Soil Surface Sealing and Crusting

Selected papers of the International Symposium on Soil Crusting, Chemical and Physical Processes, May 30-June 1, 1991, Athens, Georgia, USA

Ed.: J. W. A. Poesen; M. A. Nearing

1993. 139 pages, 45 figures, 27 tables, 3 plates, Catena ISBN 978-3-923381-33-3, US-ISBN 978-1-59326-232-7, 17x24cm, 510 g
Language: English

(Catena Supplements, Volume 24)

ISBN 978-3-510-65365-2, bound, price: 71.00 €

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BibTeX file


soil materialsurfacehumid soilerosion


Synopsis top ↑

The boundary between soil and atmosphere is an important and active place. It controls to a large extent the flux of nutrients, water, gasses, and heat to and from the underlying soil and so it has a direct and dramatic influence on the conditions of the soil below the interface, the microbes, animals, and plants that live in the soil, and the amount of surface runoff generated from excess rainfall. The upper few millimeters of soil is the gateway to the soil below, and thus it has a direct and dramatic influence on the world around us.
While the characteristics of the thin layer at the soil surface are important, they are also very much different from those of the soil underneath. Enormous amounts of energy and very high transient forces are imparted to the soil surface by impacting raindrops which break down aggregates, dislodge soil particles, and compress the upper few millimeters of soil. The physical disruption is aided by chemical processes, including dispersion, which further act to break down soil aggregates and greatly alter the surface characteristics of the soil. The resulting dense surface layer of soil is referred to generally as a surface seal. When the seal dries other physical and chemical factors cause a crust to form, which continues to have a dominating influence on gas, vapor, and heat exchange between soil and atmosphere, as well as an effect on seedling emergence.
While soil surface sealing and crusting are certainly functions of local soil properties and climate, the processes are recognized and studied worldwide. At the “International Symposium on Soil Crusting: Chemical and Physical Processes”, which was held May 30 - June 1, 1991 at the University of Georgia, Athens, Georgia, USA, 37 papers/posters were presented by representatives from every continent. This CATENA SUPPLEMENT includes selected papers from the symposium.
The first 4 studies reported here focus on quantifying changes in runoff and erosion amounts as a function of soil surface changes. Le Bissonnais & Bruand studied sealing and crusting on field plots under natural rainfall in Western Europe, and in particular they investigated seasonal differences. Nishimura & Nakano investigated sealing using a rainfall simulator and laboratory soil pans packed with an Andosol from Japan. Both of these studies also included a micromorphological study of the soil surface layer using scanning electron microscopy. Luk &; Cai performed a field study of the sealing and crusting characteristics of a loessial soil from North China, and specifically addressed the issues of how slope gradient and antecedent crusting influenced runoff and soil loss during a storm. Chiang, Radcliffe &; Miller studied the sealing of four soils from the southeastern and mid-western parts of the United States. Particularly interesting was the observation that even these soils, which had relatively high sand contents, experienced reductions in hydraulic conductivity due to surface sealing.
The following three papers investigated the effects of dispersion on sealing, structural stability, and infiltration. So h Cook studied the relationships between soil structural stability and hydraulic conductivity using several clay soils from Australia. Rengasamy, Naidu, Chan &: Chartres related results from a modulus of rupture test to exchangeable sodium percentage for several Australian soils. Norton, Shainberg & Bradford showed a reduction in soil dispersion and sealing resulting from application of gypsum to three soils from the eastern United States. Thus they introduce a potential control mechanism for surface sealing problems.
The study of Auerswald and that of Zhang &; Miller were designed to delineate the effects of moisture content on soil stability and erosion. Both studies showed that a decrease in soil moisture prior to rain produced a less stable surface and more soil loss for the same amount and intensity of rain. Lehrsch, Sojka, Carter & Jolley investigated reductions in aggregate stability as a function of freeze-thaw cycles. They determined that aggregate moisture at the time of freezing influence the degree of the freezing effects on aggregate stability. The paper by Huang &; Bradford introduces an innovative technique for quantifying density and roughness of surface seals. These are measurements which to date have been difficult to make and are important for better understanding and characterizing surface seals and crusts.

Table of Contents top ↑

Y. Le Bissonnais & A. Bruand
Crust micromorphology and runoff generation on silty soil materials
during different seasons 1
T. Nishimura, M. Nakano & T. Miyazaki
Properties of surface crusts of an Andisol and their effects on
soil-hydrological processes 17
S.H. Luk, Q.G. Cai & G.P. Wang
Effects of surface crusting and slope gradient on soil and water
losses in the hilly loess region, North China 29
S.C. Chiang, D.E. Radcliffe & W.P. Miller
Comparison of seal hydraulic properties between Ultisols and Alflsols/
Mollisols 47
H.B. So & G.D. Cook
The effect of slaking and dispersion on the hydraulic conductivity
of clay soils 55
P. Rengasamy, R. Naidu, T.A. Beech, K.Y. Chan & C. Chartres
Rupture strength as related to dispersive potential in Australian soils 65
L.D. Norton, I. Shainberg & K.W. King
Utilization of gypsiferous amendments to reduce surface sealing in
some humid soils of the eastern USA 77
K. Auerswald
Influence of initial moisture and time since tillage on surface
structure breakdown and erosion of s loessial soil 93
X.C. Zhang & W.P. Miller
The effect of drying on runoff and interrill erosion of crusted soils 103
G.A. Lehrsch, R.E. Sojka & P.M. Jolley
Freezing effects on aggregate stability of soils amended with lime
and gypsum 115
Chi-hua Huang & J.M. Bradford
Application of a laser scanner to quantify properties of soil crusts 129