Coastlines

Figure XVI-1 and the related discussion first appeared in 1960 [1], and since then a very useful mathematical approach to irregular surfaces has been applied to the matter of surface area measurement. Figure XVI-1 suggests that a coastline might appear similar under successive magnifications, and one now proceeds to assume that this similarity is exact. The result, as discussed in Section VII-4C and illustrated in Fig. VII-6, is a self-similar line, or in the present case, a self-similar surface. Equation VII-21 now applies and may be written in the form...

Seawater. Salt extraction from seawater is done by most countries having coastlines and weather conducive to evaporation. Seawater is evaporated in a series of concentration ponds until it is saturated with sodium chloride. At this point over 90% of the water has been removed, and some impurities, CaSO and CaCO, have been crystallized. This brine, now saturated in NaCl, is transferred to crystallizer ponds where salt precipitates on the floor of the pond as more water evaporates. Brine left over from the salt crystallizers is called bitterns because of its bitter taste. Bitterns is high in MgCl2, MgSO, and KCl. In some isolated cases, eg, India and China, magnesium and potassium compounds have been commercially extracted, but these represent only a small fraction of total world production. 

Winds blowing across the surface of the world s oceans are converted into waves. The total amount of power released by waves breaking along the world s coastlines has been estimated to be 2 to 3 million megawatts, equivalent to the output of about 3,()0(1... 

Wave size is determined by wind speed and fetch, the distance over the oceans surface which the wind travels. Favorable wind energy sites are generally western coastlines facing the open ocean such as the Pacific Coast of North America and the Atlantic Coast of Northern Europe. Norway, Denmark, Japan, and the United Kingdom are the world leaders in wave energy technologies. 

The reduction of SO, is best achieved by reducing the sulfur content of the fuel oil. Ship engineers arc required to replace high-sulfur fuel with expensive higher-grade oil fuel as their ships approach coastlines where strict pollution restrictions apply. 

The mechanism of Self-organized criticality, a concept first introduced by Bak, Tang and Wiesenfeld [bak87a], may possibly provide a fundamental link between such temporal scale invariant phenomena and phenomena exhibiting a spatial scale invariance - familiar examples of which are given by fractal coastlines, mountain landscapes and cloud formations [mandel82],... 

Identification and Protection of Coastlines most sensitive to Erosion (e.g., Charlottetown, P.E.I. near Vancouver, B.C.). 

Ironically, despite all this scientific progress, modern fiberoptic cables went into service during a decade of chemical catastrophes more reminiscent of the old Leblanc factories than of optical fibers superpurity. On December 3, 1984, a cloud of deadly methylisocyanate gas leaked from a Union Carbide plant in Bhopal, India the gas killed more than 3000 people and injured up to 25,000. Two years later in Europe, a Sandoz chemical factory spilled 30 tons of chemicals into the Rhine River, killing fish for 120 miles downstream. In North America, the Exxon Valdez oil tanker spilled crude oil over 1000 miles of Alaskan coastline in 1989. 

Another challenge is selecting an appropriate location for the turbine, due to the highly localized nature of wind. Low-cost anemometers may help alleviate this problem, but time must be spent to collect a sufficient amount of data [10]. Areas particularly suited to wind power because of their typical high wind velocities include coastlines, high ground, and mountain passes [12]. Wind power does not need water, so it is suitable for dry areas. 

Many inland depression areas in deserts are former lake areas in which open water was present during the early Holocene. Former river delta sequences and coastline features (e.g. coastal terraces) may still be visible. 

All soils contain soluble salts, but their concentration is low. The salt content of most arid soils is, however, much higher. Salts in desert soils are usually derived from three main sources (1) deposition of wind-blown salt spray or dust (2) in situ weathering of salt-containing rocks or sediments, and (3) upward movement with the capillary flow from a shallow salty groundwater. Along the coastline, some salinization may occur through intrusion and flooding by seawater. 

A blank and also a sterile solution containing Pb2+ of methyllead compounds showed no Pb content in the methanolic solution after the same treatment. The author concluded that Me4Pb was produced in the biomethylation of Pb2+ by bacteria123. Thompson and Crerar122 also observed that about 0.03% of lead as Pb(NC>3)2 underwent methylation and trimethyllead acetate, (CH3)3PbOAc, was methylated nearly quantitatively in incubation experiments with marine sediments from the British Columbia coastline. 

Position of the coastline. The position of the coastline with reference to the position of the aquifer intake area should remain constant. This is particularly critical along coastlines with gently sloping topography and shallow water on the continental shelf. In such areas, lateral shifts of the shoreline of more than 200 km have been common during the past 20,000 years. 

Zhejiang province is located in eastern China and has a relatively developed economy. The main plain of the northeastern part of the province was formed by alluvium, and coastal, lake and marsh sediments. There are several small plains along the eastern coastline formed by alluvium and marine sediment. These plains have undergone thousand of years of agricultural cultivation. 

The biodiversity of Mangrove ecosystems is the most profound in the islands and coastline of the Indo-West-Pacific region, where the occurrence of 44 varieties has been reported. On the Atlantic Ocean coast Mangrove ecosystems are especially widespread in the Caribbean region. The chemical composition of plant species and soils of Mangrove ecosystems have been recently discussed (Dobrovolsky, 1994). 

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