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09-24-2018 Council Packet
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09-24-2018 Council Packet
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rat method (1669 ± 748 versus 799 ± 379 g/m2 DW (x +SE, n <br />= 12, p< 0.01)), variability of the two methods was compara- <br />ble (116 versus 110% coefficient of variation). Thus, caution <br />is needed in comparing our results to other researcher's data <br />but our values indicate that the rake sampling method pro- <br />vides accurate comparisons among our sites. <br />After collection, plants were washed, roots were removed <br />and above ground shoots were dried to a constant weight at <br />60 C (after Engel 1990). Milfoil was separated from other <br />plants on the 3rd, 6th and 9th sampling date using the taxo- <br />nomic key of Fassett (1957). Dry weights were determined <br />for milfoil, and for all other plants combined, and percent- <br />age milfoil by weight was determined. <br />Dissolved oxygen, specific conductivity, and temperature <br />were measured on each sampling date at 0, 1, and 2 meters <br />depth and then averaged. Dissolved oxygen, specific conduc- <br />tivity and temperature were measured with Yellow Springs <br />Instruments (YSI) meters. Water clarity was measured on <br />each sampling date with a 20.3 cm Secchi disk in open water <br />at random locations within 5 meters of each experimental <br />plot. <br />To assess canopy density at the surface, we developed a <br />method using a Secchi disk (called a plant disk when used in <br />a weed bed). This disk was lowered into the weeds and the <br />depth at which the plant canopy obscured the disk was mea- <br />sured. This was done in both harvested and unharvested <br />areas from the 3rd to the 9th week. The disk was gently low- <br />ered <br />owered through the plant stems by moving the disk side to side <br />so that it did not push down surface mats, but rather slipped <br />underneath them. Plant surface cover was measured as the <br />ratio of Secchi disk to plant disk depth. When plant stems do <br />not obscure the plant disk at all the ratio of plant disk depth <br />to Secchi depth outside the weed bed (the plant canopy <br />04 104 <br />t <br />as <br />3 <br />13 <br />H <br />p 103 <br />L <br />Vl <br />a <br />0 <br />m <br />c <br />a <br />a <br />102 <br />0 <br />• Unharvested <br />v Harvested <br />R2=0.81 <br />T r <br />R =0.26 <br />3 4 5 6 7 8 9 10 <br />Weeks after harvest <br />JULY AUGUST SEPTEMBER <br />Figure 2. Plant biomass changes over time in harvested and unharvested <br />plots. Harvest done on July 3, 1990. Results presented as mean ± standard <br />error. <br />ratio) will be near 1.0 [this ratio may be slightly different <br />from 1.0 due to the effects macrophytes can have on phy- <br />toplankton production (Wetzel 1983) ] . <br />Sediment cores were collected in the 3 sub -divisions of <br />each plot 3, 6, and 9 weeks after harvest. Cores represented a <br />composite of the upper 15 cm of sediment. Forty grams were <br />sub -sampled from the cores for textural analysis using a <br />hydrometer (Klute 1986). An additional 20 grams of dried <br />material from each core were ashed at 545 C to determine <br />organic content (following Lillie and Barko 1990). <br />DATA ANALYSIS <br />Differences in plant biomass between harvested and <br />unharvested plots were analyzed with an ANOVA for each <br />sampling date (n= 30 for each date). Biomass data was aver- <br />aged within each depth range (near shore, mid, and furthest <br />from shore) and loglp transformed, to compensate for <br />unequal sample variance because plants grow in a geometric <br />progression. ANOVAs were also used to compare differences <br />in plant canopy ratios for each week (n=30 for each week). <br />Standard errors for both biomass and plant canopy ratios are <br />determined for weekly data and reflect the variability within <br />treatment plots, sub divisions, and between bays. <br />The rate of biomass accumulation was determined using <br />linear regression of the weekly loglp transformed biomass <br />average over all sites and depth ranges (Figure 2) (n=9). The <br />slopes were determined as: <br />log WW2 - log Wl = Relative growth rate <br />T2 -Tl _ <br />with units of week -'. W2 and Wl are biomass at time 2 (T2) <br />and time 1 (Tl) respectively. <br />We tested the statistical difference in rates of biomass <br />accumulation with the following model He: the slopes of the <br />regression lines were parallel and the intercepts are differ- <br />ent; Ha: the slopes and intercepts are different. The models <br />were compared using an F -test (Weisberg, 1985). Bay to bay <br />differences in lake physical/chemical characteristics were <br />determined using Tukey's pairwise comparison of means for <br />each bay. Pearson correlation and multiple regression tech- <br />niques were used to look at the relationships between lake <br />characteristics and plant biomass and percentages of milfoil. <br />RESULTS AND DISCUSSION <br />Regrowth after harvest <br />Harvested plots had significantly higher relative growth <br />rates over the remaining field season than did reference <br />areas (p = 0.001) . Relative growth rates, determined from the <br />slopes of the regression lines shown in Figure 2, <br />- 0.03 week-' (p=0.001 for regression) in reference areas and <br />0.02 week-' (regression not significant) in harvested areas. <br />Without the data from the 2nd week the relative growth <br />rate in the harvested areas is 0.03 week-' (p= 0.08 for regres- <br />sion). The anomalous increase in harvested biomass shown <br />the 2nd week after harvest (Figure 2) may be due to an <br />increase in fragments, which are also sampled by our <br />method. Before this sampling date there was a storm which <br />58 J. Aquat. Plant Manage. 32: 1994. <br />were <br />
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