PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest

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Dice, Steven F . 1970. The biomass and nutrient flux in a second growth Douglas-fir ecosystem (a study in quantitative ecology) . 53 p. Ph.D. thesis on file, Univ . Wash . , Seattle . Greig-Smith, P . 1964 . Quantitative plan t ecology. Ed. 2, 256 p., illus . Washington , D.C . : Butterworths . Groman, William A ., and Alan B. Berg . 1971 . Optical dendrometer measurement of increment characteristics on the boles of Douglas-fir in thinned and unthinned stands. Northwest Sci . 45(3) : 171-177 . and H. H . Allen . 1971. A technique for quantifying forest stands fo r management evaluations . U .S . Army Eng . Waterways Exp . Stn. Tech . Rep . M-71-9 , 29 p ., illus . West, H . W ., R . R . Friesz, E . A. Dardeau, Jr . , and others . 1971 . Environmental characterization of munitions test sites : Vol. 1 , Techniques and analysis of data . U .S. Army Eng. Waterways Exp . Stn. Tech. Rep . M-71-3, 31 p ., illus . 176
Proceedings-Research on Coniferous <strong>Forest</strong> Ecosystems-A symposium . Bellingham, Washington-March 23-24, 197 2 Estimates of biomass and fixed nitrogen of epiphytes from old growth Douglas fir Lawrence H . Pike and Diane M . Tracy Department of Botan y Oregon State Universit y Corvallis, Orego n Martha A . Sherwoo d Department of Biology University of Orego n Eugene, Orego n Diane Nielse n Division of Ecology and Systematic s Cornell University Ithaca, New Yor k bstract - Epiphytes are sampled concurrently with measurements of surface area of trunk and branch systems of old-growth Douglas-fir (Pseudotsuga menziesii) . Crude predictions of epiphyte biomass in branch systems are corrected by more detailed sampling of a subset of branch systems. Nitrogen analyses enable conversion of epiphyte biomass to the total amount of nitrogen present in the epiphytes. Introduction Epiphytic lichens and mosses are a conspicuous component of forest ecosystems in th e Pacific Northwest . Because of their ability t o concentrate materials from the environment and the ability of some of them to fi x atmospheric nitrogen, their importance i n nutrient cycling within the system may be greater than their contribution to total biomass would suggest . In old-growth Douglas-fir forests, epiphyt e biomass is expected to be in a steady state ; epiphyte growth is balanced by litterfall, in situ decomposition, and consumption b y herbivores. Annual turnover of epiphytic lichens varies from 5 to 25 percent (Edward s et al. 1960, Pike 1971) . Epiphyte-fixed nitrogen accounts, at least in part, for the nitrogen needed for th e growth of these epiphytes, and may represen t a significant input to the forest ecosystem . Nitrogen is added to water flowing over tre e surfaces through decomposition of epiphyte s and leakage from nitrogen-fixing epiphytes , and enters the soil from the epiphyte syste m via throughfall, stemflow, and litterfall . Measurements of biomass are necessary t o relate process studies of epiphytes to thei r contribution to forest mineral cycles on an ecosystem level . Estimating epiphyte biomass by felling and sampling selected trees is neither possible nor desirable in old-growt h Douglas-fir forests (where trees may approac h 100 m in height) because such felling i s destructive, not only of the host tree, but also of the epiphytes one wishes to study . This paper outlines the methods and give s 177
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PE EIE[R-Rg RESEARC H O N CONIFEROU
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Research on Coniferous Forest Ecosy
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Contents SOME BROADER VIEWS OF BIOM
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Page AQUATIC PROCESS STUDIES 279 St
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Proceedings-Research on Coniferous
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directly, to solution of major natu
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4. Nutritional adaptation to enviro
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where validation studies could be c
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have been developed . Prior to thei
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of gross production and respiration
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Figure 1 . Aerial photo of Findley
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Nutrient levels in stream and lake
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Acknowledgments The work reported i
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inputs into the lakes . Recent stud
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was slightly raised in 1902, the la
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climate, surrounding terrestrial en
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more similar than between the diffe
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The net rate of primary production
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community structure and energy flo
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est adapted organism vacillates bet
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U .S . Analysis of Ecosystems, Inte
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successful . Thus we can see modeli
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of the external quantities of S wou
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Figure 2 . The major subsystems of
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subsystems as objects . In addition
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several models together to form the
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The study areas are located at seve
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K m Figure 1 . Watershed 2, H . J.
