scholarly journals Status of soil acidification in North America

2006 ◽  
Vol 52 (Special Issue) ◽  
pp. S3-S13 ◽  
Author(s):  
M.E. Fenn ◽  
T.G. Huntington ◽  
S.B. McLaughlin ◽  
C. Eagar ◽  
A. Gomez ◽  
...  
Keyword(s):  
North America ◽  
Forest Soils ◽  
Soil Acidification ◽  
Sugar Maple ◽  
Base Cations ◽  
Basal Area ◽  
Base Cation ◽  
Eastern United States ◽  
San Bernardino Mountains ◽  
Wide Range

Forest soil acidification and depletion of nutrient cations have been reported for several forested regions in North America, predominantly in the eastern United States, including the northeast and in the central Appalachians, but also in parts of southeastern Canada and the southern U.S. Continuing regional inputs of nitrogen and sulfur are of concern because of leaching of base cations, increased availability of soil Al, and the accumulation and ultimate transmission of acidity from forest soils to streams. Losses of calcium from forest soils and forested watersheds have now been documented as a sensitive early indicator and a functionally significant response to acid deposition for a wide range of forest soils in North America. For red spruce, a clear link has been established between acidic deposition, alterations in calcium and aluminum supplies and increased sensitivity to winter injury. Cation depletion appears to contribute to sugar maple decline on some soils, specifically the high mortality rates observed in northern Pennsylvania over the last decade. While responses to liming have not been systematically examined in North America, in a study in Pennsylvania, restoring basic cations through liming increased basal area growth of sugar maple and levels of calcium and magnesium in soil and foliage. In the San Bernardino Mountains in southern California near the west coast, the pH of the A horizon has declined by at least 2 pH units (to pH 4.0–4.3) over the past 30 years, with no detrimental effects on bole growth; presumably, because of the Mediterranean climate, base cation pools are still high and not limiting for plant growth.

Exploring the Recruitment Dynamics of Sugar Maple and Yellow Birch Saplings into Merchantable Stems Following Harvesting in the Acadian Forest Region of New Brunswick, Canada

2021 ◽  
Author(s):  
Alex Noel ◽  
Jules Comeau ◽  
Salah-Eddine El Adlouni ◽  
Gaetan Pelletier ◽  
Marie-Andrée Giroux
Keyword(s):  
New Brunswick ◽  
Sugar Maple ◽  
Basal Area ◽  
Stem Density ◽  
Yellow Birch ◽  
Probability Of Occurrence ◽  
Silvicultural Treatment ◽  
Forest Region ◽  
Wide Range ◽  
Acadian Forest

The recruitment of saplings in forest stands into merchantable stems is a very complex process, thus making it challenging to understand and predict. The recruitment dynamics in the Acadian Forest Region of New Brunswick are not well known or documented. Our objective was to draw an inference from existing large scale routine forest inventories as to the different dynamics behind the recruitment from the sapling layer into the commercial tree size layer in terms of density and occurrence of sugar maple (Acer saccharum Marsh.) and yellow birch (Betula alleghaniensis Britt.) following harvesting, by looking at many factors on a wide range of spatial and temporal scales using models. Results suggest that the variation in density and probability of occurrence is best explained by the intensity of silvicultural treatment, by the merchantable stem density in each plot, and by the proportion of merchantable basal area of each group of species. The number of recruits of sugar maple and yellow birch stems tend be higher when time since last treatment increases, when mid to low levels of silvicultural treatment intensity were implemented, and within plots having intermediate levels of merchantable stem density. Lastly, our modeling efforts suggest that the probability of occurrence and density of recruitment of both species tend to increase while its share of merchantable basal area increases.

Present-day expansion of American beech in northeastern hardwood forests: Does soil base status matter?

