 ◽  
Author(s):  
Robert E. Bilby ◽  
James W. Ward
Keyword(s):  
Woody Debris ◽  
Sediment Accumulation ◽  
Pool Size ◽  
Large Woody Debris ◽  
Old Growth ◽  
Clear Cut ◽  
Second Growth ◽  
Stream Size ◽  
And Function ◽  
Pool Formation

Amount of large woody debris (LWD) surveyed in 70 stream reaches flowing through old-growth, clear-cut, and second-growth forests decreased with increasing stream size for all stand types but was greatest at old-growth sites. Average piece volume was larger at old-growth sites than at other stand types in streams >10 m wide, but no differences were seen in smaller streams. Scour pools accounted for 90% of the wood-associated pools at second-growth and clear-cut sites but only 50% at old-growth sites, which contained more pools than other stand types, particularly for larger streams. Pool size was similar for all stand types in smaller streams, but averaged 10 m2 in streams >10 m wide at old-growth sites and 4 m2 for other stand types. Pool size was similar for all stand types in smaller streams. Sediment and fine organic matter retained by woody debris decreased with increasing stream size for ail stand types, but old-growth sites contained greater amounts of both materials than other stand types. The frequency of pool formation, the type of pool formed, and sediment accumulation were influenced by the amount of fine debris associated with LWD. Changes in LWD amount, characteristics, and function occurred very rapidly following removal of streamside vegetation.

Treatment of old-growth stands and its effects on birds, ants, and large woody debris: a case study.

1995 ◽  
Author(s):  
Evelyn L. Bull ◽  
Torolf R. Torgersen ◽  
Arlene K. Blumton ◽  
Carol M. McKenzie ◽  
Dave S. Wyland
Keyword(s):  
Woody Debris ◽  
Large Woody Debris ◽  
Old Growth

Dynamics of large woody debris in streams in old-growth Douglas-fir forests

1987 ◽  
Vol 17 (2) ◽  
pp. 150-156 ◽  
Author(s):  
G. W. Lienkaemper ◽  
F. J. Swanson
Keyword(s):  
Woody Debris ◽  
Douglas Fir ◽  
Large Woody Debris ◽  
Time And Space ◽  
Old Growth ◽  
Order Stream ◽  
Fifth Order ◽  
Bankfull Width ◽  
Downstream Movement

Transfer of large woody debris (>10 cm diameter) from old-growth Douglas-fir (Pseudotsugamenziesii (Mirbel) Franco) forests into five first-to fifth-order stream reaches (drainage areas of 0.1 to 60.5 km2) has ranged from 2.0 to 8.8 Mg•ha−1•year−1 in 7- to 9-year study periods. Amounts of large debris in these streams range from 230 to 750 Mg•ha−1 with generally lower values in larger channels. The addition of woody debris is widely scattered in time and space and comes mainly from single trees rooted away from the streambank. We infer that wind is a major agent for entry of wood into these streams. Downstream movement of debris is strongly related to length of individual pieces; most pieces that moved were shorter than bankfull width.

Changes in the quantity and characteristics of large woody debris in streams of the Olympic Peninsula, Washington, U.S.A. (1982-1993)

1998 ◽  
Vol 55 (6) ◽  
pp. 1395-1407 ◽  
Author(s):  
Michael L McHenry ◽  
Eric Shott ◽  
Robert H Conrad ◽  
Glenn B Grette
Keyword(s):  
Woody Debris ◽  
Small Diameter ◽  
High Mobility ◽  
Decay Rates ◽  
Riparian Forests ◽  
Large Woody Debris ◽  
Olympic Peninsula ◽  
Old Growth ◽  
Second Growth ◽  
The Mean

We assessed the changes in large woody debris (LWD) abundance and composition at 28 sites in 27 low-gradient Olympic Peninsula streams between 1982 and 1993. The average number of pieces of debris was virtually identical (P = 0.98) in both years (50.7 versus 50.6). However, we found a significant (P <= 0.01) reduction in the total volume of LWD material in the stream sites surveyed (51.7 m3 ·100 m-1 in 1982 to 38.2 m3 ·100 m-1 in 1993). While the mean volume of second-growth derived LWD increased from 3.6 to 10.9 m3 ·100 m-1 (P < 0.01), the increase was insufficient to offset the loss of old-growth derived LWD. The mean volume of old-growth derived LWD for all sites decreased from 48.1 to 27.4 m3 ·100 m-1 between sample years (P < 0.01). The mean diameter of second-growth derived LWD was significantly larger in 1993 than in 1982, although still smaller than old-growth derived pieces. We measured a significant increase in the percentage of LWD pieces rated as highly decayed from 1982 to 1993. The results indicate that the loss of old-growth derived LWD following the removal of old-growth riparian forests is initially very rapid, followed by a slower rate of depletion associated with watershed destabilization. Inputs of LWD from second-growth riparian forests up to 73 years old were characterized by small diameter, high mobility, and high decay rates.

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