Northeastern forests are in a period of immense change. While forests are inherently dynamic ecosystems, a range of environmental challenges may cause unique and uncertain transformations within forests moving forward. How trees in northern forests respond to these environmental and anthropogenic changes remains uncertain; reductions and increases in the growth of various species and shifts in current species’ ranges may take place. I analyzed associations between tree growth (assessed using xylem increment cores) and a range of site, climate, and pollution deposition variables for seven major tree species in Vermont. First, I looked at red oak (Quercus rubra L.), a species that is projected to expand into the northern hardwood forest. Summer moisture metrics were consistently and positively associated with growth, while higher summer temperatures were often negatively associated with growth. Several pollution metrics were associated with reduced growth – a surprising result for a species not known to be sensitive to inputs of acid deposition. Second, I examined growth of three tree species emblematic of the northern hardwood forest: sugar maple (Acer saccharum Marsh), American beech (Fagus grandifolia Ehrh.), and yellow birch (Betula alleghaniensis Britton), plus a fourth species, red maple (Acer rubrum L.), whose abundance has increased within the region. Winter moisture (likely snow) was important for all species except for red maple, and either summer moisture (positively associated) or temperature (mostly negatively associated) variables were important for all species, with some differences in relationships based on the elevation or time period evaluated. Pollution metrics were also negatively associated with growth for all species except beech. Third, I studied correlations of growth and environmental parameters for two temperate conifers: eastern white pine (Pinus strobus L.) and eastern hemlock (Tsuga canadensis (L.) Carrière). For both species, growth was positively associated with warmer spring temperatures but negatively associated with summer temperatures. Negative relationships between pollution deposition and growth for white pine, and to a far lesser extent, eastern hemlock, were also detected. If growing seasons lengthen as projected, temperate conifers may be at a competitive advantage for increased growth if changes in summer temperature and moisture regimes do not add excessive stress that offset possible increases in spring growth. These three studies highlight the importance of considering the distinct seasonal projections for moisture availability and temperature when evaluating the likely growth trajectories of these keystone species.

Thesis (M.S.) in Resource Utilitization--University of Maine, 2002. / Includes vita. Includes bibliographical references (leaves 39-40).

Thesis (M.Sc.)--York University, 2005. Graduate Programme in Biology. / Typescript. Includes bibliographical references (leaves 70-75). Also available on the Internet. MODE OF ACCESS via web browser by entering the following URL: http://gateway.proquest.com/openurl?url%5Fver=Z39.88-2004&res%5Fdat=xri:pqdiss &rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:MR11819

We examine the role of forest blowdown in lake acidification. Our approach combines geographic information systems (GIS) and digital remote sensing with traditional field methods. The methods of analysis consist of direct observation, interpretation of satellite imagery and aerial photographs, and statistical comparison of two geographical distributions-one representing forest blowdown and another representing lake chemistry. Spatial and temporal associations between surface water pH and landscape disturbance are strong and consistent in the Adirondack Mountains of New York. In 43 Adirondack Mountain watersheds, lake pH is associated with the percentage of the watershed area blown down and with hydrogen ion deposition (Spearman rank correlation coefficients of -0.67 and -0.73, respectively). Evidence of a temporal association is found at Big Moose Lake and Jerseyfield Lake in New York and the Lygners Vider Plateau of Sweden. We conclude that forest blowdown facilitates the acidification of some lakes by altering hydrologic pathways so that waters (previously acidified by acid deposition and/or other sources) do not experience the neutralization normally available through contact with subsurface soils and bedrock. Increased pipeflow is suggested as a mechanism that may link the biogeochemical impacts of forest blowdown to lake chemistry.

A study was conducted in 2006 to investigate the long-term effects of air pollution on soil properties in the vicinity of the Arnot power station, Mpumalanga, South Africa. Fifteen sites were re-sampled and the soil chemical properties compared to baseline data gathered in 1996, resulting in a ten year period after which changes in soil properties were investigated. A spatial gradient was incorporated into the study in order to better understand the deposition of pollutants with increasing distance from the power station. The study indicates that long-term acidic deposition has led to detectable changes in soil chemical properties. Three chemical properties, namely the concentrations of calcium and magnesium in both the topsoils and the subsoils, as well as the effective cation exchange capacity in the subsoils showed a significant increase since 1996. However, five soil chemical properties, namely soil pH (K2SO4), the concentration of hydrogen and aluminium and total sulphur in both the topsoils and the subsoils, as well as extractable sulphate in the topsoils and soluble sulphate in the subsoils, all show that the soils have become more acidic over the ten years. The acidic components in the soil override the basic components, as shown by the ratio of basic cations to acidic cations in the soils. The spatial gradient generally indicates that at approximately 8 km from the power station, there is a decrease in the concentration of acidic soil properties and one explanation for this may be a reduction in the acidic components of atmospheric deposition at this site. However, this needs further investigation. Two significant relationships with distance were found, namely a significant negative relationship with soluble sulphate and a significant positive relationship with acid neutralising capacity. This research will form part of a database for other long-term monitoring programmes and will allow data to be compared to other data from this area of research. It will also provide information to important industry leaders such as Eskom.