2009 ◽  
Vol 39 (12) ◽  
pp. 2273-2282 ◽  
Author(s):  
Louis Duchesne ◽  
Rock Ouimet
Keyword(s):  
Acer Saccharum ◽  
Sugar Maple ◽  
Basal Area ◽  
Base Cation ◽  
Hardwood Forests ◽  
Fagus Grandifolia ◽  
Soil Base ◽  
Large Area ◽  
American Beech ◽  
Permanent Sample Plots

Recently, sugar maple ( Acer saccharum Marsh.) decline in northeastern North America has been regarded as a major factor structuring hardwood forests by favouring American beech ( Fagus grandifolia Ehrh.) in the understory of maple-dominated stands. To determine whether soil fertility differences associated with sugar maple decline may have promoted the expansion of American beech, we explored the relationships between the soil base status and the sapling and tree strata density and composition, using data from 426 permanent sample plots distributed throughout Quebec. Our results indicate that American beech is currently expanding in the sugar maple range of Quebec. The abundance and proportion of American beech in the sapling stratum are mainly associated with the proportion of American beech in the tree stratum, the relative basal area of dead sugar maple trees, and the base status of soils. In accordance with the many studies reporting on the high sensitivity of sugar maple to the acid–base status of soils and the decline of the sugar maple population, this study supports the hypothesis that soil base cation depletion, caused in part by atmospheric acid deposition, is among the main factors involved in the present-day expansion of American beech over a large area in Quebec.

scholarly journals A Canadian range extension for Wormslug (Boettgerilla pallens; Gastropoda: Stylommatophora: Boettgerillidae)

2019 ◽  
Vol 132 (3) ◽  
pp. 264-267
Author(s):  
Paul M. Catling ◽  
Brenda Kostiuk
Keyword(s):  
United States ◽  
North America ◽  
Acer Saccharum ◽  
Sugar Maple ◽  
Native Plants ◽  
Soil Surface ◽  
Eastern United States ◽  
Native Soil ◽  
Invasive Spread ◽  
First Time

The introduced Wormslug (Boettgerilla pallens Simroth, 1912) is reported from Quebec, Canada, for the first time, from two closely situated localities in Gatineau Park. It was previously reported from the Vancouver area of British Columbia and, very recently, from Newfoundland. Within the Americas, the species has been reported from northern California, Mexico, and Colombia, and, because it is easily overlooked, likely occurs elsewhere in North America, especially in the eastern United States. In Quebec, it was found in a natural Sugar Maple (Acer saccharum Marshall) woodland and an ornamental garden. Wormslug likely reached both sites with shrub plantings from commercial nurseries, probably quite recently, because the invasive spread of the species, worldwide, has occurred mostly during the last few decades. Although the woodland where it occurred is dominated by native plants, the gastropod fauna there is mainly introduced. Identification, characteristics, and ecology of Wormslug are discussed. The potential for impact on native soil and soil surface organisms, including native terrestrial slugs and snails, is noted.

Effects of base cation fertilization on soil and foliage nutrient concentrations, and litter-fall and throughfall nutrient fluxes in a sugar maple forest

1994 ◽  
Vol 24 (3) ◽  
pp. 542-549 ◽  
Author(s):  
J.W. Fyles ◽  
B. Côté ◽  
F. Courchesne ◽  
W.H. Hendershot ◽  
S. Savoie
Keyword(s):  
Nutrient Cycling ◽  
Forest Floor ◽  
Sugar Maple ◽  
Base Cations ◽  
Base Cation ◽  
Nutrient Concentrations ◽  
Litter Fall ◽  
Fertilizer Response ◽  
Foliar Concentrations ◽  
Cycling System

