Ecosystem nutrient responses to chronic nitrogen inputs at Fernow Experimental Forest, West Virginia

1996 ◽  
Vol 26 (2) ◽  
pp. 196-205 ◽  
Author(s):  
Frank S. Gilliam ◽  
Bradley M. Yurish ◽  
Mary Beth Adams
Keyword(s):  
West Virginia ◽  
Plant Tissue ◽  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Growing Season ◽  
N Saturation ◽  
Nitrogen Inputs ◽  
Overstory Tree ◽  
Fernow Experimental Forest

Among the current environmental concerns for forests of the eastern United States is nitrogen (N) saturation, a result of excessive inputs of N associated with acidic deposition. We studied nutrient responses on N-treated and untreated watersheds of the Fernow Experimental Forest, West Virginia, to test for evidence of N saturation on the treated watershed. The watersheds were WS7 (23-year-old even-aged control), WS4 (mature mixed-aged control), and WS3 (23-year-old even-aged treatment). WS3 has received aerial applications of (NH4)2SO4 from 1989 to the present (a total of 4 years for the study period) at 3 × ambient inputs of N and S (54 and 61 kg•ha−1•year−1, respectively). Base-flow stream samples were collected weekly from each watershed and analyzed for NO3− and Ca2+. Mineral soil was incubated in situ, placed in bags, and buried about every 30 days during the growing season in each of seven sample plots within each watershed. Moist samples of soil from the bags were analyzed for extractable NH4+ and NO3−. In addition, forest floor material and leaves of an herbaceous species (Violarotundifolia Michx.) from each plot were analyzed for N and other nutrients. Violarotundifolia was present on all 21 plots and used as an additional indicator of N availability and soil fertility. Foliage tissue was sampled from overstory tree species (Liriodendrontulipifera L., Prunusserotina Ehrh., Betulalenta L., and Acerrubrum L.) from WS3 and WS7 and analyzed for nutrient content. Results from the 1993 growing season showed few, if any, differences among watersheds for (1) N content and C/N ratio of the mineral soil and forest floor and (2) relative proportion of NH4+ and NO3− produced in the buried bags. Nitrification rates were equally high in soils of all watersheds; N concentrations were significantly higher in foliage tissue of overstory tree species and of V. rotundifolia in the treatment versus control watersheds; plant tissue Ca was significantly lower for the treatment watershed than for the control watersheds. Our results support the conclusions of earlier studies that high amounts of ambient N deposition have brought about N saturation on untreated watersheds at the Fernow Experimental Forest. This is suggested by minimal differences among watersheds in N mineralization and nitrification and soil and forest floor N. However, aggravated N saturation on our treated watershed can be seen in differences in plant tissue nutrients among watersheds and streamflow data, indicating increased losses of NO3− with accompanying losses of Ca2+ in response to further N additions to a N-saturated system.

Substrate and litterfall effects on conifer seedling survivorship in southern boreal stands of Canada

2003 ◽  
Vol 33 (4) ◽  
pp. 672-681 ◽  
Author(s):  
Marie-Josée Simard ◽  
Yves Bergeron ◽  
Luc Sirois
Keyword(s):  
Populus Tremuloides ◽  
Picea Glauca ◽  
Forest Floor ◽  
Mineral Soil ◽  
Abies Balsamea ◽  
Growing Season ◽  
Winter Survival ◽  
Thuja Occidentalis ◽  
Seedling Survivorship ◽  
Conifer Seedling

Most conifer seeds die as seeds or seedlings within 5 years after dispersal. Understanding what factors keep a few of them alive is essential if natural regeneration is to be maintained in managed forests. For example, decaying logs and the conifer seedlings that often grow on them are rare under certain canopies such as deciduous trembling aspen (Populus tremuloides Michx.). We conducted a seeding experiment to evaluate the role of certain substrates, and litterfall, on early conifer survivorship. Seeds of balsam fir (Abies balsamea (L.) Mill.), white spruce (Picea glauca (Moench) Voss), and eastern white-cedar (Thuja occidentalis L.) were sown during 2 consecutive years on mineral soil, relocated logs, and litter in deciduous aspen and coniferous (Thuja occidentalis dominated) stands. Seedling survivor ship was monitored at the end of the first growing season and 1 year after each sowing. Conifer seedling survivorship was equivalent or greater under aspen than under cedar-dominated canopies. Picea and Thuja survivorship was highest on decaying logs of approximately 9 cm high (compared with logs buried at forest floor level) and lowest on forest floor litter during both the first growing season and the following autumn–winter. Abies survivorship was little affected by substrate type, except for low autumn–winter survival on litter. Thuja autumn–winter survival was significantly reduced by litterfall in both deciduous and coniferous stands.

