Accepted: 20 February 2018
DOI: 10.1111/fwb.13101
ORIGINAL ARTICLE
Evaluating effects of weed cutting on water level and
ecological status in Danish lowland streams
Annette Baattrup-Pedersen1
| Niels B. Ovesen1 | Søren E. Larsen1 |
Dagmar K. Andersen1 | Tenna Riis2 | Brian Kronvang1 | Jes J. Rasmussen1
1
Department of Bioscience, Aarhus
University, Silkeborg, Denmark
2
Department of Bioscience, Aarhus
University, Aarhus C, Denmark
Correspondence
Annette Baattrup-Pedersen, Department of
Bioscience, Aarhus University, Silkeborg,
Denmark.
Email: abp@bios.au.dk
Abstract
1. At present, scientific evidence documenting effects of weed cutting in streams
as a measure to improve flood protection and run-off from agricultural land is
scarce, which is surprising considering the huge effect that it has on stream ecology. Instead, weed cutting is performed under the assumption that removal of
aquatic plant biomass improves runoff from agricultural land and prevents flooding of adjacent areas provided that it is performed regularly.
2. In this study, we examined linkages between weed cutting practice and water
level reductions in 126 small- and medium-sized Danish streams (catchment size
<100 km2) with continuously monitored discharge and water level data (from
1990 to 2012). Specifically, we hypothesised that (1) weed cutting reduces
stream water levels more in late summer when the biomass of aquatic plants is
higher than in early summer; (2) the efficiency of cutting declines with increasing
cutting frequency as the aquatic plant community changes with increasing abundance of species able to regrow fast following a cutting event; (3) the high-frequency cutting in Danish streams lowers the ecological status of the streams as
evaluated from aquatic plant assemblages.
3. The average effect of weed cutting on the water level was largest in July, August
and September with an average reduction of 16 cm and lowest in early spring
and late autumn with an average reduction of 11 cm. Regrowth was largest in
June, with an increase in water level of 0.41 cm/day, whereas regrowth was
absent in autumn. Regrowth also varied with the frequency of weed cutting,
from an average of 0.04 cm/day in streams subjected to one annual cutting to
an average of 0.6 cm/day in streams subjected to >6 annual cuttings. Furthermore, we found that the ecological status was either moderate or poor/bad in
streams with more than one annual cutting.
4. Our findings highlight that it is by no means certain that the current weed cutting practice is efficient for flood control since (1) regrowth is stimulated by frequent cuttings and a positive feedback loop may develop, necessitating even
more frequent cuttings to maintain the discharge capacity of the streams, and (2)
many species stimulated by weed cutting, like for instance Sparganium emersum,
form dense canopy beds across the entire stream profile and therefore reduce
the discharge capacity of the stream more than species growing in confined
Freshwater Biology. 2018;1–10.
wileyonlinelibrary.com/journal/fwb
© 2018 John Wiley & Sons Ltd
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BAATTRUP-PEDERSEN
ET AL.
patches. We encourage more studies with the aim to identify how stream maintenance should be performed to optimise flood control without compromising
the ability to reach good ecological stream quality.
KEYWORDS
aquatic plants, macrophytes, maintenance, management, river
1 | INTRODUCTION
scarce, though (but see e.g. Old et al., 2014). This is surprising considering that maintenance has a tremendous effect on the ecology
Aquatic plants are central elements of many small and shallow low-
of the streams (Armitage, Blackburn, Winder, & Right, 1994; Baat-
land streams today and may also in former times under conditions
€ the, Riis, & O’Hare, 2016; Baattrup-Pedersen
trup-Pedersen, Go
relatively undisturbed by human settlement have played a key role
et al., 2003; Dawson, Clinton, & Ladle, 1991; Kaenel & Uehlinger,
for these ecosystems (Svenning, 2002). Aquatic plants regulate and
1999). Instead, maintenance is performed under the assumption that
modify important in-stream habitat characteristics (e.g. substrate
removal of aquatic plant biomass improves flood protection and run-
composition and retention of fine particulate organic matter) and
off from agricultural land if applied regularly (Bach et al., 2016; Old
hereby the structural and functional characteristics of the biological
et al., 2014; Vogelsang, 2016).
