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iForest - Biogeosciences and Forestry
vol. 4, pp. 218-225
Copyright © 2011 by the Italian Society of Silviculture and Forest Ecology
doi: 10.3832/ifor0586-004

Collection: COST Action FP0903 (2010) - Rome (Italy)
“Research, monitoring and modelling in the study of climate change and air pollution impacts on forest ecosystems”
Guest Editors: E Paoletti, J-P Tuovinen, N Clarke, G Matteucci, R Matyssek, G Wieser, R Fischer, P Cudlin, N Potocic

Research Articles

Towards harmonization of forest deposition collectors - case study of comparing collector designs

D. Zlindra (1)Corresponding author, K. Eler (2), N. Clarke (3), P. Simončič (1)


The forest monitoring activities within the International Co-operative Programme on Assessment and Monitoring of Air Pollution Effects on Forests (ICP Forests) operating under the UNECE Convention on Long-range Transboundary Air Pollution (CLRTAP) are divided in two levels. Level I activities are based on observations of forests in the plots which systematically represent 256 km2 each and are less intensive. Level II activities are more intensive, in-depth investigations; many additional important observations are performed on these plots. Locations of Level II plots were not systematically selected by geographical coordinates. Since the beginning of forest monitoring within the ICP Forests program the methods and approaches have differed from country to country, especially for Level II activities. Nevertheless, large data series from a long time period have been collected and evaluated. Specifically under the FutMon Life project (LIFE07 ENV/D/000218; 2009-2010), with several actions coordinating quality assurance and quality control of monitoring data (QA/QC) and quality assurance in laboratories for all applied methods (⇒ http:/­/­www.­futmon.­org/­structure-and-organisation), huge steps in the harmonization of forest monitoring in Europe have been made, beginning with large-scale harmonization, laboratory method harmonization and manual harmonization.

Methods to estimate forest deposition have until now rarely been compared. Different collector designs and their spatial representativeness were compared by Reynolds & Leyton ([17]), Kostelnik et al. ([9]), Reynolds & Neal ([18]), Crockford & Richardson ([7]) and Bleeker et al. ([5]). Ziegler et al. ([24]) compared stationary and mobile collectors in tropical rain forest and discovered good agreement at precipitation levels higher than 700 mm. To obtain good agreement they argued for testing and correction for the splash loss of collectors. In the intercomparison of twenty throughfall sampling systems used by different participating countries of the ICP Forests network, Bleeker et al. ([5]) found fairly good agreement between systems with large enough collector size and total coverage area but weaker agreement for smaller collectors where spatial variation gave a more pronounced difference from the best estimate (average of all systems). Mean deviation of throughfall quantities was 8% and ranged between -22% and 22.5%. Measurements of concentrations of main nutrients and ionic species mainly had larger deviations than quantities and were especially high for H (mean 21%, max 65%). Concentrations of NO3-, K+ and Kjeldahl-N were generally assessed more accurately. The authors stressed the significantly higher importance of harmonization of field methods (collector type, placement, size, total cover area, geometry of collectors) compared to laboratory methods for accurately assessing the throughfall fluxes. A very comprehensive review of forest deposition monitoring, equipment and sampling design was made by Thimonier ([22]) where all the details on deposition monitoring equipment, sampling design and sampling frequency, and spatial representativeness are presented.

In order to compare different national collectors to one reference, the Expert Panel on Deposition of ICP Forests provided a prototype of a collector (so-called “harmonized” collector) fulfilling all the requirements of WMO ([23]) for precipitation collectors. The collectors were exposed for one year, except for snow periods when present. The numbers of the collectors per site are prescribed in the ICP Forests Manual Chapter XIV ([6]), generally depending on type and homogeneity of the forest stand (conifers or broadleaf species, one or two main tree species), age, canopy closure etc. Because of high variability of the designs of the plots and the spatial design of national collectors among the participating countries, other crucial parameters were kept as homogeneous as possible on the country level; i.e., generally only the collectors were different. It was suggested that the spatial design should be as far as possible similar to the spatial design of the national collectors, the sampling frequency of the harmonized collectors should be the same as for national collectors, and also the procedures for cleaning the collectors and bulking the samples for subsequent chemical analyses. This paper describes the sampler comparison for one Level II plot in Slovenia.

