A chronosequence of soils near the Franz Josef Glacier
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Authors
Date
1968
Type
Thesis
Fields of Research
Abstract
One method of studying the effects of Time as a Soil Forming Factor is the recognition and investigation of a Chronosequence, wherein four of the five Soil Forming
Factors are kept constant or ineffectively varying. Thus, observed differences between soils of different ages forming a sequence are deemed to be the result of the
lapse of varying intervals of Time since the initiation of soil formation.
It is helpful to assign accurate ages to the soils of such a Chronosequence, allowing the derivation of Chronofunctlons, rate equations of soil formation. In many
parts of the world, intermittent alteration of the Earth's surface by mudflows, volcanism or processes of glaciation
has provided areas of terrain whose relative and absolute
ages can be determined by the techniques of the botanist
and geomorphologist with some degree of confidence. Such an area occurs in the vicinity of the Franz Josef Glacier,
which has at various known times deposited morainic and
alluvial debris in defined places. A succession of plants
has colonised these ground-surfaces, and on them a
Chronosequence of soils has developed concomitantly,
Deposition of organic matter in and upon the parent
material initiates depth-gradients of many soil
characteristics such as reaction, bulk-density, and
contents of organic carbon, nitrogen and various fractions
of phosphorus. Under the influence of a warm and
extremely humid climate the processes of weathering and
leaching within the soil profile are responsible for
striking gains, losses, transformations and
redistributions of many organic and inorganic constituents,
Some of these changes have been studied during the
past four years, following an earlier investigation by the
present author of the most youthful soils of the Chronosequence in 1962 and 1963. This initial work traced
the development of six ecosystems 0, 6, 12, 25, 45 and 55
years of age. Spectacular accretion of nitrogen,
especially, showed no indications of having reached any
apparent steady-state in the oldest ecosystem, despite the
impending elimination from the botanical succession of
Carmichaelia grandiflora, a native legume, Clearly, it
was important to determine nitrogen contents and the point
of steady-state of nitrogen in soils older than 55 years,
which lack any plants known to be capable of nitrogen
fixation. In addition, the recognition of older soils, whose position on an orderly continuum of soil development
could be assumed with some degree of confidence, would
provide considerable information about rates of change of
many other aspects of soil morphology, mineralogy and
physical and chemical characteristics.
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