stream communities (Caffrey, 1991; Carpenter & Lodge, 1986; Gur-
In Denmark, plant growth is highly seasonal and begins in early
nell, 2014; Sand-Jensen, 1997). For example, aquatic plants usually
spring when light and temperature conditions increase to levels suit-
have a stimulating effects on macroinvertebrate abundance and spe-
able for photosynthesis. Subsequently, the accumulation of plant
cies richness (Ferreiro, Feijoo, Giorgi, & Leggieri, 2011; Iversen,
biomass gradually declines as the availability of light becomes the
1988), which may further support dense and productive populations
limiting resource (Sand-Jensen, 1997) and die back occurs for most
of fish such as brown trout (Salmo trutta; Madsen, 1995; Mortensen,
species during autumn. Maintenance is performed regularly in a
1977; Teixeira-de Mello et al., 2015).
majority of streams, but over the last three decades, the frequency
Aquatic plants also influence the hydraulic conditions in streams
of weed cutting has increased, from typically 1–2 to 2–3 times per
by increasing the resistance against flow and, hence, the water level
year, and the frequency is even higher in many streams due to
within the channel (Curran & Hession, 2013; Sand-Jensen et al.,
extensive regrowth. At the same time, stream maintenance has been
1989). The spatial variability of aquatic plant growth within the
increasingly confined to the central parts of the stream channel,
channel makes it difficult to predict the resistance from coverage
which is supposed to be more environmentally friendly (Baattrup-
alone, however, as it may change with the distribution of patches
Pedersen, Skriver, & Wiberg-Larsen, 2000). However, it has never
and patch architecture (Folkard, 2011; Green, 2005). Additionally, at
been systematically explored to what extent the higher cutting fre-
high flow plant configuration may change radically (e.g. O’Hare,
quency has improved flood protection or run-off from agricultural
Hutchinson, & Clarke, 2007; Sand-Jensen, 2003), making it even
land, nor has it been explored how it affects the ecological quality of
more difficult to predict their resistance. Flow resistance associated
the streams also in terms of downstream reaches that are likely to
with aquatic plants is the main reason for active maintenance of
receive increased loads of eroded sediments and associated chemi-
aquatic plant populations in streams (Dawson & Robinson, 1984;
cals (Old et al., 2014). It can be argued that an increase in weed cut-
Naden, Rameshwaran, Mountford, & Robertson, 2006; Pitlo & Daw-
ting frequency reduces the efficiency of the cutting because
son, 1990), and maintenance is performed regularly in many lowland
improved light conditions stimulate the regrowth of aquatic plants
streams to increase the discharge capacity (e.g. Baattrup-Pedersen
and, furthermore, that plant decay may be delayed due to renewal
et al., 2009; Caffrey, 1993; Fox & Murphy, 1990; Kaenel & Uehlin-
of the biomass (Dawson, 1978a, 1978b). Additionally, weed cutting
ger, 1999; Vereecken, Baetens, Viaene, Mostaert, & Meire, 2006;
may act as a strong species-specific environmental filter generating
€ ring, Filetti, Brux, & Herr, 2014). Maintenance methods
Wiegleb, Bro
cascading effects on the composition of aquatic plant communities
include simple weed cutting involving removal of aquatic plant bio-
(Baattrup-Pedersen & Riis, 1999, 2004; Baattrup-Pedersen et al.,
mass or removal of selected species using a scythe or boat mounted
2003; Pedersen, Baattrup-Pedersen, & Madsen, 2006; Sabbatini &
with knives (Baattrup-Pedersen, Larsen, & Riis, 2003; Old et al.,
Murphy, 1996b) and potentially compromise the ability to reach
2014; Schwarz & Snelder, 1999) and dredging of the total macro-
good ecological status as meeting this goal requires that all ecologi-
phyte biomass and associated accumulated sediments using an exca-
cal quality elements are in at least good ecological status (the one-
vator (Caffrey, 1993; Sabbatini & Murphy, 1996a, 1996b).
out-all-out principle; European Commission, 2000).
