Titlebook: ;

Licentious

Ausgangsbedingungen der Politischen Bildung, the most difficult physical parameters to quantify in extrapolating from the laboratory to the soil plot to the watershed (White and Peterson, 1990). Most models of solute transport in aquifers and in soils simply ignore the mineral-water surface area term by combining it with the kinetic rate cons

Paradox

字的誤用

Indicative

Crystal Growth and Morphology: A Multi-Faceted Approach,ence of faceted crystals also holds for almost all inorganic crystals grown in the laboratory and inorganic mineral crystals grown in nature. Examples are the very well known crystals of quartz, gypsum, pyrite, etc. Note that the occurrence of facets on crystals does not depend on the size of the cr

epicondylitis

CREEK

Discrete

The Diffusion-Limited Aggregation Model and Geological Pattern Formation,upied by the random walker) is filled to represent the growth process. The process of launching random walkers from outside of the region occupied by the growing cluster and terminating them when they wander too far from the cluster or ‘sticking’ them to the growing cluster when they reach an occupi

乏味

Structural Evolution of the Mineral Surface During Dissolution Probed with Synchrotron X-Ray Techni) and the epitaxial precipitation of otavite (CdCO.) on calcite (Chiarello and Sturchio, 1994) have been successfully completed .. Roughness of the surface is determined at the angstrom-scale and is a root mean square (r.m.s.) measure of the average peak to trough height of features on the surface.

一大塊

Surface Area of Primary Silicate Minerals, the most difficult physical parameters to quantify in extrapolating from the laboratory to the soil plot to the watershed (White and Peterson, 1990). Most models of solute transport in aquifers and in soils simply ignore the mineral-water surface area term by combining it with the kinetic rate cons

Negotiate

On Mechanisms and Kinetics of Creep by Intergranular Pressure Solution,ers and Ortoleva, 1989, 1990; Merino, 1992), pervasive intergranular pressure solution is an important deformation mechanism, manifested by many types of partially dissolved objects such as grains and fossils (Elliot, 1973; Rutter, 1976). It occurs under conditions ranging from diagenetic to greensc