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A linear term of relative humidity (lag 0) was added to the model as another indicator of weather.
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This study evaluates the use of magnetic properties as an indicator of weathering of tropical soils.
As a result, the Rb/Sr ratios of lake sediments should be cautiously used as an indicator of weathering intensity in the catchments.
Therefore, it is necessary to study the geochemistry of Rb/Sr ratio of lake sediments (especially that on short term timescales) particularly before it is used as an indicator of weathering intensity of the catchment.
The Rb/Sr ratios of lake sediments have been suggested as indicators of weathering intensity by increasing work.
Despite the evidence of element leaching during the Pliocene depositional cycle, the geochemical and mineralogical indicators of weathering intensities are largely determined by the nature of the previous cycle units.
The presence of this 500-nm band can also be taken as an indicator of Antarctic weathering (Table 3).
This sensitivity to climatic influences should make the LegIT a good early indicator of surface weathering patterns.
Some studies thus use the Rb/Sr ratios of lake sediments as a potential indicator of chemical weathering intensity in the catchment (e.g. [5]).
Therefore, the Mg depletion found in our AMMs can be explained by weathering in the Antarctic ice for a relatively long period and, therefore, can be taken as an indicator of Antarctic weathering (Table 3).
Yet the high field magnetic susceptibility, a measure of total iron concentration, and strontium isotope values on bulk sediment, an indicator of sediment weathering provenance, are not different in the Marlboro Clay from the immediately underlying Vincentown Formation.
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