Scientific evidence documenting the effects of stream mainte-
In this study, we examined 3,000 weed cuttings performed in
nance as a measure to maintain the discharge capacity (Dawson,
small- and medium-sized Danish streams (catchment size <100 km2)
1978a, 1978b; Gurnell & Midgley, 1994; Pitlo & Dawson, 1990) is
to explore to what extent the stream water level declines following
BAATTRUP-PEDERSEN
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ET AL.
cutting and how this response is influenced by the timing and frequency of weed cutting. Specifically, we hypothesised that (1) weed
3
2.2 | Hydraulic calculations
cutting reduces stream water levels more in late summer when the
The fundamental problem encountered when attempting to estimate
biomass of aquatic plants is higher than in early summer; (2) the effi-
discharge from stage at a stream gauging station at a site with
ciency of cutting declines with increasing cutting frequency as the
downstream growth of macrophytes is that the resistance of the
aquatic plant community changes with an increasing abundance of
flow is subject to variations with increasing resistance during the
species able to regrow fast following a cutting event; (3) the high-
spring and summer season (Dawson, 1978a, 1978b). The increase in
frequency cutting in Danish streams lowers the ecological status of
resistance might be counteracted by stream maintenance involving
the streams as evaluated from aquatic plant assemblages applying
cutting of the macrophytes. We have utilised this normally seen pat-
the Danish Stream Plant Index (DSPI; Baattrup-Pedersen, Larsen, &
tern in Danish lowland streams to analyse each stream hydraulically
Riis, 2013; Baattrup-Pedersen et al. 2017) that is currently used to
to register: (1) time of cutting, (2) water level drop associated with
assess the ecological status of the aquatic plant community in com-
cutting and (3) water level increases resulting from vegetation
pliance with the Water Framework Directive.
regrowth following cutting (Figure 2).
Base discharge (Q)–stage (H) relationships were established for
2 | METHODS
2.1 | Study sites
each stream gauging station based on monthly measurements of discharge and water stage utilising only measurements of discharge and
stage during the winter and early spring period where the hydraulic
influence of growing macrophytes in the downstream channel is
A total of 126 Danish stream reaches with continuously monitored
absent or very small (Figure 2a; Herschy, 1995). Discharge was mea-
discharge and water level data for at least 10 years within the period
sured following the guidelines in ISO-standard ISO748 according to
1990–2012 were included in this study (Figure 1; Ovesen et al.,
number of depth transects established and point measurements of
2000). The streams were all small- to medium-sized and distributed
current velocity utilising OTT C31, OTT C2. However, Doppler
throughout Denmark (Figure 1). A total of 3,086 weed cutting
instruments (ADCP) like StreamPro from RD Instruments have been
events were registered in the 126 streams following the procedure
applied in most larger and deeper Danish streams following the ISO-
described below.
standard ISO/TS 24154 in recent years. The annual number of discharge measurements was 10–12.
The influence of macrophyte growth during the summer period
can be observed in the Q/H relationship as deviations of water
stage from the base Q/H relationship (Figure 2a; Dawson, 1978a,
1978b; Gurnell & Midgley, 1994). The deviations in H from the base
Q/H relationship are caused by a change in resistance of flow in
the downstream channel from especially growing macrophytes are
described as new Q/H variants (Figure 2a). In fact, for calculation of
discharge, a new Q/H relationship is established for every time step
in the water stage record between the dates with actual measured
discharge and stage utilising an interpolation procedure to produce
the suite of Q/H curves. Discharge for every time step is then calculated based on the water stage record (every 10 min) making use
of the established corresponding Q/H relationship variants (Figure 2b).
To analyse and extract the influence of macrophyte growth and
weed cutting during the summer period independent of changes in
discharge, a control discharge for the summer period (median summer discharge) was estimated for all streams (Figure 2a). The water
stage record for every time step (10 min) is then referred back to
the control discharge (in the example stream control discharge is
800 L/s) and calculation of the water stage at that control discharge
is used for showing the changes (increase) in stage more or less
solely ascribed to changes in resistance due to regrowth of macrophytes in the channel downstream of the gauging station (Figure 2c).
