Decomposition, litter fall, and forest floor nutrient dynamics in relation to fire in eastern Ontario jack pine ecosystems

1987 ◽  
Vol 17 (12) ◽  
pp. 1496-1506 ◽  
Author(s):  
M. G. Weber
Keyword(s):  
Organic Matter ◽  
Old Age ◽  
Forest Floor ◽  
Nutrient Dynamics ◽  
Jack Pine ◽  
Litter Fall ◽  
Turnover Rates ◽  
Equilibrium Conditions ◽  
Age Class ◽  
Eastern Ontario

Decomposition, litter fall, and nutrient and organic matter turnover rates were determined in five eastern Ontario jack pine (Pinusbanksiana Lamb.) stands having various burning histories, including wildfire. The stands included a 65-year-old age-class (stand No. 1), two stands within this age-class that were treated with nonlethal understorey fires in 1962 and 1963 (stand Nos. 2 and 3, respectively), a 21-year-old age-class (stand No. 4), and an 8-year-old age-class (stand No. 5) created by experimental burning plots within the 21-year-old age-class. Overstorey and understorey litter decomposition was assessed separately using the litterbag (1-mm mesh size) technique over a 2-year period. Overstorey litter weight loss did not vary among stands and understorey litter lost significantly more weight (P < 0.05) in the older age-classes (stands 1,2, and 3) compared with the younger stands (stands 4 and 5). Litterbag nutrient dynamics between overstorey and understorey were significantly different (P < 0.05) for P, K, and Cain all stands. Magnesium and N dynamics were the same in both litter types on all treatments, as was Fe, except in the 65-year-old stand where significantly more Fe was accumulated in understorey litter (P < 0.04) at the end of the litterbag exposure period. Three-year averages of annual litter fall ranged from 119 kg•ha−1•year−1 in the 8-year-old age-class to 4182 kg•ha−1•year−1 in the older stands. Nutrient inputs through litter fall reflect the developmental stage occupied by the younger stands along a continuum leading to equilibrium conditions of the 65-year-old age-class. Forest floor nutrient and organic matter residence times (or annual fractional turnover) were longest (least amount cycled) in the 8-year-old stand (57.6 years for organic matter), indicating harsh environmental controls over nutrient dynamics. Recovery for the 21-year-old age-class to turnover rates approaching equilibrium conditions (10-year residence time for organic matter) was rapid, demonstrating ecosystem stability in its interaction with fire. Detrimental effects on ecosystem processes can be expected if a stand-replacing fire recurs during early stages of jack pine ecosystem development.

scholarly journals Nutrient Dynamics in an Avicennia marina (Forsk.) Vierh., Mangrove Forest in Vamleshwar, Gujarat, India

2011 ◽  
Vol 3 (1) ◽  
pp. 51-56 ◽  
Author(s):  
Isaiah Nirmal KUMAR ◽  
Poliyaparambil Ravi SAJISH ◽  
Rita Nirmal KUMAR ◽  
George BASIL ◽  
Viyol SHAILENDRA
Keyword(s):  
Mangrove Forest ◽  
Nutrient Dynamics ◽  
Tree Height ◽  
Nutrient Budget ◽  
Avicennia Marina ◽  
Fall Rate ◽  
Litter Fall ◽  
Turnover Rates ◽  
Nutrient Use ◽  
One Year

The study was carried out to determine the nutrient budget of plants, sediments and nutrient dynamics in an Avicennia marina (Forsk.) Vierh., dominated forest in Vamleshwar near Narmada estuary, West Coast of Gujarat for a period of one year from November 2008 to October 2009. The average tree height of the mangrove is 1.5 to 2 m without much vertical stratification. Allometric methodology was used to measure the biomass, and yield a figure of 86.47 t ha-1 and the litter fall rate amounted to 2.9 t ha-1. Nutrient stocks of N, P and K in this mangrove were 137.05, 14.38 and 241.29 kg ha-1, with an annual accumulation of 55.74, 12.38 and 83.94 kg ha-1, and an annual return of 51.30, 10.83 and 13.52 kg ha-1, respectively, in the form of litter. The annual uptake for N, P and K were 61.04, 14.28 and 97.46 kg ha-1, and turnover rates of N, P and K were estimated at 3, 6 and 14 years, respectively, for the study period. Flow coefficients, which reveal the dynamic processes of nutrients between mangrove plants and sediments, are also explained. The present study concluded that the A. marina dominated mangrove plantation is more efficient in nutrient use and conservation.

