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Report - ICP Forests

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56 3. Intensive Monitoring<br />

centrifugation of soil samples and saturation extraction had rarely been used for soil solution<br />

collection.<br />

Evaluation of soil solution data is based on single samplers that are of a defined type (i.e.<br />

tension and zero tension lysimetry) and that sample soil solution in a defined layer and soil<br />

depth. On each plot more than one sampler may exist in each sampling depth. Most countries<br />

submit data for one ‘sampler’ per soil depth and plot. This ‘sampler’ can represent a mean of<br />

different single measurements per soil depth and plot or one single measurement of a sample<br />

that was pooled from different lysimeters in one soil depth of the same plot. If data for more<br />

than one lysimeter per soil depth and plot were submitted, means were calculated for each<br />

sampling depth and plot and evaluated as one ‘sampler’.<br />

Data availability was best for the calculation and evaluation of (Ca+Mg+K)/Al ratio. Data were<br />

available for 2054 samplers on 263 plots. From the total of these, only those samplers were<br />

included in the analysis from which data were available for at least 6 months per year in 2006<br />

and in at least three more previous, consecutive years, i.e. complete data availability in the years<br />

2003 – 2006 was a criterion for plot selection. This resulted in 160 plots with 396 soil solution<br />

samplers in different soil depths.<br />

Mean sampler pH and trend of pH were calculated for all samplers that continuously provided<br />

data from 2000 to 2006 with at least four measurements per monitoring year.<br />

The calculation of trends of BC/Al ratio used all samplers that continuously provided data from<br />

2000 – 2006 and at least six single measurements per monitoring year. Following these criteria,<br />

linear trends for BC/Al were calculated for 111 samplers on 58 plots and for pH 166 samplers at<br />

66 plots. From single measurements annual arithmetic means were calculated. Trends were<br />

evaluated using regression coefficients and significance of linear regression analysis of<br />

monitoring year and annual mean.<br />

Soil solution has been sampled in different soil depths. The manual of <strong>ICP</strong> <strong>Forests</strong> (Submanual<br />

on Soil Solution and Analysis, updates 6/2002) (ANONYMOUS, 2004) suggests sampling<br />

depths for soil solution chemistry assessment of 10-20 cm (within the rooting zone) and 40-80<br />

cm (below the rooting zone). Both suggested sampling depths are well represented; about 77%<br />

of all samplers are located in the upper 20 cm and 17% below the rooting zone. About 10% of<br />

the samplers had been located below 90 cm soil depth. Table 3.3.2.2-1 gives an overview on<br />

data availability for all monitoring years of parameters that are mandatory or optional according<br />

to the <strong>ICP</strong> <strong>Forests</strong> manual. Even though those parameters are mandatory to assess following the<br />

current version of the <strong>ICP</strong> Forest manual they are not available from all plots.

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