Similarly, cutting of weed in the channel downstream of the gauging
FIGURE 1
streams
Map showing the geographical location of the study
station will result in an abrupt reduction in resistance shown as a
sudden decline in the control water stage (Figure 2c).
4
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BAATTRUP-PEDERSEN
(a)
240
Control Q
(800 l/s)
220
Water stage (cm)
ET AL.
200
180
Base
160
Q/H-r
elatio
nship
140
120
100
Discharge measurement
Q/H variants
80
0
1,000
2,000
3,000
4,000
Discharge (l/s)
(b)
Water stage (cm)
260
240
220
200
180
160
Discharge (l/s)
140
5,000
4,000
3,000
2,000
1,000
0
Jan
(c)
Water stage (cm)
260
240
Feb
Mar
Apr
May
Jun
Jul
Discharge measurement
Control point
Control water stage
Aug
Sep
Oct
Nov
Dec
Weed cutting
220
200
180
160
140
Apr
May
Jun
Jul
Aug
Sep
Oct
F I G U R E 2 An example stage (H)–discharge (Q) relationship at a gauging station in the stream Trend
A with inserted control Q (a), observed
water stage and calculated discharge (b) and the calculated control water stage during summer period (c)
2.3 | Hydrographs and weed cutting
the result. Finally, the water level increase due to regrowth of the
vegetation following cutting was estimated as the increase in con-
A sudden drop in water level on the hydrographs over a couple
trol water level following cutting. The period used for this estima-
of hours was registered as a weed cutting event. The drop had to
tion was restricted to 3 weeks to prevent underestimation of
be a sudden and not a continuous drop in water level over days
regrowth due to intensified internal shading within the plant beds
since the latter may reflect more factors than just weed cutting
upon regrowth. In streams that were left uncut, growth was calcu-
such as removal of cut biomass with reduced stowing in conse-
lated as the increase in control water level from 1 May and
quence (Figure 2). Often, a sudden increase was registered just
3 weeks ahead. This approach was chosen to avoid that the bio-
prior to the drop, reflecting that the water stowed just upstream
mass reached levels promoting internal shading with negative
of the maintenance machinery. The water level drop associated
effects on growth estimations.
with a cutting was estimated as the difference between the water
level before and after cutting (denoted a in Figure 2). The water
level prior to cutting was estimated from a regression line cover-
2.4 | Physical and chemical variables
ing the increase in control water level over the last 3 weeks,
Physical and chemical environmental variables were assessed accord-
thereby avoiding that minor water level fluctuations would affect
ing to the technical guidelines of the Danish monitoring programme
BAATTRUP-PEDERSEN
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ET AL.
5
(Pedersen & Baattrup-Pedersen, 2003). Water chemistry parameters
of the number of weed cuttings. The effect of site was included in
(NO23-N, PO4-P, total-P) were determined at least twice annually
the ANCOVA model as a random effect since sites are regarded as a
(spring and autumn) at base-flow and means were used in the analy-
random subsample from a larger population of sites.
sis. Stream width, depth and slope were measured, and the stream
Since weed cutting practice may change over time, we only
reach was categorised according to (1) channel shape (i.e. a natural
included sites with similar cutting frequency in 2012 and 2013 when
shape being meandering or sinuous and a channelised shape being
analysing the influence of cutting frequency on the ecological status
straight) and (2) stream profile (i.e. a natural profile having natural
applying DSPI.
variations in depth, hydrology and substrate and a channelised profile having a rectangular shape). The number of sites with information on each variable is given in Table 2.
3 | RESULTS
3.1 | Effects of weed cutting on water level
2.5 | Aquatic plant data
The average discharge of the 126 streams was 1.71 m3/s, average
Aquatic plant data for 2012 and 2013 were obtained from the
width (66 streams) was 7.4 m, and average depth 42.7 cm (Table 1).
