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Table 1 Investigated parameters that may influence \( {\text{N}}{{\text{O}}_3}{^{ - }_{\text{seepage}}} \) with measurement depth/layer and time/period

From: Causes for the small scale variability of nitrate concentration in seepage water of an N saturated mature spruce stand

Parameter group

Parameter

Unit

Layera

Time/period of measurment

Number of variables

Nitrat in sepage water

NO 3

mg l−1

4

April–October

 

N input via throughfall

Input of NH +4 , NO 3 and total inorganic N

mg m−2

−1

July–October

3

Average volume weighted concentration of NH +4 , NO 3 and total inorganic N

mg l−1

−1

July–October

3

Water input and substrate availability in the organic layer

Input of water

l m−2

−1

July–October

3

Dry weight organic layer

g dw m−2

0

October

1

Depth of organic layer

cm

0

October

1

N-turnover parameters in the organic layer

Net N mineralization, net nitrification, gross nitrifikation

mg N day−1 kg−1 dw

0

July–August

3

Pools of NH +4 and NO3

mg N kg−1 dw

0

2

N-uptake parameters

Tree root biomass (<2, 2–5, >5 mm)

g m−2

0–4

October

15

Vegetation cover of mosses, oxalis, other vascular plants

% coverage

−1

July

3

Chemical soil parameters

pH in H2O and KCl

 

0–4

October

10

N and C content

%

0–4

October

10

C/N

Ratio

0–4

October

5

Physical soil parameters

Bulk density

g cm−3

1–4

October

4

Pore volume of macro- (>50 μm), meso- (50–10 μm) and fine pores (<10 μm) and whole pore volume

vol.%

1–4

October

16

Grain size distribution

% sand, % silt, % clay

1–4

October

12

Stand parameters

Distance to next trees

cm

−1

July

1

Breast hight diameter of the next trees

cm

−1

July

1

Basal area of trees within a radius 4 m

cm2

−1

July

1

Number of trees in a radius of 4 m

n

−1

July

1

Sum of variables

    

93

  1. The number of variables which are finally tested with \( {\text{N}}{{\text{O}}_3}{^{ - }_{\text{seepage}}} \) is the result of the parameter/-s multiplied by the number of investigated soil layers
  2. dw dry weight
  3. a−1 = above organic layer, 0 = organic layer, 1 = mineral soil 0–10 cm, 2 = mineral soil 10–20 cm, 3 = mineral soil 20–30 cm, 4 = mineral soil 20–30 cm