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An alternative way of considering i
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Snowmelt A flow chart of the snow a
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d Gs Gr = (1 - Ki) d t By integrati
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Calibration of Parameter s In gener
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model being developed under the Con
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Usually, we are interested in the o
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LINEAR Y~(T) 2nd ORDER Y2 (T) 3rd O
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the watershed. The hydrologic model
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considered as part of another food
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PRIMARY PRRODUCTIO N ■ FOLIAGE CO
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Graham, S. A. 1952. Forest entomolo
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ful in regions with relatively unif
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epresents the basic linkages betwee
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Cleary and Waring 1969, Reed 1971,
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vation that species such as Brewer
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Table 3.-Predicted plant response i
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Walker, Reed, Scott, and Webb are c
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Water and Nutrien t Movement Throug
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Here v is the volume of water cross
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2 10 7100 .160 .220 .280 .340 .400
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.0500 .040 0 z .030 0 E L.) 0 .020
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ment of the flux of ions through th
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Table 2 .-Forest floor composition
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Table 5 .-Monthly amounts of litter
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Figure 2 illustrates how CO 2 produ
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Ballard, T. M. 1968 . Carbon dioxid
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2. How effectively are these chemic
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Table 2 .-Nutrient budget for disso
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Figure 1 . Water content of the sur
Page 121 and 122: 0.12_ _30 rn z 0 Q z w 0 z 0 0 z Q
Page 123 and 124: _3 0 . Outflow Concentration _ __ R
Page 125 and 126: 0.10_ 0.08 _ Pea k 0.04_ Concentrat
Page 127 and 128: 8J Calciu m 0 I I I I 0.25 0.50 0.7
Page 129 and 130: water is dominant because flowing w
Page 131 and 132: Proceedings-Research on Coniferous
Page 133 and 134: Table 1.-Characteristics of study p
Page 135 and 136: Z w 2 w J w 3 0 Table 2. Average to
Page 137 and 138: of the nitrogen was not determined.
Page 139 and 140: Table 6. Total kg per hectare per y
Page 141 and 142: through litterfall . More amounts o
Page 145 and 146: Figure 3. Two additional carabiners
Page 147 and 148: 1 1 Figure 11 . The climber places
Page 149 and 150: Figure 16. The spar in use. The sus
Page 151 and 152: in our example) and the running tot
Page 153 and 154: Dashed lines are dead branches . Th
Page 157 and 158: Table 1.-Transpiration rates, mean
Page 159 and 160: this case the slopes of activity-ti
Page 161 and 162: solve equation 2 for Tm since the f
Page 165 and 166: ing methods . Every point in the sa
Page 167 and 168: Patterns in Point Displacemen t Mea
Page 169 and 170: trees indicates that the coordinate
Page 171: data; there is no obvious explanati
Page 175 and 176: where C is the percentage cover by
Page 177 and 178: Table 1.-Epiphyte biomass on the tr
Page 179 and 180: NZ. 4 50 100 150 EPIPHYTE IMPORTANC
Page 181 and 182: Table 4.-Biomass estimates (kg) for
Page 183 and 184: watershed 10 (C . T. Dyrness, perso
Page 185 and 186: Table 1 .-Some population character
Page 187 and 188: Table 2 .-Annual litter fall in Col
Page 189 and 190: Table 4. Biomass and growth increme
Page 191 and 192: Table 6.-Annual turnover from certa
Page 193 and 194: Kiil, A. D. 1968. Weight of the fue
Page 195 and 196: condition differ) ; the turnover ra
Page 197 and 198: proportionally about the same for e
Page 199 and 200: Bird Studies The forest birds were
Page 201 and 202: Further Studies The data provided f
Page 203 and 204: Terrestrial Process Studies 209
Page 205 and 206: from theses. The principal processe
Page 207 and 208: Table 1 .-Saturating light intensit
Page 209 and 210: at least 0 .06 percent CO 2 . Howev
Page 211 and 212: Pharis et al. 1967). Again Helms (1
Page 213 and 214: Effects of Leaf Temperature an d Le
Page 215 and 216: Literature Cited Baule, H., and C.
Page 217 and 218: Lopushinsky, W . 1969. Stomatal clo
Page 221 and 222: Von Bertalanffy (1969) calls nonsum
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which may be of importance in model
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The first three terms of equation 1
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P = F+ R where F = net assimilation
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This function is asymptotic to zero
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The important interaction between l
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(3 = H/AE=yo$/De (3 ) where y is th
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0.4 0.2 v 0 0 w IX -0.2 I- cr -0.4
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Table L-Diurnal energy budget compo
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4 8 10 12 14 16 18 20 22 24 TIME, H
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1970. Evapotranspiration an d meteo
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may bias the results . Meteorologic
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7.4 ppm . The lysimeters at Coshoct
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Acknowledgments The work reported i
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extracted was determined by the wei
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I - 5 -l o -1 5 HPV 1 10 . 0 I . 6
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Table 1 .- Tukey's w Multiple Compa
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studies in conifers-a review . In J
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permeable to both CO 2 and water va
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insolation (1 cal cm 2 min-1 ) and
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Aquatic Process Studies 279
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stream environments (Krygier and Ha
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S, - 4ydrolo9i c S2 = I¢rr¢strIa
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ingestion variation between individ
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contribute to detrital compartment
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volume measurement, realizing that
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fer of the indicated carbon-14 trac
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18L LAKE WATER LIGH T 50m1 HOURLY D
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a function of time and space, (b) c
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Table 1.-Suggested criteria for jud
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Table 4.-Average C, N, and P conten
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during 1963 to 1967 and from Lake S
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greater than 7 .2:1 (16:1 by atoms)
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2 .0 1 .0 0 Si P-N N-Si P-Si P-N-Si
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detectable increase in concentratio
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in lakes . J. Ecol . 29 : 280-329 .
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Woodey 1970 ; Thorne, Reeves, and M
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targets are insonified several time
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This program will automatically cal
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The FOREST SERVICE et ; U :' S D pa
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