Is Horizon Sampling More Powerful

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Presentation transcript:

Is Horizon Sampling More Powerful Than Depth Sampling? Chris Johnson Syracuse University

The ‘Quantitative Pit’ Method

The Method

The Method

The Method

Advantages of Depth Sampling Generally Reproducible: No need for ‘expert’ horizon delineation. Easy (if not using ‘quantitative’ technique). Statistically efficient: not all profiles will have all horizons. Advantages of the Quantitative Pit Method Specifically Sample integrates all soil in the layer. Soil mass per unit area (Mg/ha) is measured directly. No need for bulk density estimate. Bulk density and “coarse fragment” content can be estimated in stony soils.

Horizon Sampling

Horizon Sampling

Advantages of Horizon Sampling Ease of interpretation: Horizonation reflects soil processes. Statistically efficient: Horizons are differentiated by chemistry, texture, organic matter. Chemical properties should be relatively consistent for a given horizon. Depth layers incorporate multiple horizons. Presence/absence of horizons varies in the landscape. Data derived from horizon sampling should be less variable than data derived from depth layers.

Advantages of Horizon Sampling Ease of interpretation: Horizonation reflects soil processes. Statistically efficient: Horizons are differentiated by chemistry, texture, organic matter. Chemical properties should be relatively consistent for a given horizon. Depth layers incorporate multiple horizons. Presence/absence of horizons varies in the landscape. Data derived from horizon sampling should be less variable than data derived from depth layers. Is this true?

Hubbard Brook Watershed 5 Experiment 60 quantitative pits, sampled by depth increment: 0-10 cm, 10-20 cm, 20 cm-C/R In 1983 (before cutting), 30 pits were also sampled by horizon. Whole-tree clear-cut in winter 1983-84 Resampled in 1986, 1991, 1997. 60 quantitative pits each year Horizon sampling carried out: 48 pits (1986) 59 pits (1991) 60 pits (1998)

Average Thickness Where Present (cm) Matching Horizons to Depths 1983 (Pre-Harvesting) Data: Horizon Average Thickness Where Present (cm) E 3.5 Bh 4.3 Bs1 4.9 Bs2 39.6 Compare to 0-10 cm layer Compare to 10-20 cm layer Compare to 20+ cm layer Johnson et al., SSSAJ (1991)

Example: Soil Nitrogen 1983 (Pre-Harvesting) Data: Horizon Mean N (g kg-1) Std. Dev. CV (%) E 1.24 0.86 69 Bh 3.36 1.02 30 Bs1 2.81 0.64 23 Bs2 1.44 0.51 35 Layer Mean N (g kg-1) Std. Dev. CV (%) 0-10 cm 3.60 1.90 53 10-20 cm 2.48 1.31 20+ cm 1.57 0.73 46

Example: Soil Nitrogen   Total Nitrogen Data: Horizon / Layer VarHor VarLayer F Fcritical VarHor < VarLayer? E vs. 0-10 .740 3.61 4.88 1.95 Yes Bh vs. 0-10 1.04 3.47 1.87 Bs1 vs. 10-20 .410 1.72 4.20 1.93 Bs2 vs. 20+ .260 .533 2.05 1.88

Example: Soil Nitrogen Are these differences “important”? Power Calculation: Set: N = 60 a = 0.05 b = 0.75 = Power Horizon Mean N (g kg-1) Detectable Difference ± % E 1.24 0.42 ± 34% Bh 3.36 0.49 ± 15% Bs1 2.81 0.31 ± 11% Bs2 1.44 0.25 ± 17% Layer Mean N (g kg-1) Detectable Difference ± % 0-10 cm 3.60 0.92 ± 26% 10-20 cm 2.48 0.64 20+ cm 1.57 0.35 ± 22% A change of 20%, for example, would be detected using horizons, but not layers.

Exchangeable Calcium F-Test for Equality of Variances: Horizon / Layer VarHor VarLayer F Fcritical VarHor < VarLayer? E vs. 0-10 0.103 0.172 1.67 1.92 No Bh vs. 0-10 0.0918 1.87 1.83 Yes Bs1 vs. 10-20 0.0296 0.0670 2.26 1.90 Bs2 vs. 20+ 0.0256 0.0313 1.22 1.84

Exchangeable Calcium Power Calculation: N = 60 a = 0.05 b = 0.75 = Power Horizon Mean Ex. Ca (cmolc kg-1) Detectable Difference ± % E 0.41 0.156 ± 38% Bh 0.63 0.147 ± 23% Bs1 0.35 0.083 ± 24% Bs2 0.17 0.078 ± 46% Layer Mean Ex. Ca (cmolc kg-1) Detectable Difference ± % 0-10 cm 0.79 0.201 ± 25% 10-20 cm 0.36 0.126 ± 35% 20+ cm 0.19 0.086 ± 45%

Conclusions For total N and exchangeable Ca, the variance of the layer data was always greater than the variance of the horizon data. In 6/8 cases, the difference was statistically significant. Power calculations suggest that sampling by horizon can reduce the detectable difference in concentration by more than 50%. However, estimating chemical pools using horizon data is difficult in stony soils (maybe next year…)