Admixing other tree species to European beech forests: Effects on soil organic carbon and total nitrogen stocks. A review.

2020 ◽  
Author(s):  
Stephanie Rehschuh ◽  
Michael Dannenmann
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Total Nitrogen ◽  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
European Beech ◽  
Summer Drought ◽  
Beech Forests ◽  
Soc Stocks

<p>Drought-sensitive European beech forests are increasingly challenged by climate change. Admixing other, preferably more deep-rooting, tree species has been proposed to increase the resilience of beech forests to summer drought. This might not only alter soil water dynamics and availability, but also soil organic carbon (SOC) and total nitrogen (TN) storage in soils. Since information of these effects is scattered, our aim was to synthesize results from studies that compared SOC/TN stocks of beech monocultures with those of mixed beech stands as well as of other monocultures. We conducted a meta-analysis including 40 studies with 208, 231 and 166 observations for forest floor, mineral soil and the total soil profile, respectively. Pure conifer stands had higher SOC stocks compared to beech in general, especially in the forest floor with up to 200% (larch forests). Other broadleaved tree species (ash, oak, lime, maple, hornbeam) showed in comparison to beech lower SOC storage in the forest floor, with little impact on total stocks.  Similarly, for mixed beech-conifer stands we found significantly increased SOC stocks of >10% and a small increase in TN stocks of approx. 4% compared to beech monocultures, which means a potential SOC storage increase of >0.1 t ha<sup>-1</sup>yr<sup>-1 </sup>(transformation of mineral soil to 100 cm depth). In contrast, mixed beech-broadleaved stands did not show a significant change in total SOC stocks. Currently, the influence climatic and soil parameters on SOC changes due to admixture of other tree species is analyzed based on this dataset. This is expected to facilitate an assessment which mixtures with beech have the largest potential towards increasing SOC stocks.</p>

Tree species and soil nutrient profiles in old-growth forests of the Oregon Coast Range

2011 ◽  
Vol 41 (1) ◽  
pp. 195-210 ◽  
Author(s):  
Alison Cross ◽  
Steven S. Perakis
Keyword(s):  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Soil Nutrient ◽  
Douglas Fir ◽  
Western Hemlock ◽  
Coast Range ◽  
Old Growth ◽  
Oregon Coast Range ◽  
Old Growth Forests

Old-growth forests of the Pacific Northwest provide a unique opportunity to examine tree species – soil relationships in ecosystems that have developed without significant human disturbance. We characterized foliage, forest floor, and mineral soil nutrients associated with four canopy tree species (Douglas-fir (Pseudotsuga menziesii (Mirbel) Franco), western hemlock (Tsuga heterophylla (Raf.) Sarg.), western redcedar (Thuja plicata Donn ex D. Don), and bigleaf maple (Acer macrophyllum Pursh)) in eight old-growth forests of the Oregon Coast Range. The greatest forest floor accumulations of C, N, P, Ca, Mg, and K occurred under Douglas-fir, primarily due to greater forest floor mass. In mineral soil, western hemlock exhibited significantly lower Ca concentration and sum of cations (Ca + Mg + K) than bigleaf maple, with intermediate values for Douglas-fir and western redcedar. Bigleaf maple explained most species-based differences in foliar nutrients, displaying high concentrations of N, P, Ca, Mg, and K. Foliar P and N:P variations largely reflected soil P variation across sites. The four tree species that we examined exhibited a number of individualistic effects on soil nutrient levels that contribute to biogeochemical heterogeneity in these ecosystems. Where fire suppression and long-term succession favor dominance by highly shade-tolerant western hemlock, our results suggest a potential for declines in both soil Ca availability and soil biogeochemical heterogeneity in old-growth forests.

Response of N2O emissions to logging residue piles of Norway spruce, Scots pine and silver birch

2020 ◽  
Author(s):  
Tiina Törmänen ◽  
Antti-Jussi Lindroos ◽  
Veikko Kitunen ◽  
Aino Smolander
Keyword(s):  
Norway Spruce ◽  
Tree Species ◽  
Forest Floor ◽  
Growing Season ◽  
N Losses ◽  
Clear Cut ◽  
Net Nitrification ◽  
Logging Residues ◽  
Soil Temperatures ◽  
Logging Residue

