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• W2040171569 abstract "Abstract Rates of soil development (determined from the slopes of chronofunctions of soil development indices) of a post-incisive chronosequence that formed on a sequence of outwash terraces (ages 5 ka to 1.8 Ma) in the Ljubljana Basin decrease with time (i.e., soil development increases with the logarithm or power of soil age). The development of soil properties can be affected by soil forming factors other than time (climatic fluctuations, intrinsic thresholds), and does not reach a steady state during the observed time-span. Cumulative soil development expressed by weighted means of profile development calculated by combining the four most time-dependent properties (rubification, total texture, pH-decrease, and clay films), however, ceases to increase at about 980 ka; therefore. a steady state could be assumed. Weighted means cease to increase because some of the four properties continue to increase whereas others begin to decrease after 980 ka. Steady state could thus be defined as a stage in soil development when the sum of progressive (those that contribute to the increase in soil development: weathering, translocations, profile differentiation) and regressive (those that contribute to the decrease in soil development or cause the changes in the direction of development: intrinsic thresholds, erosion) processes equals zero (i.e., regressive = progressive). The trends in soil development indices are consistent with the hypothesis that weathering followed by clay translocation were the main pedogenic processes that affected the soils of the Ljubljana Basin chronosequence. Rates of soil development derived from chronofunctions can change if age estimates change considerably. The change in age estimates within the uncertainty intervals for the Ljubljana Basin chronosequences caused the differences in rates that were less than 15% for semi-logarithmic and power chronofunctions, and about 80% for linear chronofunctions. Since most of the Ljubljana Basin chronofunctions were semi-logarithmic or power, the estimated rates would not change significantly if the age estimates changed within the existing uncertainty interval. Compared to chronosequences in other climatic settings (humid, xeric, aridic), the rates of soil development in the humid Ljubljana Basin generally exceed those in other areas, especially in xeric and aridic areas. The rates of soil morphology development seem to depend on the climatic conditions, and generally increase with increasing precipitation, even though some of the properties, such as rubification, may develop faster in xeric than in humid areas." @default.
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• W2040171569 date "1997-03-01" @default.
• W2040171569 modified "2023-09-27" @default.
• W2040171569 title "Rates of soil development of the chronosequence in the Ljubljana Basin, Slovenia" @default.
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• W2040171569 doi "https://doi.org/10.1016/s0016-7061(96)00098-5" @default.
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