Leaf nutrient dynamics of two tree species and litter nutrient content in Southern Bakundu Forest Reserve, Cameroon

1997 ◽  
Vol 13 (1) ◽  
pp. 1-15 ◽  
Author(s):  
Nicholas C. Songwe ◽  
F. E. Fasehun ◽  
D. U. U. Okali
Keyword(s):  
Forest Floor ◽  
Nutrient Dynamics ◽  
Leaf Age ◽  
Magnesium Concentration ◽  
Nutrient Concentrations ◽  
Leaf Fall ◽  
Litter Fall ◽  
Terminalia Superba ◽  
Phosphorus And Potassium ◽  
Nitrogen Phosphorus

ABSTRACTThe variations in macronutrient concentrations of the leaves of Terminalia superba and Pycanthus angolensis were studied and the concentrations of nutrients in leaves before abscission were compared with those after abscission. The amounts of nutrients returned to the forest floor were also computed from litter fall data at the start of maximum annual fall in the Reserve. With the exception of potassium in Pycanthus angolensis, there were significant variations in the nutrient concentrations of the two species with the time of year. With increasing leaf age the concentration of nitrogen, phosphorus, potassium and magnesium declined in Terminalia superba while magnesium concentration decreased in Pycanthus angolensis leaves. Furthermore, calcium showed an increasing concentration in Terminalia superba with increase in leaf age. The concentrations of nitrogen, phosphorus and potassium decreased before leaf fall. Estimated losses in nitrogen phosphorus and potassium before abscission were 44, 53 and 50%, respectively, whereas generally there was an increase (40%) in the concentration of calcium at leaf fall. Magnesium did not follow a definite pattern. The return of calcium through litter fall to the forest floor was the greatest of all the major elements. The distribution and variation of foliar nutrient concentrations in the leaves of Terminalia superba and Pycanthus angolensis and the importance of the amount of litter and the concentration of the various nutrients in the influencing soil fertility are discussed.

Annual Macroelement Transfer From PinusBanksiana Lamb. Forest to Soil

1974 ◽  
Vol 4 (4) ◽  
pp. 470-476 ◽  
Author(s):  
Neil W. Foster
Keyword(s):  
Forest Floor ◽  
Nutrient Content ◽  
Jack Pine ◽  
Pine Forest ◽  
Ground Vegetation ◽  
Litter Fall ◽  
Northern Ontario ◽  
Glacial Outwash ◽  
Annual Total ◽  
Total Potassium

The annual amounts of N, P, K, Ca, and Mg in litter-fall, throughfall, and stemflow were measured in a 30-year-old jack pine (Pinusbanksiana Lamb.) stand on a coarse glacial outwash soil in northern Ontario. Litter from ground vegetation and from the pine overstory was estimated. The nutrient content of precipitation was measured and the quantity of nutrients in leaf wash determined.Tree litter was the most important source of N, P, Ca, and Mg for the forest floor (51–69% of the total depending on the element), whereas throughfall supplied most K (54% of the total). Ground vegetation litter contributed significant amounts of nutrients (7–23% of the total depending on the element) but stemflow added little (1–8% of the total). Potassium in throughfall was derived mainly from leaf wash whereas N, P, Ca, and Mg in throughfall were derived primarily from precipitation entering the ecosystem. This jack pine forest floor received an annual total of 30 kg/ha of N, 22 kg/ha of Ca, 19 kg/ha of K, 3 kg/ha of Mg, and 2 kg/ha of P from the processes studied. Most of the nutrients in these totals were returning to the forest floor from the vegetation.