<p>Utilization of forest bioenergy is increasing; however, the overall environmental impacts of forest bioenergy utilization are not fully understood. Especially effects on N<sub>2</sub>O emissions in mineral soils are less studied. With current harvesting practices, either whole-tree-harvest or stem-only-harvest, piles of logging residues are left on the forest floor. As a result, soil nitrogen (N) cycling processes can be accelerated on clear cut area under the piles, especially net nitrification. When N is transformed to more mobile form, the risk for N losses via nitrous oxide (N<sub>2</sub>O) emissions from the forest floor may increase.</p><p>We studied how logging residue piles of three tree species, Norway spruce (Picea abies (L.) Karst.), Scots pine (Pinus sylvestris L.) and silver birch (Betula pendula Roth.), influence gaseous losses of N after clear-cut. A Norway spruce dominated mixed stand on a mineral soil site was clear-cut and N<sub>2</sub>O emissions were monitored. There were four treatments; three tree species treatments consisting of 40 kg m<sup>-2</sup> of fresh logging residues and control plot without residues as an additional treatment. Effects of logging residue piles on N<sub>2</sub>O emissions were monitored over 4 growing season with closed chamber technic. Simultaneously soil temperatures were recorded over 2 growing season. Soil denitrification activity and the contribution of nitrification and denitrification to N<sub>2</sub>O production were determined in laboratory experiments.</p><p>Logging residue piles lowered and balanced fluctuation of soil temperatures. N<sub>2</sub>O fluxes peaked under the piles during the second and third growing season after the establishment of the piles; however inconsistent fluxes tended to be low. The production of N<sub>2</sub>O was driven by both nitrification and denitrification processes, the proportion depending on the tree species. Our results indicate that logging residue piles accelerate N losses as gaseous form; however studies on the same field experiment shows that most of the N losses occur through soil percolation waters. Spruce residues tend to stimulate N<sub>2</sub>O emissions longer compared to other tree species. There was a positive correlation with net nitrification and microbial biomass C (Törmänen et al. 2018, FORECO). These results have implications for sustainable and productive forest management practices and nutrition of re-growing vegetation.</p>

scholarly journals Factors Influencing Spatial Variability in Nitrogen Processing in Nitrogen-Saturated Soils

2001 ◽  
Vol 1 ◽  
pp. 505-513 ◽  
Author(s):  
Frank S. Gilliam ◽  
Frank C.C. Somerville ◽  
Frank N.L. Lyttle ◽  
Frank M.B. Adams
Keyword(s):  
Spatial Variability ◽  
N Mineralization ◽  
Forest Floor ◽  
Mineral Soil ◽  
Nitrifying Bacteria ◽  
Saturated Soils ◽  
N Saturation ◽  
Net N Mineralization ◽  
Net Nitrification ◽  
Floor Material

Nitrogen (N) saturation is an environmental concern for forests in the eastern U.S. Although several watersheds of the Fernow Experimental Forest (FEF), West Virginia exhibit symptoms of N saturation, many watersheds display a high degree of spatial variability in soil N processing. This study examined the effects of temperature on net N mineralization and nitrification in N-saturated soils from FEF, and how these effects varied between high N-processing vs. low N-processing soils collected from two watersheds, WS3 (fertilized with [NH4]2SO4) and WS4 (untreated control). Samples of forest floor material (O1 horizon) and mineral soil (to a 5-cm depth) were taken from three subplots within each of four plots that represented the extremes of highest and lowest rates of net N mineralization and nitrification (hereafter, high N and low N, respectively) of untreated WS4 and N-treated WS3: control/low N, control/high N, N-treated/low N, N-treated/high N. Forest floor material was analyzed for carbon (C), lignin, and N. Subsamples of mineral soil were extracted immediately with 1 N KCl and analyzed for NH4+ and NO3-to determine preincubation levels. Extracts were also analyzed for Mg, Ca, Al, and pH. To test the hypothesis that the lack of net nitrification observed in field incubations on the untreated/low N plot was the result of absence of nitrifier populations, we characterized the bacterial community involved in N cycling by amplification of amoA genes. Remaining soil was incubated for 28 d at three temperatures (10, 20, and 30°C), followed by 1 NKCl extraction and analysis for NH4+and NO3-. Net nitrification was essentially 100% of net N mineralization for all samples combined. Nitrification rates from lab incubations at all temperatures supported earlier observations based on field incubations. At 30°C, rates from N-treated/high N were three times those of N-treated/low N. Highest rates were found for untreated/high N (two times greater than those of N-treated/high N), whereas untreated/low N exhibited no net nitrification. However, soils exhibiting no net nitrification tested positive for presence of nitrifying bacteria, causing us to reject our initial hypothesis. We hypothesize that nitrifier populations in such soil are being inhibited by a combination of low Ca to Al ratios in mineral soil and allelopathic interactions with mycorrhizae of ericaceous species in the herbaceous layer.