Application of base cation fertilizers is widely used to ameliorate decline symptoms in hardwood forests in southern Quebec, but little is known about the effects of fertilization on nutrient cycling. Control and fertilized plots in a sugar maple (Acersaccharum Marsh.) dominated stand were monitored over a 4-year period to determine the effects of fertilization on exchangeable soil base cations in soil, foliar nutrient concentrations, and fluxes of N, K, Ca, and Mg in litter fall and throughfall. Fertilization had a large, immediate effect on exchangeable K, whereas effects on Ca and Mg were delayed and restricted to the organic forest floor, presumably because of the lower solubility of the limestone-based Ca and Mg components of the fertilizer. Fertilization raised pH in the organic forest floor the second and third years after application but had no effect in the B horizon. Foliar K, Ca, and Mg were elevated in the year of fertilization, but foliar concentrations of Ca and Mg did not differ from, or were lower than, controls in following years. Litter-fall K flux was increased by fertilization, but litter-fall Ca and Mg fluxes and all through-fall base cation fluxes were unaffected. In control plots, nutrient concentrations in soil remained relatively constant throughout the study, but foliar concentrations and, in particular, litter-fall fluxes varied widely from year to year. This natural variation caused control plots to shift from a state of deficiency in N, Ca, and Mg to a nutrient-sufficient state between the first and second years of study. Fertilization effects are superimposed on a naturally variable nutrient cycling system, and controls on this variability must be understood if fertilizer response is to be accurately predicted.

Base cation reservoirs in soil control the buffering capacity of lakes in forested catchments

2006 ◽  
Vol 63 (3) ◽  
pp. 471-474 ◽  
Author(s):  
Daniel Houle ◽  
Rock Ouimet ◽  
Suzanne Couture ◽  
Christian Gagnon
Keyword(s):  
Surface Water ◽  
North America ◽  
Surface Waters ◽  
Base Cations ◽  
Base Cation ◽  
Acid Neutralizing Capacity ◽  
Forested Catchments ◽  
Northeastern North America ◽  
Poor Recovery ◽  
Neutralizing Capacity

The acidification of forest soils and surface waters and their relatively poor recovery record following reductions in atmospheric sulphur emissions is a major ongoing environmental problem, particularly in northeastern North America. The slow recovery of surface water is widely hypothesized to result from depletion of reservoirs of base cations in soil. This is concordant with the theory that the acid-neutralizing capacity (ANC) of lakes is likely proportional to the size of the exchangeable base cation reservoirs present in surrounding watershed soils. However, data describing these linkages are still nonexistent in the literature. Here we show that lake ANC is highly predictable (r2 = 0.75) based on the size of the exchangeable Ca2+ reservoir in soil in 21 catchments representative of soil and lake conditions encountered in northeastern North America. This finding indirectly supports the hypothesis that the poor recovery of surface water from acidification is governed by the size of base cation reservoirs present in catchment soils. The size of the base cation reservoir in soil is thus a strong indicator of the acid–base status of both soils and surface waters.

Beyond oak regeneration: modelling mesophytic sapling density drivers along topographic, edaphic, and stand-structural gradients in mature oak-dominated forests of Appalachian Ohio

2020 ◽  
Vol 50 (11) ◽  
pp. 1215-1227
Author(s):  
Don C. Radcliffe ◽  
Stephen N. Matthews ◽  
David M. Hix
Keyword(s):  
Sugar Maple ◽  
Acer Rubrum ◽  
Basal Area ◽  
Fagus Grandifolia ◽  
Active Management ◽  
Permanent Plots ◽  
Eastern United States ◽  
Red Maple ◽  
American Beech ◽  
Sapling Density

Shade-tolerant mesophytic tree species tend to dominate the understories of present-day oak–hickory and mixed-hardwood forests in the eastern United States. We quantified the sapling density associations with abiotic and biotic variables for three important mesophytic species: red maple (Acer rubrum L.), sugar maple (Acer saccharum Marsh.), and American beech (Fagus grandifolia Ehrh.) in southeastern Ohio. In this study, we sampled 165 permanent plots in oak-dominated, topographically diverse, mature (>90 years old), second-growth forests following a time span of 21–25 years (1993–1995 and 2016–2018) between samples on the Athens and Marietta units of the Wayne National Forest. Our models showed that sugar maple was strongly associated with high pH soils and red maple was strongly associated with low pH soils. Additionally, red maple was associated with upper slope positions and older stands, while American beech was associated with lower slopes, northeasterly aspects, and northeast-facing upper slopes. Basal area of competing species, solum depth, and management unit were not significantly related to sapling density for our focal species. American beech sapling density doubled between the two sampling periods, while densities of both maple species declined by half. Our results will help scientists and managers by providing insight into potential future composition of currently oak-dominated forests in areas without active management intervention.