Nutrient cycling in relation to decomposition and organic-matter quality in taiga ecosystems

1983 ◽  
Vol 13 (5) ◽  
pp. 795-817 ◽  
Author(s):  
P. W. Flanagan ◽  
K. Van Cleve
Keyword(s):  
Organic Matter ◽  
Nitrogen Content ◽  
Forest Floor ◽  
Fungal Biomass ◽  
Microbial Respiration ◽  
Black Spruce ◽  
Litter Fall ◽  
Substrate Quality ◽  
Respiration Rates ◽  
Forest Floors

A variety of evergreen and deciduous forests in the taiga of interior Alaska were studied over a 5-year period to examine how the chemical quality of forest-floor organic matter affected its rate of decomposition and mineral cycling within and outside the tree vegetation. Litterbag and respiration studies were used to monitor decomposition. Natural forest-floor substrates and others altered by addition of N, P, and K fertilizer and glucose as a carbon source were studied in the laboratory and field for rates of weight loss and O2 consumption. Forest floors differing in C/N ratios, including those deficient in N, were used to measure substrate quality influences on seedling growth, nutrient content, and tannin content. Microbial (bacteria and fungi) biomass was measured across a range of forest types along with pH, base saturation total pool sizes of N and P, and annual mineralization of organic matter per square metre. Under identical moisture and temperature conditions average respiration rates in evergreen forest-floor L, F, and H substrates were 1.8, 2.8, and 2.0 times less than in the corresponding deciduous forest horizons, respectively. Birch L and F horizons had respiration rates 11.5 times higher than the corresponding black spruce layers. Weight losses in birch L, F, and H horizons were 6, 3, and 2 times higher, respectively, than in the corresponding black spruce substrates. Substrates had a quality-dependent decay rate which did not change when they were relocated within or between sites indicating that measured field climatic differences were not as influential on decay rates as substrate quality components. Fungal biomass was significantly correlated with the quantity of organic matter in all sites (n = 15, r = 0.62) but correlations were better for deciduous (n = 9, r = 0.89), and evergreen (n = 6, r = 0.82) forests separately. Strong correlations exist also between grams of organic matter decayed per square metre per year and fungal biomass (n = 13, r = 0.86), and fungal biomass and grams of N and P mineralized per square metre per year (n = 14, r = 0.95) and (n = 11, r = 0.94, respectively). Seedlings on mineral-deficient substrates produced more tannins than the controls, and seedlings on substrates with widening C/N ratios had successively less tissue with lower N content, and proportionally more roots. Nitrogen content of litter fall in increasingly nitrogen-poor forest floors was correspondingly lower. Nitrogen content of litter fall on N rich forest floors and N fertilized forest floors was proportionately higher. Nitrogen withdrawal in leaves at senescence was inversely correlated with grams N mineralized per square metre per year in forest floors. Fertilization did not influence microbial processes in the field, though lab studies indicated a negative influence of NH4, P, and K on microbial respiration. Glucose added in the laboratory and field markedly increased forest-floor microbial respiration. In vitro glucose-induced increases in respiration were not influenced by addition of ammonium nitrate and were significantly depressed by addition of P and K. In the field, fertilization had no effect on either glucose-induced respiration or microbial biomass.

The effect of forest floor manipulation on nitrogen status and tree growth in an eastern Ontario jack pine ecosystem

1985 ◽  
Vol 15 (2) ◽  
pp. 313-318 ◽  
Author(s):  
M. G. Weber ◽  
I. R. Methven ◽  
C. E. Van Wagner
Keyword(s):  
Tree Growth ◽  
Forest Floor ◽  
Mineral Soil ◽  
Complete Removal ◽  
Jack Pine ◽  
Site Quality ◽  
Stand Development ◽  
Untreated Plot ◽  
Soil Effects ◽  
Eastern Ontario

Four forest floor manipulation treatments were applied to an eastern Ontario jack pine (Pinusbanksiana Lamb.) ecosystem. These included a one-time complete removal of the forest floor to mineral soil; annual removal of the total forest floor to mineral soil; one-time removal of the forest floor, ashing of the material, and broadcast spreading of the ash onto exposed mineral soil; and an untreated control. Eight years after treatment radial tree growth on the treated plots showed a 30% reduction compared with the untreated plot. Annual removal of the forest floor caused most severe nitrogen depletion in jack pine foliage, forest floor, and mineral soil. Effects of one-time removal and burning treatments were less severe, but significant. Any interference with the normal buildup of the forest floor during stand development should be avoided if site quality is to be maintained for tree growth.