Danish
environment,
Some of the streams were quite small, however, with a mean width
NOVANA (Friberg, Baattrup-Pedersen, Pedersen, & Skriver, 2005).
of only 1.0 m and a mean depth of 5.6 cm (Table 1). The plant cov-
Aquatic plant data were collected following the protocol described
erage of the streams was, on average, 59% but with a large
in Pedersen and Baattrup-Pedersen (2003). In each stream reach,
between-stream variability (Table 1). Of the total of 3,086 weed cut-
plant recordings were made in July/August at maximum biomass.
tings registered in the 126 streams, most were performed from June
Recordings were made in approximately 150 plots (25 9 25 cm)
to September and <15% outside this period (Figure 3). The earliest
placed side by side in cross-sectional transects at a 100-m-long
cutting was performed at the start of April and the latest at the end
stream reach. Depending on the width of the stream, the number
of November.
monitoring
programme
on
the
aquatic
of transects varied from a minimum of 10 to maximum 20 in small
We found significant effects of weed cutting on the water level
streams. A cover score was allocated to each species present in
in the streams and that these varied over time (Figure 4; Mixed
the plots using the following abundance scale: 1 = 1%–5%,
model ANOVA; F = 5.73; p < .0001). Generally, the effect was
2 = 6%–25%, 3 = 26%–50%, 4 = 51%–75%, 5 = 76%–100%. Spe-
strongest in July, August, and September, with an average reduc-
cies abundance at each stream reach was then calculated as the
tion of 16 cm, and lowest in early spring and late autumn, with an
sum of cover scores to the maximum score sum (i.e. the number of
average reduction of 11 cm. The smallest effect of weed cutting
plots multiplied by the maximum score of five; Pedersen et al.,
was a few cm and the greatest was 73 cm, such large drops being
rare, though, as the upper 75% quantile was a little <20 cm and
2006).
the lower 25% quantile <5 cm (data not shown). The observed
2.6 | Ecological status assessment from aquatic
plant data
variability in water level drop associated with cutting may be partly
explained by differences in the slope of the streams and stream
size in terms of stream width and depth (data not shown). Thus,
Ecological status was calculated from the Danish Stream Plant Index
the effect of weed cutting declined with increasing stream slope in
(DSPI; Baattrup-Pedersen et al., 2013). The index gives an Ecological
the range of 0&–3& (r =
Quality Ratio (DSPI_EQR) that expresses the deviation from the nat-
increasing stream width in the range from 2 to 16 m (r = .38;
.32; p < .0001) and increased with
ural undisturbed conditions. The ratio is expressed as a numerical
p = .016) and with stream depth within the range of 8–90 cm
value between 0 and 1 and translates in to high, good, moderate,
(r = .51; p < .0001).
poor and bad using the flowing boundary between ecological status
classes:
high/good = 0.70;
good/moderate = 0.50;
moderate/
poor = 0.35; poor/bad = 0.20. DSPI complies with the requirements
of the Water Framework Directive (WFD) and is currently used in
the ecological assessment of aquatic plant communities in mediumsized and large streams in Denmark.
