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Throughout the taiga zone the dominant soil type is the podzol, a product of the intense leaching characteristic of this area of moisture surplus.
As the moisture surplus diminishes, leaching becomes less intense, and true podzols give way to gray and brown forest soils, which are less acidic and have a much greater organic content and a higher natural fertility.
The moisture surplus caused by low temperatures results in the area's being poorly drained, and the limited and discontinuous vegetation cover provides little organic matter; moreover, this matter decays slowly, and the soils are highly acidic.
A water balance model (monthly precipitation minus monthly ET) defines three broad climate zones along the sampling transect: an arid zone with moisture deficit in every month, an intermediate zone with moisture deficit during low-rainfall summer months and moisture surplus during high-rainfall winter months, and a humid zone with moisture surplus during every month.
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Risk is highest in areas with extended high annual rainfall, high soil moisture and surplus water.
Mrs. Kraft has learned that she cannot plant bulbs in her boggy soil in Islip, because if the deer don't eat them, the surplus moisture rots them.
Mrs. Kraft has learned she cannot plant bulbs in her boggy soil in Islip, because if the deer don't eat them, the surplus moisture rots them.
Surplus moisture was removed with cotton tipped applicator.
Well-drained soil will allow the plant to receive the necessary moisture without maintaining surplus water around the root system, which may cause root rot.
Soil storage is also independent from the other hydrologic dynamics, except that groundwater recharge, calculated as infiltration below the zone of evapotranspiration, is calculated only from surplus, after soil moisture capacity has been filled.
Squeeze out any excess moisture.
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