Addition of organic matter and elements to the forest floor of an old-growth Acersaccharum forest in the annual litter fall

1991 ◽  
Vol 21 (4) ◽  
pp. 462-468 ◽  
Author(s):  
I. K. Morrison
Keyword(s):  
Organic Matter ◽  
Forest Floor ◽  
Base Cations ◽  
Dry Weight ◽  
Turnover Time ◽  
Residence Times ◽  
Litter Fall ◽  
Old Growth ◽  
Northern Ontario ◽  
Element Transfer

Litter fall and its content of N, P, K, Ca, Mg, S, Fe, Mn, Zn, and Cu were measured monthly over a 5-year period in an old-growth Acersaccharum Marsh, stand on a till site in central northern Ontario. Determined were the following: the amount, and the temporal and spatial distributions, of organic matter and elements deposited annually in the different litter fractions; the proportion of elements conserved within the tree phytomass through retranslocation versus that shed in the annual litter fall; and the residence time of litter-transported elements in the forest floor. Element transfer through the annual litter fall was also compared with that by other vectors of transport to the forest floor. Over the study period, total litter fall averaged 3730 kg•ha−1•year−1 (dry weight), with 78% consisting of leaves, 8% of flowers and fruits, and the remaining 14% mainly of twigs, branches, and bark slough. Annual element depositions (kg•ha−1) averaged as follows: N, 40.6; P, 1.8; K, 9.1; Ca, 37.6; Mg, 3.9; S, 3.0; Fe, 0.57; Mn, 2.67; Zn, 0.28; and Cu, 0.03. Turnover time of the forest floor was calculated as 7.4 years. Residence times (years) of elements in the forest floor were as follows: N, 18.3; P, 18.3; K, 1.5; Ca, 6.1; Mg, 6.8; S, 5.1; Fe, 257.2; Mn, 4.8; Zn, 18.1; and Cu, 5.8. Although the turnover time of forest-floor organic matter did not differ appreciably from values reported for A. saccharum forests elsewhere, residence times for elements suggested somewhat slower cycling, probably as a result of reduced uptake related to the advanced age of the stand. Potassium, followed by S, P, and N, were all conserved to a high degree by A. saccharum trees through retranslocation to the tree's perennial parts prior to leaf fall; Cu, Mn, and Mg were conserved to a lesser degree; Zn, Ca, and Fe were conserved very little. In comparing the leaching loss of elements from foliage with quantities conserved through retranslocation and quantities shed in the annual litter fall, the relative orders of magnitude do not give cause for concern that A. saccharum trees risk appreciable leaching losses of base cations, including K, from foliage as a result of acidified precipitation, at least at levels experienced in central northern Ontario during the early 1980s.

Seasonal Nutrient Dynamics of Litter in a Subtropical Eucalypt Forest, North Stradbroke Island

1977 ◽  
Vol 25 (1) ◽  
pp. 47
Author(s):  
RW Rogers ◽  
WE Westman
Keyword(s):  
Half Life ◽  
Forest Floor ◽  
Nutrient Dynamics ◽  
Early Summer ◽  
Litter Production ◽  
Litter Fall ◽  
Nutrient Inputs ◽  
Sodium Potassium ◽  
Nutrient Pools ◽  
Eucalypt Forest

The plant components and chemical composition of litter fall and the litter layer in a forest growing on deep, nutrient-poor sands were examined on North Stradbroke Island, south-eastern Queensland. The seasonal distribution of litter fall was examined over a 26-month period. While the total litter fall was greatest during summer months, the dominant tree species differed in their individual patterns of litter fall. Eucalyptus signata showed a single summer peak for leaf fall while E. umbra exhibited one peak in early summer and another in autumn. The possibility is discussed that these and other temporal differences are evolutionary expressions of niche differentiatibn to reduce competition between species in the ecosystem. The total litter fall averaged 640 g m-1 yr-1 and the accumulated forest floor mass totalled 2700 g m-2. Total nutrient pools and nutrient inputs in litter fall are presented. A litter half-life of 2.9 years is estimated, a figure close to the half-life of most of the nutrients in the litter. Manganese appears to be markedly concentrated in eucalypt leaves before they fall. Only sodium, potassium, copper and chloride appear to be leached easily from leaves slashed from trees and left on the forest floor. Patterns of litter production and decay in this subtropical forest fit within trends extrapolated from temperate Eucalyptus-dominated communities studied to date.