2.7 | Statistics
T A B L E 1 Characteristics of the 126 streams used in the study
showing mean, minimum and maximum discharge, depth, width and
plant coverage. Values on depth, width and plant coverage are based
on measurements in summer (July, August), while discharge
measurements are yearly measurement means. Note that plant
coverage can exceed 100% in multi-layer communities (see for
instance Baattrup-Pedersen et al., 2002)
No. of streams
The effect of weed cutting measured in terms of a water level drop
was tested in a linear covariance model (ANCOVA) with month as
the categorical independent variable and the number of weed cuttings as the covariate. The covariate model evaluates the means of
the effect of weed cutting across months controlling for the effect
3
Discharge (m /s)
Depth (cm)
Width (m)
Plant coverage (%)
126
Mean
Min
1.71
Max
0.05
26.10
42.7
5.6
89.9
66
7.4
1.0
34.8
126
59.5
4.6
97.9
66
6
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BAATTRUP-PEDERSEN
T A B L E 2 Results of linear regression models between regrowth,
expressed as the increase in water level following weed cutting and
stream water chemistry (PO4-P, total-P, and NO23-N), stream
channel morphology (shape and profile) and vegetation
characteristics (coverage and community-weighted means [CWM] of
growth from basal, multi-apical and single-apical meristems). All
regression models were statistically significant (p < .05). NS denotes
that the obtained model was without significance (p > .05)
800
Number of weed cuttings
700
600
500
400
300
200
Variable,
category
Variable
Chemistry
PO4-P
100
0
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
F I G U R E 3 The number of weed cuttings performed in the 126
investigated streams in months with weed cutting
Morphology
Vegetation
18
16
14
No. of
streams
54
Fvalue
Pr > F
3.35
NS
total-P
54
0.47
NS
NO23-N
54
0.04
NS
Channel shape
20
1.04
NS
Channel profile
20
0.18
NS
Coverage
126
2.40
NS
CWM basal growth
126
7.63
0.0076
CWM multi- apical
growth
126
4.68
0.0345
CWM single-apical
growth
126
5.91
0.0181
12
0.6
10
8
0.5
6
0.4
4
2
0
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
F I G U R E 4 The effect of weed cutting in terms of cm drop in
water level in months with weed cutting
Regrowth (cm/day)
Cutting effect (cm water level)
ET AL.
0.3
0.2
0.1
0
–0.1
–0.2
3.2 | Regrowth
The increase in water level following weed cutting due to vegetation
regrowth did not vary significantly with either stream water chem-
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
F I G U R E 5 Regrowth in terms of increases in water level after
weed cutting applying a period restricted to 3 weeks in months with
weed cutting
istry (PO4-P, total-P, NO23-N; Table 2; p > .05), morphometric
properties of the stream (channel shape, channel profile; Table 2;
Regrowth also varied significantly with cutting frequency as a
p > .05), or total plant coverage in the streams (Table 2; p > .05).
significant interaction was observed between the time and the fre-
However, regrowth did vary significantly with growth characteristics
quency of cutting (mixed model covariance analysis; F = 2.61;
of the vegetation (Table 2). Thus, regrowth increased with an
p < .0163). Thus, regrowth increased with enhanced cutting fre-
increasing abundance of species growing from basal growth meris-
quency (Figure 6), from an average of 0.04 cm/day in streams sub-
tems (Table 2; p < .05) but decreased with increasing abundance of
jected to one annual cutting to an average of 0.6 cm/day in streams
species growing from single or multi-apical growth meristems (Fig-
subjected to >6 annual cuttings. No significant differences in
ure 5, Table 2; p < .05).
regrowth were found in streams cut 6, 7 and 8 times annually (Fig-
The increase in water level following weed cutting due to vegetation regrowth varied significantly with cutting time (Mixed model
ure 7). Regrowth in June was 0.2 cm/day in streams cut once per
year and 0.9 cm/day in streams cut eight times per year.
covariance analysis; F = 4.04; p = .0005; Figure 5). Regrowth was
largest in June, with an increase in water level of 0.41 cm/day,
whereas no regrowth took place in autumn. In October, negative
3.3 | Ecological status
regrowth was registered, indicating that the plant biomass was
We found that ecological status assessed applying DSPI depended
decaying.
significantly on the annual number of weed cuttings (ANOVA;
BAATTRUP-PEDERSEN
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ET AL.
7
with those in comparable streams outside Denmark. However, in
1.0
support of our results, a study conducted in River Lambourn, UK,
revealed responses to cutting comparable with those observed in
Regrowth (cm/day)
0.8
our investigation (average 16 cm), varying between 16 and 29 cm in
three successive years of cutting (Old et al., 2014), and another
0.6
study, although based on modelling, reported a change in water level
of app. 50 cm (Hearne & Armitage, 1993).