Carbon and nitrogen in forest floor and mineral soil under six common European tree species

2008 ◽  
Vol 255 (1) ◽  
pp. 35-48 ◽  
Author(s):  
Lars Vesterdal ◽  
Inger K. Schmidt ◽  
Ingeborg Callesen ◽  
Lars Ola Nilsson ◽  
Per Gundersen
Keyword(s):  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Carbon And Nitrogen

Forest floor chemistry under seven tree species along a soil fertility gradient

1998 ◽  
Vol 28 (11) ◽  
pp. 1636-1647 ◽  
Author(s):  
Lars Vesterdal ◽  
Karsten Raulund-Rasmussen
Keyword(s):  
Soil Fertility ◽  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Nutrient Status ◽  
Nutrient Ratios ◽  
Fertility Gradient ◽  
Soil Fertility Gradient ◽  
Element Contents ◽  
Forest Floors

Forest floor chemistry, i.e., C/nutrient ratios, pH, and element contents, were determined in stands of two deciduous species and five conifer species replicated at seven sites along a soil fertility gradient. There were consistent differences between forest floors of the tree species. Lodgepole pine (Pinus contorta Dougl.) forest floors had highest C/nutrient ratios, lowest pH, and the greatest element contents, whereas oak (Quercus robur L.) forest floors had low C/nutrient ratios and the lowest element contents of all species. Differences in forest floor C/nutrient ratios, pH, and element contents between sites of low nutrient status and sites of intermediate to high nutrient status were also great. Forest floor pH was related to mineral soil pH, and C/P, C/Ca, and C/K ratios were related to mineral soil nutrient concentrations. Forest floor C content was negatively related to most mineral soil fertility variables and was closest related to texture, pH, and concentrations of P and Ca. The C content of lodgepole pine and oak forest floors tended to be less affected by the soil fertility gradient. The results suggest that C storage and immobilization of nutrients in forest floors may be managed along an extensive soil gradient by selection of the proper tree species.

Effect of tree species on carbon stocks in forest floor and mineral soil and implications for soil carbon inventories

2008 ◽  
Vol 256 (3) ◽  
pp. 482-490 ◽  
Author(s):  
Catharina J.E. Schulp ◽  
Gert-Jan Nabuurs ◽  
Peter H. Verburg ◽  
Rein W. de Waal
Keyword(s):  
Soil Carbon ◽  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Carbon Stocks

The Forest Floor and Mineral Soil Carbon Pools of Six Different Forest Tree Species

Ekoloji ◽  
2011 ◽  
Vol 20 (81) ◽  
pp. 8-14 ◽  
Author(s):  
Orhan Sevgi ◽  
Ender Makineci ◽  
Omer Karaoz
Keyword(s):  
Soil Carbon ◽  
Tree Species ◽  
Forest Floor ◽  
Mineral Soil ◽  
Forest Tree ◽  
Carbon Pools ◽  
Forest Tree Species ◽  
Soil Carbon Pools

Asymbiotic nitrogen fixation and denitrification in a mature forest in coastal British Columbia

1989 ◽  
Vol 19 (9) ◽  
pp. 1194-1200 ◽  
Author(s):  
G. H. Cushon ◽  
M. C. Feller
Keyword(s):  
British Columbia ◽  
Nitrogen Fixation ◽  
Forest Floor ◽  
Mineral Soil ◽  
Gaseous Nitrogen ◽  
Blue Green Algae ◽  
Asymbiotic Nitrogen Fixation ◽  
Nitrogen Inputs ◽  
Decaying Wood ◽  
Floor Material

Gaseous nitrogen inputs due to asymbiotic nitrogen fixation and outputs due to biological denitrification were estimated for a mature mid-successional Pseudotsugamenziesii (Mirb.) Franco–Thujaplicata Donn–Tsugaheterophylla (Raf.) Sarg. forest in southwestern British Columbia. Forest floor material, mineral soil, decaying wood, foliage, and bark were incubated in an atmosphere of 10 kPa C2H2 to allow the simultaneous measurement of N2O production by denitrifying bacteria and C2H2 reduction by free-living bacteria and blue-green algae. Forest floor material accounted for 70% of an estimated total annual nitrogen fixation of 0.3 kg N•ha−1•year −1.•Relatively small amounts of nitrogen were fixed in mineral soil, decaying wood, and foliage, and no indication of nitrogen fixation activity in bark was detected. Some denitrification was found; it was essentially negligible, although possibly underestimated. The net gaseous nitrogen input into the mid-successional forests of the study area is likely to be < 5% of the total net nitrogen inputs, which are primarily from precipitation.

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