Material and Methods  

Study Site

The study was conducted on the ICP Forests Level II plot no. 4, which is also a FutMon core plot, located on the Brdo estate in Gorenjska region in north-west Slovenia, latitude 46°17’ N, longitude 14°24’ E, elevation 471 m a. s. l.

The monitoring activities on the selected plot have been performed starting in 2003. The research plot of 10 000 m2 (100 x 100 m) area is fenced and encompasses an inner part of 50 x 50 m. The inner part is dedicated to the study of growth, defoliation, forest health and ground vegetation monitoring and research. In the outer part, different collectors are installed e.g., throughfall collectors for precipitation other than snow (gutter-type), throughfall collectors for snow (cornet-type), baskets for litterfall, and soil solution sampler devices (suction cup lysimeters - Fig. 1). The main tree species in the plot is Scots Pine (Pinus sylvestris L.). The stand belongs to the Vaccinio myrtilli-Pinetum forest type, is 80 to 120 years old, and canopy openness is 18%. The prevailing soil unit is Dystric Cambisols ([8]) developed from fluvioglacial gravels and sands. The site is slightly exposed to the south-east (210°). The open-field plot (Fig. 2) is located about 150 meters from the main plot and is dedicated to bulk precipitation measurements, meteorological observations and ozone sampling with passive sampler dosimeters.

Fig. 1 - The configuration of the collectors in the stand - line A (Photo: D. Zlindra).
Fig. 2 - The configuration of the collectors in the open field (Photo: D. Zlindra).

Collector designs and sampling procedure

In the outer 25 m borders of the plot, 10 national throughfall collectors of gutter type were placed. They were divided in two lines (named Line A and Line B). Each gutter was a 3 m long tube with 4 cm in diameter. Each tube had three slits in line, 87 cm long and 0.9 cm wide. Each gutter was connected to a 5 litre collecting bottle by silicone tubing. The collecting bottles were placed in the ground in order to minimize temperature influence on the samples. For the purpose of the experiment, 30 additional throughfall collectors of the harmonized design (which were of funnel type) were placed in the near vicinity of the gutters: along every gutter 3 funnels were installed on each side alternately, at a perpendicular distance of 1 meter from the gutter. The funnels were installed at a height of 1.0 m above ground level by means of PVC pipe. The sampling area had a diameter of 159 mm. The funnel construction was made of white polyethylene (PE) and meets the requirements of the relevant Manuals ([23], [6]). An especially important detail of the funnel design was the rim, because the rim (vertical on the inner side, very steep slope on the outer side) prevented rain drops splitting and partly (uncontrollably) sprinkling into or out of the funnel. Another very important geometrical attribute of the collector is the height of the vertical part of the funnel in connection with the more gradually sloping part of it, leading into the outflow tube. The height of the vertical part had to be high enough and the gradual part steep enough so that the whole amount of the precipitation could be captured without losses due to splashing. The collecting bottles (5 litres volume) were directly connected to the funnel. Around the funnel a bird ring was mounted, consisting of two rings in two heights formed by fishing line. For avoiding tree litter dropping into the collecting bottles a cone shaped PE mesh with openings of 1 mm was placed in the neck of every funnel. Sampling started in July 2009 and lasted until October 2010, except for the snow period in January and February 2010. Both types of collectors were sampled on the same days, fortnightly. The cleaning procedures were also the same for both types: after the first 14-day period the sampling equipment (funnels, gutters and both types of collecting bottles) was cleaned and washed with ultra pure water in the field, and after the second 14-day period all parts of the sampling equipment, except the gutters, were cleaned and washed in the laboratory.

The amount of precipitation was registered after every 14-day period and for each collector. For the chemical analysis samples were pooled. Samples from harmonized collectors were bulked in such a way that the first 15 of them, placed near line A of national throughfall collectors, contributed to one sample for chemical analyses and the other 15 collectors, placed near line B of national throughfall collectors, contributed to the other. Samples gained by national collectors were also bulked from the A and B lines separately. Before chemical analysis, samples of the first (Period a) and second (Period b) 14-day period were bulked in proportion to their volumes.