Relationships among crown condition, growth, and stand nutrition in seven northern Vermont sugarbushes

1995 ◽  
Vol 25 (3) ◽  
pp. 386-397 ◽  
Author(s):  
Timothy R. Wilmot ◽  
David S. Ellsworth ◽  
Melvin T. Tyree
Keyword(s):  
Soil Ph ◽  
Sugar Maple ◽  
Basal Area ◽  
Base Cation ◽  
Strongly Correlated ◽  
Crown Condition ◽  
Basal Area Growth ◽  
Area Growth ◽  
Crown Dieback

We compared growth with soil and foliar elemental composition in seven stands of sugar maple (Acersaccharum Marsh.) in northern Vermont characterized by high or low incidence of crown dieback over the period 1989–1992. In stands with low-quality crown conditions, such as elevated crown dieback, long-term basal area growth rates were approximately half of those in stands with higher crown quality. Average annual basal area growth was 17.5 cm2 for dominant trees in these stands during the period 1953–1992 compared with 32.3 cm2 for trees in higher quality stands. The occurrence of elevated crown dieback was apparently unrelated to stand characteristics such as stand age, basal area, stem density, elevation, or aspect among the stands sampled. Stands with elevated crown dieback were found on soils characterized by low pH ( <4.0), low base cation pools (particularly Ca and Mg), and higher Al in soil surface horizons than higher quality stands. Over 4 years, sugar maple stands with elevated crown dieback exhibited significantly lower (P < 0.01) foliar Ca concentrations and somewhat lower foliar N and Mg than higher quality stands, while soil and foliar K were similar in both dieback classes. Among survey plots sampled in 1989, soil pH and Ca were strongly correlated with foliar Ca and K (P < 0.001). Soil pH, soil Ca, and foliar Ca were also strongly correlated with the level of crown dieback among plots and stands (P < 0.0001). Our results indicate that podzolic soils in northern Vermont may present marginal conditions for sugar maple growth in terms of soil pH and soil Ca availability, but that P and K pools appear to be sufficient for growth. While a lack of historical data prevents identification of long-term trends in nutrient availability in these soils, factors promoting losses of base cations from acidic, base-cation-poor Podzols may also exacerbate foliar nutrient deficiencies and thus affect the crown condition of sugarbushes in northern Vermont.

scholarly journals Forty-Eight Years of Forest Succession: Tree Species Change across Four Forest Types in Mid-Missouri

Forests ◽  
2018 ◽  
Vol 9 (10) ◽  
pp. 633 ◽  
Author(s):  
Benjamin O. Knapp ◽  
Stephen G. Pallardy
Keyword(s):  
Sugar Maple ◽  
Forest Succession ◽  
Basal Area ◽  
Juniperus Virginiana ◽  
Quercus Alba ◽  
Eastern United States ◽  
Forest Types ◽  
Eastern Redcedar ◽  
White Oak ◽  
Importance Value

In the central and eastern United States, many forest ecosystems have undergone recent shifts in composition and structure that may conflict with contemporary management objectives. Long-term forest inventory data were used to determine patterns of forest succession over a 48-year period for four forest types in mid-Missouri: bottomlands, dry ridge and slope, glade-like, and mesic slopes. All forest types increased in stand basal area and overstory quadratic mean diameter through time, with concomitant decreases in the number of midstory trees. Sugar maple (Acer saccharum Marshall) increased in importance value on dry ridge and slope and mesic slope forest types, largely due to the accumulation of trees in smaller diameter classes. White oak (Quercus alba L.) increased in overstory basal area in dry ridge and slope plots through the duration of the study, whereas black oak (Quercus velutina Lam.) and Shumard oak (Quercus shumardii Buckley) decreased in overstory density and basal area through time. Oak stems were nearly absent from the midstory across forest types in the recent sampling, suggesting future challenges for maintaining oak-dominated canopies following attrition of canopy trees through time on upland forest types. In glade-like plots, eastern redcedar (Juniperus virginiana L.) increased in both overstory density and basal area through time, and Shumard oak decreased in density. The importance value of chinkapin oak (Quercus muehlenbergii Engelm.) in the overstory decreased through time in glade-like plots, largely due to the increase in density of eastern redcedar rather than the loss of chinkapin oak from the overstory. The patterns of succession in this forest landscape of mid-Missouri suggest that forest management may be needed to address two common contemporary concerns: (1) the need for increasing oak advance reproduction and recruitment to maintain oak as a canopy species; and (2) reducing eastern redcedar encroachment for glade restoration and management.