0.4
We also observed that plant regrowth was highest in early summer, in June, and absent in autumn, and furthermore, and in accor-
0.2
dance with our second hypothesis, that regrowth occurred faster in
streams that were cut frequently. Actually, we observed a fourfold
higher regrowth in streams cut eight times during summer compared
0
0
1
2
3
4
5
6
8
7
Number of cuttings (per year)
with that observed in streams cut once during summer. Fast
regrowth reduces the time where the discharge capacity is main-
F I G U R E 6 Regrowth in terms of increases in water level after
weed cutting applying a period restricted to 3 weeks after weed
cutting as a function of the number of weed cuttings performed in
the streams
tained or partly maintained in the channels. For example, if the
increase in water level is 0.6 cm/day, then it takes 4 weeks to reach
pre-cutting conditions (applying the average water level drop of
16 cm). In contrast, in June when regrowth is at its maximum
(0.9 cm/day),
pre-cutting
conditions
are
obtained
after
only
Weed cutting frequency (per year)
2.5 weeks.
2.0
A
The finding that plant regrowth increased with increasing weed
A
cutting frequency is unlikely to reflect differences in growth conditions among the streams. Thus, regrowth did not vary following a
1.5
predictable pattern with either stream water chemistry or morpho-
B
1.0
metric properties of the stream channel. Instead, we observed that
B
regrowth increased with the abundance of plant species growing
from basal meristems and decreased with the abundance of species
growing from single- and multi-apical meristems. In accordance with
0.5
this, previous studies have also shown that weed cutting prompts
higher abundance of species growing from basal meristems while
0
being less abundant in streams without cutting (Baattrup-Pedersen
1–2
3
4
5
Ecological status (DSPI)
F I G U R E 7 Relationships between weed cutting frequency
(annual cuttings) and ecological status class based on aquatic plant
assemblages in the streams applying DSPI (Danish Stream Plant
Index). Different letters denote significant difference between mean
values (ANOVA; p < .5)
et al., 2016), whereas species growing from apical meristems show
the opposite pattern (Baattrup-Pedersen et al., 2016). Hence, the
position of the growth meristem likely determines the potential for
plant regrowth following weed cutting, reflecting that species that
have an intact growth point after weed cutting can start regrowth
immediately after the intervention, whereas species with apical
growth meristems exhibit delayed regrowth. Consequently, the
increased weed cutting frequency in Danish streams may have
p < .05). Stream sites that were cut more than once per year were
caused a shift in the composition of plant species towards increasing
either classified as poor/bad or moderate ecological status sites,
dominance of species possessing traits that enable them to cope
whereas sites cut once per year or less were classified as either
with frequent cutting (Abernethy, Sabbatini, & Murphy, 1996; Baat-
good or high ecological status sites (Figure 7).
trup-Pedersen et al., 2016; Sabbatini & Murphy, 1996b). Consequently, our findings strongly question the underlying assumption
that the change in cutting practice in Danish streams around 1990
4 | DISCUSSION
from less comprehensive to more frequent weed cutting (BaattrupPedersen et al., 2000) has maintained the discharge capacity of the
In accordance with our first hypothesis, we found that weed cutting
streams. In fact, the observed increase in plant regrowth with
lowered the water levels in the investigated streams and that the
enhanced frequency of weed cutting may have intensified the need
effects of cutting were strongest in late summer when the biomass
for regular cutting to maintain the same discharge capacity.
of aquatic plants was highest. As stated already in the introduction,
Other studies have shown that species with high tolerance
quantifications of the hydraulic impacts of weed cutting are rare,
towards weed cutting often exhibit a high overwintering capacity as
making it difficult to compare the here observed water level drops
well by producing vegetative propagules that remain dormant during
8
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BAATTRUP-PEDERSEN
ET AL.