In the open-field plot three national bulk collectors were installed. These were funnels, placed in a triangle at a distance of 4 meters from each other. They were installed at a height of 1.45 m above ground level. The funnels had diameters of 230 mm and were made of black polyethylene (PE). The collecting bottles (8 litres volume) were directly connected to the funnel. There were no bird rings around the funnel and no mesh for excluding litter in them.

Also here harmonized bulk collectors (funnel type) were placed in the triangle at a distance of 6.5 meters from each other. The fictive centre of this triangle was the same as for the national collectors, but the end points were 1.5 m outwards. The design of the harmonized collectors was the same as in the stand. Sampling periods and cleaning procedures were the same as for the collectors in the stand.

The designs of the national and harmonized bulk deposition collectors were similar except for minor details: the diameter of the national funnel was larger and consequently the collecting bottle was of higher volume to prevent overflow. The vertical edge was in both cases 10 centimetres but the angle to the lower, gradually sloping part of the funnels was 150 and 160 degrees for national and harmonized funnels respectively. Thus the possibility for losses of precipitation was bigger in the case of the national collectors. For both collectors a pipe of suitable diameter was used for placing them at the acceptable height.

The precipitation quantity was registered after every 14-day period for each collector separately. For the chemical analysis samples from the two national and two harmonized collectors were taken separately for every 14-day period. Before chemical analysis, samples of the first (Period a) and second (Period b) 14-day period were bulked in proportion to their volumes.

Data analysis 

Brief theory of testing the agreement between methods

When a new measurement method or device is developed it is important to test its agreement with other standardized or already established methods. The agreement is considered adequate when we might replace the old method with the new one. To test for agreement, the same samples are measured using both new and old method. In the case of destructive methods or where there are other reasons which prevent repeatability of measurement on the same samples (space and time variability), a larger number of samples is measured from the same population. Within the measurement comparison approaches the agreement is evaluated by testing for significant systematic differences. The differences or bias can be fixed (same shift across the range of values) or proportional (shift related to the magnitude of a measured variable). What is sought for in method comparison studies is actually not the agreement but the bias ([13]) which results from the statistical foundations itself. At a certain confidence level only the rejection of the zero hypothesis stating the agreement between methods is possible but not its confirmation.

Different statistical techniques are used to test for bias significance: regression methods, Altman-Bland plot, ANOVA approaches, kappa statistics, structural equation modelling etc. The choice is dependent on the type of variables being studied (continuous vs. categorical - [13], [4]), the presence of a “gold-standard” method for comparison ([2]), the number of replicate measurements per sample and the study design.

Calculating the Pearson correlation coefficient (r) is often the first choice of investigators when comparing methods. Nevertheless, this measure of strength of a linear relationship between two variables is not an appropriate measure for the agreement ([13], [3]). We might compute a high r but if the data do not lie along the identity (1:1) line the agreement is poor. Correlation also depends on the range of values of the measured quantity.

Secondly, regression analysis is often used. However, ordinary least squares regression (OLS), included in all statistical software, is mostly not the proper choice when comparing methods because it assumes fixed values of the independent variable. In terms of method comparison this would mean the existence of a gold-standard method with no measurement errors. This assumption is only rarely met (if ever). In praxis it can be used if measurement errors of the gold-standard method are considerably lower than the errors of the new method and can be considered negligible.

When errors not controlled by the researcher are present in both methods then OLS regression underestimates the slope of the regression line ([10]). In these cases model II regression approaches ([21], [10]) such as Deming regression (also known as major axis regression or least product regression), which allow values of both methods to be attended by random error, should be used. Deming regression, contrary to OLS, minimizes the perpendicular distances between points and regression line ([11]). Similarly to OLS, it assumes constant standard deviations across the range of values. When deviations change considerably, weighted variants of the methods are preferable ([11]). Whatever the regression approach chosen, the fixed and proportional bias of the new method are determined using intercept and slope estimates, respectively, together with the confidence intervals for each parameter. Significant fixed bias is ascertained when intercept confidence intervals do not contain 0 and proportional bias is significant when slope confidence intervals do not contain 1.

