Ecology of Red Maple Swamps in the Glaciated Northeast: A ...
Ecology of Red Maple Swamps in the Glaciated Northeast: A ... Ecology of Red Maple Swamps in the Glaciated Northeast: A ...
Surface-water depression wetland Surface-water slope wetland Precip. I ET Precip. ET . .:.. - below wetland . ' . , . .' . . ' Groundwater depression wetland Groundwater slope wetland Precip. ET Precip. Overland ET .. . ' '.-:'- when water table drops below wetland Fig. 22 Inland wetland hydrologic classes (based on Novitzki 1979a, 1982). The shaded area is the groundwater zone; ita upper surface is the water table.
y e~rr~mtrtm~~,irzst ion. Cat~t,inulrxg &yc>mlc.iwakr irr- events, lotst rur~ollnts are fikf31y to be negligible, Elrtw rrrtry cvrtlmb wci(ltxtlrt wdr*r ICTW~S to rim* in Uub frdl, eqewiitU y wlzem wetliuld saih have formed over w1.ic.n uvti~xitmtrwltintticrtilcit~lirlrn, ofan in exm.w of clew idgexncexlt till depits. Where such deposits dinx* ~>nwipitrrt.i
- Page 2 and 3: Technical IIbpg~rt Series U.S. Fish
- Page 5 and 6: Preface In many areas of the glacia
- Page 7 and 8: Acer rubrum (red maple) diagnostic
- Page 9 and 10: Zone 111 . St . Lawrence Valley and
- Page 11 and 12: Fig . 3.7. Red maple swap with unde
- Page 13 and 14: Table 4.5. Flood tolerance of trees
- Page 15 and 16: Chapter I. Introduction Wetland kbr
- Page 17 and 18: Regional Setting throughout the gla
- Page 19 and 20: C-J Spruce-Fa Beech-Birch-Maple Mit
- Page 21 and 22: Fig. 1.4. The range of red maple (a
- Page 23 and 24: ~ b 1.5, h fircort~ of Wet landc Ir
- Page 25 and 26: Fig. 22. &~lrit~ve Irtndtici~pe yos
- Page 27: egional groundwakr table by the roc
- Page 31 and 32: inflow^ Outflows OF SWQ SWI Fig. 25
- Page 33 and 34: Fig, 23.6,Soasonally flmded red map
- Page 35 and 36: Fig. 27. Water levels in six mode I
- Page 37 and 38: The duration of soil saturation has
- Page 39 and 40: Organic soils are always very poorl
- Page 41 and 42: Chapter 3. The Plant Community The
- Page 43 and 44: .dar02f 'B Xi? s%u?mma -?sway+xqq p
- Page 47 and 48: Community S tructare Red maple swam
- Page 49 and 50: suggesta a strong correlation betwe
- Page 51 and 52: Table 3.2. Stmtuml chumcteristics o
- Page 53 and 54: Table 3.3. Continued. "- -- - Speci
- Page 55 and 56: Table __ 3.3. _ Continued ._.lll.__
- Page 57 and 58: Table 3.3. Continued. . * - __.. ^.
- Page 59 and 60: Zone I II III TV C" Drppnmriad* sp.
- Page 61 and 62: on Long Island, pin oak, swamp whit
- Page 63 and 64: fern moea (?ki.c&inz &limfulum), an
- Page 65 and 66: countered (Table 3.3). The herb lay
- Page 67 and 68: ~akareous Seepage Swamps England si
- Page 69 and 70: and globeflower are. listed in four
- Page 71 and 72: was the most likely reason for diff
- Page 73 and 74: kvei fluctuation during the gmwing
- Page 75 and 76: Table 4.2. .Rektit.e ~bmchnce w Q)
- Page 77 and 78: difficuit to delineate in many inst
y e~rr~mtrtm~~,irzst ion. Cat~t,<strong>in</strong>ulrxg &yc>mlc.iwakr irr- events, lotst rur~ollnts are fikf31y to be negligible,<br />
Elrtw rrrtry cvrtlmb wci(ltxtlrt wdr*r ICTW~S to rim* <strong>in</strong> Uub frdl, eqewiitU y wlzem wetliuld saih have formed over<br />
w1.ic.n uvti~xitmtrwlt<strong>in</strong>tticrtilcit~lirlrn, <strong>of</strong>an <strong>in</strong> exm.w <strong>of</strong> clew idgexncexlt till depits. Where such deposits<br />
d<strong>in</strong>x* ~>nwipitrrt.i
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