the coldest seasons (Baattrup-Pedersen et al., 2003, 2016; Wiegleb
combination of increased average flow and higher plant biomass can
et al., 2014). Consequently, the resilience of these species may be
intensify the need for management targeting flood prevention. Our
huge once they become dominant. This may also explain why Spar-
findings highlight that it is questionable if the current weed cutting
ganium spp. and other species that both have basal growth and a
practice is an efficient flood protection measure since (1) regrowth
high overwintering capacity are highly tolerant of weed cutting, as
seems to be stimulated by frequent weed cutting and a positive
observed previously (Baattrup-Pedersen et al., 2003, 2016; Wiegleb
feedback loop may develop, requiring even more frequent cuttings
et al., 2014). For example, Wiegleb et al. (2014) noticed an increase
to maintain the discharge capacity, and (2) many species that are
in S. emersum in response to increasing anthropogenic disturbance in
stimulated by weed cutting, such as for instance S. emersum, form
German rivers when combining hydromorphological stressors (e.g.
dense canopy beds across the entire stream profile and may there-
weed cutting, dredging, and construction work) and stressors associ-
fore cause a greater reduction in the discharge capacity than species
ated with water quality such as malfunctioning sewage plants and
growing in confined patches (Sand-Jensen & Mebus, 1998). At pre-
conventional agriculture. Interestingly, S. emersum is also widely dis-
sent, however, very limited information exists on how different plant
tributed in less disturbed lowland streams in Europe (Baattrup-Ped-
morphologies impact flow (Naden et al., 2006) and how a shift in
ersen et al., 2008) but less abundant than in anthropogenically
species composition can influence flow resistance (e.g. Pitlo & Daw-
disturbed streams (Baattrup-Pedersen, Larsen, & Riis, 2002; Birk &
son, 1990).As an alternative to weed cutting, the establishment of
Willby, 2010; Pedersen et al., 2006; Riis, Sand-Jensen, & Vester-
buffers along streams that can act as measures against flooding of
gaard, 2000; Steffen, Becker, Herr, & Leuschner, 2013). It has been
downstream areas under high flow events may be more efficient.
suggested that the success of this species in less impacted streams
is linked to a low light compensation point and a low photosaturation level (Sand-Jensen et al., 1989). Hence, different traits can
ACKNOWLEDGEMENT
contribute to its success in different types of streams (Baattrup-
This study was supported by the European Union Seventh Frame-
Pedersen et al., 2002).
work Project MARS under contract no. 603378. We thank Anne
In accordance with our third hypothesis, we found that weed
cutting clearly conflicts with the probability of reaching good ecolog-
Mette Poulsen for manuscript editing and Tinna Christensen for
figure layout.
ical status in the investigated streams as meeting this goal requires
that all ecological quality elements are in at least good ecological status (the one-out-all-out principle; European Commission, 2000). We
ORCID
found that the ecological status assessed from species composition
Annette Baattrup-Pedersen
applying DSPI (Baattrup-Pedersen et al., 2013) was either moderate
344X
http://orcid.org/0000-0002-3118-
or poor/bad in streams with more than one annual weed cutting.
This finding highlights the necessity of developing new management
practices for lowland streams to secure both the discharge capacity
and the ecological quality. At present, little research has been conducted into developing alternative management methods, but other
measures should be considered. Based on our findings, we suggest a
reduction in weed cutting frequency and its postponement to late
summer to avoid fast regrowth. Additionally, we suggest that weed
cutting should be risk-based so that cutting is only performed when
there is a risk of flooding of adjacent areas as opposed to cuttings
performed at fixed time periods. As long as the frequency is
reduced, such a practice may hinder cuttings that only lower the
water table marginally and counteract the development of aquatic
plant communities with fast regrowth.
4.1 | Perspectives under climate change
The ongoing climate change will increase the average flow in lowland streams, mainly due to higher precipitation (and less snow accumulation) during winter months with an increase in the frequency
and magnitude of extreme flow events (Karlsson, Sonnenborg, Seaby,
Jensen, & Refsgaard, 2015; van Roosmalen, Sonnenborg, & Jensen,
2009; Thodsen et al., 2014). In addition, increasing temperatures
may prolong the plant growing season in the streams. The
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How to cite this article: Baattrup-Pedersen A, Ovesen NB,
Larsen SE, et al. Evaluating effects of weed cutting on water
level and ecological status in Danish lowland streams.
Freshwater Biol. 2018;00:1–10. https://doi.org/10.1111/
fwb.13101