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引用次数: 3

摘要

为了无线电传播的目的,已经对五大湖水域的电导活度值进行了一项重要的检查。在实验室测量的电导率值与从场强测量中推断出的电导率值之间的差异表明,这是实验误差和使用故障场强标准来计算理论场强的结果。后一种误差来源是标准曲线本身误差的结果,所有的误差都是由于在水中传播时使用的15个选择常数造成的。电导值推导自l。在实验室对水样的测量中,如果它与发表在《科学》和《科学》上的结果没有任何不同,就会显示出明显的差异。, lvlty地图。al:电导率的季节变化很大,在某些情况下接近2倍,而在某些情况下,电导率是一个很小的复杂因素。
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Electrical conductivity of the Great Lakes
A cri tical exa mination has bcen made of the electrical co ndu ct ivity valu es ass igned, for radio propagation purposes, to t he waters of the Great Lakes. Discrepa ncies between co nductivi ty values measured in t he laboratory and t hose deduced from fi eld s t rength measurements are shown to have been t he resul t of both expenmental error and the use of faul ty standard t heoretical fi eld strength cmves. The latter source of errol' is the result of e rror in thc standard curves t hemselves and lll t he usc of a d lelectn c cons tant of 15 for overwater propagation. Condu ctivi ty valu es derived frOl.n laboratory m easuremen ts of water sa mples are sign ifi ca ntly d ifferent from those published In co nd uc!,lvlty maps. Lal:ge seasonal var iat ions in conductivity, approac hi ng a factor of two 11l some cases, a rc a slgnlfi cant complicating fac tor.
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