A simple, yet efficient approach was proposed by Altman & Bland ([1]) and Bland & Altman ([3]). These authors stated that it was the differences between methods that are most useful in searching for bias. By plotting the differences of the methods against their means and computing mean difference and 95% confidence intervals for the difference (a.k.a., limits of agreement) one can easily determine how good the agreement between the methods is and if the confidence interval is within the reasonable limits for the accuracy required from specific measurements. Limits of agreement are calculated as (eqn. 1):

Davg ± z2α SD

where Davg is the mean difference between methods, z is the standardized normal deviation of two sided P = 0.05 (1.96) and SD is the standard deviation of the differences.

In the case of smaller sample size (n), a more conservative approach using the Student t distribution should be used ([13]), which is calculated as (eqn. 2):

Davg ± tn-1.2α SD √[1 + (1/n)]

where tn-1.2α is the value of the t distribution corresponding to two sided P = 0.05 for n-1 degrees of freedom and √(1 + 1/n) is the correction for small sample size.

Besides determination of fixed bias (mean difference tested using a paired t-test), the Altman-Bland method can also estimate proportional bias if differences are regressed (using OLS) against the means. If no proportional bias is expected, the slope of that regression line will not significantly differ from 0, which is determined by looking at the slope confidence intervals.

The above mentioned approaches hold when the measurements of each method are independent, which means they are performed only once on each sample. Sometimes it is valuable or even only feasible to obtain replicate measurements by each method on each sample. The case of repeated measurements on the same samples is frequent in forest research where a temporal trend (time series) of a quantity is investigated. Different variants of random effects models are used where the variability of differences between methods is divided into within-subject variability and between- subject variability, with the latter estimating the agreement between the methods ([4], [14]).

Evaluation of the collector data  

The agreement between harmonized (funnel-type) and national (gutter-type) throughfall deposition collectors was evaluated using different approaches. In this way we also tried to determine the performances of different statistical techniques. For precipitation quantities (volumes) the approach was different than for the chemistry (concentrations and calculated depositions) because volume data were known for individual collectors, in contrast to chemistry where pooling of volume weighted samples of half of the collectors took place. Because volume data were known for individual collectors in each of the sampling periods, the data quality was considerably higher and tests stronger than for the chemistry data where the volume weighted samples of deposits were pooled from half of the collectors giving us two data points for each collector type per sampling period.

Regarding quantities, the following agreements were evaluated: open-field (bulk) precipitation, throughfall precipitation and canopy interception. For the chemical data, agreement between collector types for bulk and throughfall was assessed in terms of concentration, deposition and canopy interaction (throughfall / open-field).

Generally three techniques were used: Deming regression, the Altman-Bland method and repeated ANOVA. The first two methods were used to test for fixed and proportional bias; samples of the different sampling periods were assumed to be independent. For the calculation of limits of agreement according to Bland & Altman ([3]), eqn. 2 was used.

Repeated measures ANOVA was used to correct for sample dependence occurring due to repetitive sampling during the observation time. A partly nested ANOVA design was used for throughfall quantities and ratios with sampling period as the within-subjects factor, collector type as the between-subjects factor and collector pair (one gutter with the mean of the corresponding 3 harmonized funnels) as the random factor nested within collector type. The interaction term between collector type and sampling period was also included as the within subject factor. ANOVA for chemistry data was performed by preliminarily computing the mean of two data points of each method per sampling term, since it is difficult to estimate the variability on the basis of two data points, which would result in very large confidence intervals. Mean concentration or deposition or canopy interaction per sampling term was subjected to simple repeated measures (RM) ANOVA with collector type and sampling periods as the factors. With only one replicate per each combination of sampling period and sampling type, calculating the interaction is not feasible and this represents the error term in ANOVA.

As a descriptive measure of disagreement between collectors the mean relative deviation (d) in % was computed using the following equation (eqn. 3):


where pharmonized and pnational are the volumes or chemical parameters analysed (i) and j is the number of sampling periods taken into consideration.

