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Native Plant Synoptic Garden<br />

15<br />

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significant amounts of potassium available in the soil is desirable, <strong>and</strong> has not been found to be<br />

limiting in the Puget Sound region (Chalker-Scott, 2004).<br />

At high levels, aluminum can be detrimental to plants. Aluminum can hinder calcium<br />

<strong>and</strong> magnesium uptake <strong>and</strong> cause subsequent deficiencies (Marschner, 1995). “Aluminum<br />

sensitivity varies greatly with plant type; for instance, rhododendrons can tolerate very high levels<br />

of aluminum” (UMass, 2004). The level of aluminum in the soil analysis was found to be 68<br />

ppm, which is in the low to medium range. Typical soils range from 10 to 300ppm, so the soils in<br />

the proposed areas are at a tolerable level (UMASS, 2004). If aluminum levels should reach<br />

levels that would begin to cause problems, liming can lower the level of aluminum (UMASS,<br />

2004).<br />

“Phosphorus aids plants in using the energy from <strong>photo</strong>synthesis to power the plants<br />

metabolism” (UMASS, 2004). A phosphorus deficiency can limit healthy plant growth <strong>and</strong> result<br />

in weak root systems; signs of a deficiency can be abnormal size <strong>and</strong> number of leaves.<br />

Represented by blue in figure six, phosphorus levels on site were low but do not mean that there<br />

is a deficiency problem (Umass, 2004). Phosphorus deficiency does not tend to be a factor<br />

affecting plant health in Western Washington (Chalker-Scott, 2004). Most phosphorus tends to<br />

accumulate near the soil surface <strong>and</strong> does not move readily in soil because it is tightly adsorbed to<br />

soil particles (Harris et la., Umass, 2004). Since phosphorus tends to be at or near the surface, too<br />

much disturbance of the soil surface can lower phosphorus levels (Harris, 2004). Since the soils<br />

located at the Graham Visitors Center site are low in phosphorus, it may be necessary to fertilize<br />

with a phosphorus enriching fertilizer to help newly planted trees <strong>and</strong> shrubs grow. Remember<br />

though that phosphorous is generally not limiting in Puget Sound soils, so it would be advisable<br />

to first monitor shrubs for phosphorous deficiencies symptoms before application. Symptoms<br />

would include “distorted, dark green leaves with abaxial reddening or purpling with the<br />

symptoms being more common with younger plants that have less developed root systems”<br />

(Chalker-Scott, 2004). If necessary a soil analysis of soil immediately within the plant’s root<br />

zone coupled with simultaneous tissue analysis could be helpful in detecting a true phosphorous<br />

deficiency.<br />

Nitrate <strong>and</strong> ammonium were both found at low levels within the soil sample; they are<br />

represented by light blue in Figure six. Nitrate is a soluble nutrient that is made available to<br />

plants by mass flow of water within the soil (Harris, 2004). Because of mass flow, nitrate can<br />

also be leached through the soil too quickly or to depths that do not allow for roots to absorb it<br />

(Harris, 2004). “In contrast ammonium ions do not move freely with soil water, the positively<br />

charged ammonium ions are adsorbed onto soil particles” (Harris, 2004). So instead, ammonium<br />

is converted into more readily available nitrate by soil organisms. This process is called

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