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Protocol for the Derivation of Environmental and Human ... - CCME

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Appendix A<br />

Appendix A<br />

Nutrient <strong>and</strong> Energy Cycling Check<br />

1.0 Using Soil Nutrient <strong>and</strong> Energy Cycling Data to Derive Effects-based<br />

Guidelines<br />

Soils are dynamic, open, systems characterized by fluxes <strong>of</strong> energy <strong>and</strong> nutrients. The ability <strong>of</strong> soils to<br />

support plant life depends on <strong>the</strong> coordinated activities <strong>of</strong> a myriad <strong>of</strong> invertebrates <strong>and</strong> microorganisms<br />

that mediate nutrient <strong>and</strong> energy cycles. Decomposition, respiration, <strong>and</strong> organic nutrient cycles are<br />

examples <strong>of</strong> measurable soil processes whose rates may be adversely affected by contaminants.<br />

In <strong>the</strong>ory, <strong>the</strong>se processes should be good indicators <strong>of</strong> soil quality. In practice, however, it is difficult<br />

to integrate currently available literature into <strong>the</strong> derivation process because <strong>of</strong>:<br />

• uncertainties in interpretation <strong>of</strong> results, including variability seen in dose-response relationships<br />

(Denneman <strong>and</strong> van Gestel 1990),<br />

• frequent lack <strong>of</strong> a reference toxicant, <strong>and</strong><br />

• uncertainty over appropriate controls ("acceptability criteria") (Environment Canada 1992).<br />

On <strong>the</strong> o<strong>the</strong>r h<strong>and</strong>, soil process data have <strong>the</strong> desirable property <strong>of</strong> ecological relevance -- <strong>the</strong> use <strong>of</strong><br />

<strong>the</strong>se measures as indicators or predictors <strong>of</strong> ecosystem per<strong>for</strong>mance is well established (see Paul <strong>and</strong><br />

Clark 1989). Fur<strong>the</strong>rmore, data on effects <strong>of</strong> common contaminants on some soil microbial processes<br />

is abundant (see, <strong>for</strong> example, Bååth 1989). A balance is struck among <strong>the</strong>se considerations by using<br />

qualifying nutrient <strong>and</strong> energy cycling data as a check against preliminary soil quality guidelines derived<br />

from single-species bioassay.<br />

The microbial ecology relevant to <strong>the</strong> cycling <strong>of</strong> organic nutrients indicates that contaminant data from<br />

nitrogen fixation, nitrification, nitrogen mineralization, decomposition, <strong>and</strong> respiration studies are all<br />

potentially acceptable <strong>for</strong> use in a checking role against guidelines derived from single species bioassay<br />

(See Section 2.0). Of <strong>the</strong>se, N-fixation <strong>and</strong> nitrification data are preferred, but carbon cycling <strong>and</strong><br />

nitrogen mineralization measures may be used when <strong>the</strong> <strong>for</strong>mer are unavailable or insufficient <strong>for</strong><br />

guideline derivation.<br />

2.0 Nutrient <strong>and</strong> Energy Cycling Processes as Indicators <strong>of</strong> Soil Quality<br />

Because biological activity in soils is dominated by <strong>the</strong> detrital food chain, energy flow is closely linked<br />

to carbon cycling, which is normally observed through measurements <strong>of</strong> decomposition <strong>and</strong> respiration.<br />

O<strong>the</strong>r elements whose cycling rates in soils are mainly functions <strong>of</strong> biological activity include <strong>the</strong> plant<br />

macroelements nitrogen, sulfur <strong>and</strong> phosphorus. Activities <strong>of</strong> microorganisms are primarily responsible<br />

<strong>for</strong> liberating <strong>the</strong>se elements from organic <strong>for</strong>ms (mineralization), <strong>and</strong> making <strong>the</strong>m available <strong>for</strong> uptake<br />

by plants.<br />

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