This thesis reports an investigation into methods of determining the long term deposition field for atmospheric aerosols in areas of complex topography using the soil inventories of atmospherically derived radionuclides. Measurements of the radionuclides ²¹⁰Pb, ¹³⁷Cs, ¹³⁴Cs and ⁷Be in vegetation and soil have been made at five mountain locations in northern Britain. A description of the field sampling procedure, sample processing and y-ray analysis is given. Loss-on-ignition experiments to determine the organic fraction of sampled soils were also conducted on selected samples. The presence of frequent low level cloud shrouding mountain tops in the uplands of northern and western Britain leads to enhanced precipitation and also deposition of the major acidic ions, eg SO₃²⁻ and N0₃, due to the washout of the low level cloud by falling rain ('seeder-feeder scavenging') and also the direct deposition of cloud droplets ('occult deposition'). It is important to quantify the inputs of acidic deposition in these acid sensitive regions and direct measurements present many logistical problems. The radionuclide ²¹⁰Pb is attached to the same sub-micron aerosol size range in the atmosphere as the major acidic ions and following deposition attaches very strongly to organic matter in soils. In this study the soil inventory of atmospherically derived ²¹⁰Pb is used as a tracer of the deposition of acidic ions. As the half-life of ²¹⁰Pb is 22.3 years the soil inventory of ²¹⁰Pb(atmos), at a site undisturbed for - 100 years, represents deposition integrated over several decades. Initial sampling took place at the Merrick, an isolated mountain close to the coast in southwest Scotland, to test and develop the technique. Measurements showed the ²¹⁰Pb(atmos) inventory to increase with altitude at a greater rate than precipitation. Sampling at Great Dun Fell in Cumbria enabled the measured radionuclide inventories to be compared with detailed measurements of the variation of the wet deposition pattern with altitude, and also with a model of sulphate deposition. Close correspondence was found between the ²¹⁰Pb deposition profile and the deposition pattern, with altitude, for the major acidic ions. The three mountains Ben Cruachan, Beinn Dorain and Ben Lawers lie along an 80 km transect running roughly west to east from the western coast into the central Highlands. Sampling at these three mountains has yielded information on the change in the wet deposition field with distance inland. The measurements suggest that deposition of ²¹⁰Pb decreases, with distance from the western coast, at a greater rate than does precipitation. The soil inventory of ²¹⁰Pb(atmos) increases with altitude at a greater rate than rainfall at 4 of the 5 mountains. The results show that, around summits, on average, the concentration of ²¹⁰Pb in low level cloud is a factor of - 2 greater than in the frontal ('seeder') rain falling from higher altitude. This finding is in good agreement with detailed wet deposition measurements. The ²¹⁰Pb measurements are important in themselves as they help define the global and UK ²¹⁰Pb budget. From measurements made at 65 individual sites the mean ²¹⁰Pb(atmos) inventory is 0.44 ± 0.03 Bq cm⁻², with the mean of the average annual rainfall being 2,060 ± 70 mm yr⁻¹. These figures correspond to a mean concentration of ²¹⁰Pb in rainfall of 66 mBql⁻¹. The ¹³⁷Cs inventory has been separated into the fraction originating from nuclear weapons testing, ¹³⁷Cs(bomb), and the fraction due to the Chernobyl accident, ¹³⁷Cs(Chern). The measured ¹³⁷Cs(bomb) inventory ranges from a mean of 3,300 Bq m⁻² at Ben Lawers to 5,200 Bq m⁻² at Beinn Dorain. The ¹³⁷Cs(Chern) inventory is highly variable between locations ranging from a mean of 440 Bq m⁻² at Great Dun Fell to 14,900 Bqm⁻² at Ben Lawers reflecting the patchy nature of deposition, due largely to convective storms, during the passage of the radioactive plume. The radionuclide ¹³⁷Cs is shown to be relatively mobile in the organic soils which characterise the study areas. The cosmogenic radionuclide ⁷Be was measured in samples collected from the Merrick on 26th Oct 1988. The mean inventory was 0.039 Bq cm⁻², being associated with vegetation and the top few cm of the soil profile.

Thesis (M.S.)--West Virginia University, 2009. / Title from document title page. Document formatted into pages; contains vii, 119 p. : ill. (some col.). Includes abstract. Includes bibliographical references.

Two studies were conducted to assess physiological responses of declining sugar maple (Acer saccharum Marsh.) in southern Quebec to wet acidic precipitation and increased soil fertility. Leaves of sugar maple were relatively acidic, had low external neutralization capacity (ENC = 5.1 $ mu$equiv. H$ sp{+} rm g sp{-1}$) and buffering capacity index (BCI = 103 $ mu$equiv. H$ sp{+} rm g sp{-1}$), and higher ENC/BCI compared to three other tree species. Deciduous species showed a higher BCI and a lower ENC in August. Our results suggest that sugar maple may be relatively sensitive to wet acidic deposition and that leaf buffering capacity is related to photosynthesis potential and seasonal change in foliar Ca concentration. Foliar analyses revealed that fertilization with a mixture of K, Ca, and Mg had significant effects on leaf concentrations of K, free amino acids (FAA) and the ratios of N to K, and FAA to N after two growing seasons. Our results suggest that base cation fertilization improved the N and K status of sugar maple and that leaf carbon partitioning appeared to be more dynamic in fertilized trees.

Thesis (M.S.)--West Virginia University, 2008. / Title from document title page. Document formatted into pages; contains vi, 131 p. : ill. (some col.). Includes abstract. Includes bibliographical references.

Thesis (Ph. D.)--West Virginia University, 2008. / Title from document title page. Document formatted into pages; contains xiv, 258 p. : ill., maps. Includes abstract. Includes bibliographical references.