Acid rain and soils of the Adirondacks. III. Rates of soil acidification in a montane spruce–fir forest at Whiteface Mountain, New York

1994 ◽  
Vol 24 (4) ◽  
pp. 663-669 ◽  
Author(s):  
A.H. Johnson ◽  
A.J. Friedland ◽  
E.K. Miller ◽  
T.G. Siccama
Keyword(s):  
New York ◽  
Soil Acidification ◽  
Forest Floor ◽  
Base Cations ◽  
Base Cation ◽  
Mineral Weathering ◽  
Published Data ◽  
Whiteface Mountain ◽  
The Impact ◽  
Loss Rates

To assess the impact of atmospheric deposition on soil acidification and base cation supplies in montane spruce–fir forest soils at Whiteface Mountain, New York, base cation and proton fluxes were determined for organic and mineral horizons from measurements made at four stands (1020–1090 m above sea level) over a 4-year period. Our best estimates indicate an annual accumulation of H+ and a net loss of base cations from the forest floor of about 0.71 kmolc/ha, a 2.8% per year loss of the total forest floor base cation pool. This high rate of acidification is attributable to base cation leaching by sulfate and organic anions, and uptake by living biomass. From 1986 to 1990, the annual net loss rate of forest floor Ca, the most abundant base cation, was several times greater than historical loss rates as determined by 50-year comparisons of forest floor Ca in nearly identical forests of the Adirondack High Peaks region. Published data on long-term trends in Ca deposition in the U.S. Northeast suggest that the difference between historical and current net loss rates of forest floor Ca may be due to sharply reduced atmospheric inputs of Ca after about 1970, exacerbated by sulfate leaching. In mineral horizons where the total base cation pool (mostly mineral bound) is very large, the net losses of base cations were substantially lower and in the range where losses due to leaching and uptake can be countered by mineral weathering.

scholarly journals Comment on “Present-day expansion of American beech in northeastern hardwood forests: Does soil base status matter?”Appears in Can. J. For. Res. 39: 2273–2282 (2009).

2011 ◽  
Vol 41 (3) ◽  
pp. 649-653 ◽  
Author(s):  
Christian Messier ◽  
Nicolas Bélanger ◽  
Jacques Brisson ◽  
Martin J. Lechowicz ◽  
Dominique Gravel
Keyword(s):  
Acer Saccharum ◽  
Sugar Maple ◽  
Complex Dynamics ◽  
Base Cations ◽  
Base Cation ◽  
Hardwood Forests ◽  
Fagus Grandifolia ◽  
Soil Base ◽  
American Beech ◽  
Atmospheric Acid Deposition

In a recent rapid communication, Duchesne and Ouimet (2009. Can. J. For. Res. 39: 2273–2282) reported that the current expansion of American beech ( Fagus grandifolia Ehrh.) in Quebec is mainly caused by soil base cation depletion due to atmospheric acid deposition. They based their conclusions on an examination of the relationships between stem densities in the sapling and tree strata compared against canopy composition and the availability of base cations in 426 sample plots. Here in this comment, we raise some shortcomings with their study and provide a more prudent and complete perspective on the complex dynamics associated with fluctuations in American beech and sugar maple ( Acer saccharum Marsh.).

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