Results and Discussion  

Quantities of precipitation

Open field (bulk) precipitation

On the basis of Deming regression and the Altman-Bland method, statistically significant fixed and proportional bias of bulk collectors was shown (Fig. 3); the intercept of the Deming regression was -3.342 (confidence interval, C.I.: -4.852, -1.874) and the slope was 1.082 (C.I.: 1.054, 1.111). The significant bias is the result of two influential data points with large precipitation (>150 mm per period) where the volumes measured by harmonized collectors were larger than the volumes found in the national collectors. If these points are not regarded the bias is not significant. No clear explanation for the deviation at larger precipitation volumes can be given. Due to the national collector being shallower than the harmonized collector, larger splashing of rain out of gauges might have occurred at more intense rainfall ([22]). Moreover, the larger collecting area and larger collector height of the national collectors can change the wind flow around the collector, resulting in lower catch ([19], [20]). However, despite statistical significance the mean deviation of the bulk collectors is so small (< 1%) that we regard it as irrelevant. If we take mean volumes measured by both collectors as the best estimate, the accuracy of both collectors is well within the 10% accuracy suggested by Bleeker et al. ([5]).

Fig. 3 - Scatter plot with Deming regression (A) and Altman-Bland plot (B) showing the agreement in volumes between national and harmonized bulk collectors.

Throughfall precipitation

Due to the different design of the throughfall collectors in our study (gutter vs. funnel), higher disagreement was expected in the measurements in the forest stand. A scatter plot with Deming regression and an Altman-Bland plot are shown in Fig. 4, both indicating supposedly fixed and proportional negative bias of the harmonized collector compared to the national gutter collector. The mean difference between collectors was 5.3 mm which is significantly different than 0 (p>0.001). In relative terms, this amounts to 9.4% smaller volumes measured by the harmonized collectors compared to the gutters. The slope of the Deming regression line was 0.814 (C.I.: 0.792, 0.836) and the slope of the regression line of differences on means from the Altman-Bland plot was -0.203 (C.I.: -0.230, -0.176), both indicating significant proportional bias. When calculating RM ANOVA, the harmonized collectors again measured significantly lower precipitation quantities than the national gutter collectors (p=0.0012).

Fig. 4 - Scatter plot with Deming regression (A) and Altman-Bland plot (B) showing the agreement in volumes between national and harmonized throughfall collectors.

A few other investigations showed larger volumes measured by gutters ([9], [7]) but studies showing no difference ([17]) or inverse results ([18]) also exist. There might be several reasons for this relatively important disagreement between collectors in our case. As pointed out by Bleeker et al. ([5]) the wrongly calculated (or measured) area of collectors very frequently leads to overestimation or underestimation of precipitation. Falsely determined area can also easily explain proportional bias in either of the collectors. The area should be defined with 0.5% precision according to the World Meteorological Organisation (after [22]) or 2% precision according to the ICP Forests Manual ([6]). The design of our gutters is similar to the design of the collector number 11 in the study of Bleeker et al. ([5]). For this collector the largest negative deviation (-6.4 %) between the collector area reported by the participating country and the area measured was observed, which shows the difficulty of properly measuring the collecting area of this type of collector. Bleeker et al. ([5]) emphasized that when the collector rim is wide enough the inclusion of the area of half the rim width might contribute to better estimates, but for this type of gutter it is difficult to even determine what is the collector rim and what is not. The part of the gutter between the slits can also contribute to the capture area of the collector. Additional research, best with some simulation measurements, would be needed to correct the collecting area estimates.

The presence of any obstacles for air flow around the collectors (e.g., a bird ring) can also influence precipitation estimates ([20]). In our case a bird ring was mounted on the harmonized collectors only, and that could theoretically explain the lower volumes in this collector. However, we do not regard the bird ring as important due to its slender design. The raindrop splash out of the collector is another reason for poor estimates ([5], [22], [24]) which should be ruled out in our case due to the collector designs.