Effects of bigleaf maple on soils in Douglas-fir forests

1990 ◽  
Vol 20 (3) ◽  
pp. 259-266 ◽  
Author(s):  
Jeremy S. Fried ◽  
James R. Boyle ◽  
John C. Tappeiner II ◽  
Kermit Cromack Jr.
Keyword(s):  
Forest Floor ◽  
Mineral Soil ◽  
Nutrient Content ◽  
Douglas Fir ◽  
Organic Carbon Content ◽  
Coast Range ◽  
Litter Fall ◽  
Turnover Rates ◽  
Calcium Magnesium ◽  
Forest Floors

Soil chemical and physical properties, forest floor weights, nutrient content and turnover rates, and litter fall weights and nutrient content under bigleaf maple (Acermacrophyllum Pursh) and Douglas-fir (Pseudotsugamenziesii (Mirb.) Franco var. menziesii) were compared on five sites on the eastern margin of the Oregon Coast Range. Litter fall weight and nutrient content were significantly greater under maple on every site for every macronutrient and for most micronutrients. Forest floor biomass and nutrient content were extremely variable, much more so than litter fall, and there were no consistent differences between the two species. However, turnover rates for forest floor biomass and nutrients were significantly faster under maple for every nutrient at every site. Bulk density of mineral soil was also highly variable with significant differences at only two sites. Soil under maple was consistently higher in nitrogen, and less consistently, in potassium. There were no consistent trends in amounts of calcium, magnesium, or phosphorus. Soil organic carbon content under maple was significantly greater than under Douglas-fir on four of five sites. These differences may result from the more rapid turnover of forest floors under maple trees.

Nutrient dynamics in the litter fall and forest floor of an 18-year-old loblolly pine plantation

1986 ◽  
Vol 16 (5) ◽  
pp. 1109-1112 ◽  
Author(s):  
B. G. Lockaby ◽  
Jane Ellen Taylor-Boyd
Keyword(s):  
Steady State ◽  
Loblolly Pine ◽  
Forest Floor ◽  
Nutrient Dynamics ◽  
Sampling Period ◽  
Dry Weight ◽  
Litter Fall ◽  
Pine Plantation ◽  
Rapid Decomposition ◽  
North Louisiana

Dry weight and N, P, K, Ca, and Mg concentrations were monitored in the litter fall and forest floor of a loblolly pine (Pinustaeda) plantation in north Louisiana for 2 years. Dry weights of both litter fall and forest floor were statistically stable during the sampling period, possibly indicating steady-state conditions. A comparison of litter fall with forest floor weights indicated rapid decomposition (floor turnover = 1.5 years) relative to that of other loblolly pine systems.

Selected Parameters of Fire Behavior and Pinus banksiana Lamb. Regeneration in Eastern Ontario

1987 ◽  
Vol 63 (5) ◽  
pp. 340-346 ◽  
Author(s):  
M. G. Weber ◽  
C. E. Van Wagner ◽  
Monte Hummel
Keyword(s):  
Forest Floor ◽  
Pinus Banksiana ◽  
Tree Mortality ◽  
Mineral Soil ◽  
Fire Behavior ◽  
Jack Pine ◽  
Fire Intensity ◽  
Seedling Height ◽  
Ecological Requirements ◽  
Eastern Ontario

Fire behavior variables were quantified in eastern Ontario jack pine (Pinus banksiana Lamb.) ecosystems and used to interpret observed fire impacts and effects. A series of seven fires, ranging in frontal fire intensity from 70 to 17 000 W/m, were documented. Forest floor moisture content prior to burning was negatively correlated with weight of forest floor consumed per unit area (r2 = 0.97) and per cent mineral soil bared (r2 = 0.95). Frontal fire intensity was positively correlated with per cent tree mortality (r2 = 0.98) and mean height of char (r2 = 0.76). Frontal fire intensities of 17 000 kW/m resulted in seedling numbers of 30 000 to over 50 000 ha−1 considered to be more than adequate for establishing the next generation of crop trees. Jack pine mean seedling height, 13 to 16 years after fire, was also positively correlated with frontal fire intensity (r2 = 0.82), ranging from 0.5 to 3.8 m on lowest and highest intensity burns, respectively. Similar relationships were found when seedling height was regressed against per cent tree mortality (r2 = 0.62) and forest floor consumption (r2 = 0.79).Results are discussed in terms of ecological requirements of the species, particularly during the regeneration phase, and it is concluded that quantification of fire behavior observations is mandatory if burning conditions are to be understood and/or duplicated by the land manager for the attainment of a given forest management objective.

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