Canopy interception

The ratio between throughfall and bulk precipitation represents the inverse of canopy interception. To calculate the interception mean precipitation per period of all collectors of each type was divided by the mean bulk precipitation per period measured by both collector types (Fig. 5). Mean interception for the observation period was -0.81% and 9.05% for gutters and harmonized funnels, respectively. The difference in canopy interception between collectors was significant (p<0.001) with national collectors estimating a 9.9 percentage points lower interception of the forest canopy. The value obtained from gutters differs from previously reported interceptions for Pinus sylvestris forests ([12], [15]), whereas estimates of interception using harmonized collectors are closer to literature values despite being in the lower range of these reported values. This indicates that gutter precipitation quantities are most probably overestimated, and the values measured with the harmonized equipment are more realistic.

Fig. 5 - Canopy interception derived from national and harmonized throughfall collectors. Means ± standard errors are presented.

Chemistry data: agreement in concentrations of ions

The data on ion concentrations were generally more variable than quantity data. For bulk deposition no significant disagreement was found when comparing national and harmonized collectors, which was expected from the similar collector designs. For bulk deposition concentrations absolute mean deviation between different types of bulk collector ranged between 0.16% (Ca2+) and 29.1 % (H). Deviation below 5% was found for Na, Ca2+, Mg2+, Cl-, NO3- and SO42-, below 15% for K+, Mn3+, NH4+, NO2-, total N and DOC, and above 15% for H, alkalinity and electroconductivity. Relatively high deviation of H and alkalinity between different collector types was also reported by Bleeker et al. ([5]), indicating the difficulty of measuring these two parameters accurately.

An even larger scatter was observed when analyzing throughfall chemistry data, which caused larger problems when evaluating the agreement. Additionally, data sets for individual ions and other compounds were small, causing further problems. Tab. 1 shows the summary agreement analysis for ions and other chemical parameters measured.

Tab. 1 - Summary table of volume-weighted mean concentrations and range of concentrations for harmonized and national throughfall deposition collectors. Relative and absolute deviation of harmonized collectors with respect to national collectors (negative values indicate lower measured concentrations in harmonized collectors). Significance of fixed and proportional bias between collectors according to the Altman-Bland method. (*) for alkalinity the unit is µeq L-1 and for conductivity µS cm-1.

No disagreement was found for Na, Ca2+ , Mg2+, Mn3+, NO2- and SO42-. Of these, mean deviations were less than 10 % for Ca2+, Mg2+, Mn3+ and SO42-. For Na and NO2- larger but non significant deviations were detected. There were minor deviations found for K+, NO3- and total nitrogen which were significant with either fixed or proportional bias. Relatively small but persistent deviations were observed for DOC and NH4 with harmonized collectors measuring lower concentrations. Larger, significant, persistent and more relevant disagreement was found for Cl- and H+ concentrations. No final explanation is found for high disagreement for chloride ions, especially if we take into account the relative passivity of this ion in canopy interactions ([16]). According to information from the manufacturer of the plastic pipes gutters are made of such material that no Cl- ions should be added to the solution. However, in gutters there are no meshes to prevent litter and other particles from entering the solution and chloride could be derived from these; this still has to be investigated. Significant fixed bias and large positive deviation (95.5%) were found for alkalinity; this deviation however was caused by some very low measurements which magnified the relative deviation.

Seasonal variation in concentrations of ions and other parameters of throughfall precipitation measured by harmonized and national collectors is shown in Fig. 6.

Fig. 6 - Concentrations of ions and other parameters of throughfall precipitation measured by harmonized and national collectors during the investigation period from July 2009 till October 2010.

Deviations of volume-weighted mean concentrations from the harmonized collectors relative to the national collectors were negative for all ions except for NO3-, where the mean deviation was almost zero, and NO2-. There are many possible reasons for lower concentrations in the harmonized collectors and higher concentrations in the national collectors. Gutters are generally more difficult to clean properly after each sampling, which is crucial to remove algal growth and other dirt capable of causing biochemical transformations and/or additions of some ions and compounds (e.g., DOC, Cl-). Further, due to the larger collecting area per collector and lower collector height gutters may be more efficient in collecting dry deposition ([5]). This could also help to explain the Cl results as Cl is often deposited as dry deposition.

Spatial representativeness

In this study the area covered by each collector type was considerably different. The total sampling areas of ten gutters and thirty harmonized collectors were 1850 and 5879 cm2, respectively. Both coverages are beyond the minimal requirements according to the ICP Forests Manual ([6]), but only the harmonized collector system is within the limits suggested by Bleeker et al. ([5]), who for spruce forest suggested using at least 26 collectors to reach the accuracy of 10% of the population mean.

Due to their oblong design gutters cover a larger spatial gradient in the canopy above them, which would cause lower variability in concentrations and volumes measured ([7]). However, the 3.18-times larger total area of the harmonized collectors may have compensated for the weakness of spot measurements of harmonized collectors, so that the variability in quantities of the collectors was not significantly different. Mean coefficients of variation in precipitation quantity of national and harmonized collectors were 13.6% and 10.0%, respectively.


Within this study a harmonized collector proposed by the ICP Forests Expert Panel on Deposition was compared with the Slovenian collectors. In terms of quantities and concentrations of ions and compounds only minor disagreement was found for bulk deposition, which was expected due to the similar funnel-type designs of both collectors.

For throughfall quantities significant disagreement was found. National collectors measured 9.4% higher volumes than harmonized collectors, which we mainly attributed to the difficulty of properly measuring the real collecting area of the national collector. Proof that the national collectors overestimated the volumes rather than that the harmonized collectors underestimated them was the comparison of interception. No interception (-0.8%) of Pinus sylvestris forest was perceived using national collectors, which is very unlikely considering the literature reports. The interception estimated using harmonized collectors was closer to the literature values (9.0%).

Regarding the concentrations of ions and other compounds, gutters again in almost all cases overestimated these concentrations although bias was not significant or not relevant for a large part of the ions and compounds measured (Na, Ca2+, Mg2+, Mn3+, NO2-, SO42-, K+, NO3-, total N). High and persistent deviations (up to 48%) between collectors throughout the investigation period were found for Cl-, H and DOC. No final explanation is found yet for the disagreement in some of the chemical parameters, although poor washing of gutters after each sampling is suspected to cause the observed deviation.

Several statistical approaches were tested within this research. Each of them with certain advantages and disadvantages and it is preferable to test the agreement using several approaches. The Altman-Bland method has proved simple and efficient in visualization of the agreement between methods of measurement but also in inference on the significance of fixed and proportional bias. Deming regression is probably the most general, easy to calculate and should be the first choice in method comparison studies.

The effort has been made across the European intensive forest monitoring network to harmonize the collectors for assessing the quantities and chemistry of bulk and throughfall forest depositions. A large diversity of designs, total collector areas and collector placements exists throughout Europe. Previous studies have shown large differences between currently used national collectors in terms of precipitation quantities and concentrations of ions and other compounds. The funnel-type 16 cm diameter collector has been chosen as the harmonized collector. To check its performance and the agreement with the national collectors, field investigations across Europe coupled with proper statistical data analysis are needed. For the Slovenian case, the harmonized collector system proved to be the better choice for several reasons: more realistic and precise throughfall volume estimates, and easier collector cleaning. For historic data, obtained by national collectors, calibration of results is possible using the results of this comparison. Similar comparisons however will be needed in other forest types with larger spatial variability. The harmonized collector system has the disadvantage of large sample size (3-times as many collectors) which makes the sampling much more labour intensive (up to 4-times more time was needed per one sampling activity) and consequently more expensive. The solution would be fewer collectors (e.g., 10-15), but in that case additional surveys should be performed in this respect if such reduction of sample size is feasible and acceptable in terms of spatial representativeness.


The study was supported by the FutMon project (LIFE07 ENV/D/000218), COST FP0903 and SFI programme group P4-0107.


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Zlindra D, Eler K, Clarke N, Simončič P (2011).
Towards harmonization of forest deposition collectors - case study of comparing collector designs
iForest - Biogeosciences and Forestry 4: 218-225. - doi: 10.3832/ifor0586-004
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Paper ID# ifor0586-004
Title Towards harmonization of forest deposition collectors - case study of comparing collector designs
Authors Zlindra D, Eler K, Clarke N, Simončič P
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