Hydrothermal vents: a novel theory of illumination

D. J. Bogorff
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Abstract

There are many theories revolving around the source of non-thermally based visible light emissions from deep-sea hydrothermal vents. Although many of these theories have been proven possible in a controlled laboratory environment, none have been directly linked to hydrothermal vents through on-site experimentation and evaluation. Nor have any of them conclusively lain to rest the unanswerable and unpredictable source and exact circumstances of this mysterious light. Visible light has been shown to occur in larger than background concentrations intermittently at both black smokers and beehives, in the presence and absence of mineral emissions, and just above and below vent openings. This behavior cannot be explained by crystalloluminescence, triboluminescence, or even chemiluminescence where illumination is dependent on specific physical characteristics of the vent which cannot guarantee the presence or absence of visible light anomalies. These theories are also not restricted to just the vent openings, as many of the physical requirements occur beyond the vent and, in some cases, into the plume. A novel theory of hydrothermal vent illumination by way of amplified C/spl caron/erenkov radiation through internal plume reflection will be presented. This theory includes the already known creation of visible light by muons in seawater created by the bombardment of the Earth by extraterrestrial neutrinos. When these particles enter seawater directly or through collision, they produce a lagging wave of visible light known as C/spl caron/erenkov radiation. This lagging wave, like normal visible light, can be trapped and magnified, as in C/spl caron/erenkov radiation detectors. The large variation in density between exiting plume emission and surrounding seawater may be enough to trap visible light within the base of the plume itself making the visible light from C/spl caron/erenkov radiation appear to be brighter than the surrounding seawater. The variation and unpredictability of extraterrestrial muons in the deep ocean may help account for the appearance, disappearance, and reappearance of light at some hydrothermal vents. It would also help explain the presence of illumination in a variety of hydrothermal vents and differing plume emission. Taking known data and theory from actual visits to deep sea hydrothermal vents combined with known data of present theories of illumination and experimentation, a composite holistic view of this quandary will be evaluated, and a theoretical written model will be composed. This new theory hopes to satisfy data obtained on-site at the hydrothermal vents by previous study, as well as attempt to bring some sort of closure to the unpredictable and mysterious question of hydrothermal vent illumination.
热液喷口:一种新的照明理论
有许多理论围绕着深海热液喷口的非热基可见光辐射的来源。虽然这些理论中的许多已经在受控的实验室环境中被证明是可能的,但通过现场实验和评估,没有一个与热液喷口直接相关。对于这神秘之光的无法回答的、不可预测的来源和确切的情况,他们也没有一个能彻底地加以解释。在黑烟和蜂房,在有或没有矿物排放物的情况下,以及在排气口的上方和下方,可见光线间歇性地以大于背景浓度的形式出现。这种行为不能用晶体发光、摩擦发光甚至化学发光来解释,因为化学发光的照明依赖于通风口的特定物理特性,不能保证存在或不存在可见光异常。这些理论也不局限于喷口开口,因为许多物理要求发生在喷口之外,在某些情况下,进入羽流。提出了一种通过内部羽流反射放大C/spl碳/叶伦科夫辐射的热液喷口照明新理论。这一理论包括已知的由地球外的中微子轰击地球而产生的海水中的μ子产生的可见光。当这些粒子直接或通过碰撞进入海水时,它们会产生一种被称为C/spl碳/叶伦科夫辐射的可见光滞后波。这种滞后波,像普通可见光一样,可以被捕获和放大,就像在C/spl碳/叶伦科夫辐射探测器中一样。羽流发射和周围海水之间的巨大密度差异可能足以将可见光困在羽流本身的底部,使C/spl碳/叶伦科夫辐射的可见光看起来比周围海水更亮。深海中外星介子的变化和不可预测性可能有助于解释一些热液喷口的光的出现、消失和再现。这也将有助于解释在各种热液喷口和不同羽流喷发中存在的照明。根据深海热液喷口实际访问的已知数据和理论,结合现有的照明和实验理论的已知数据,评估这一困境的综合整体观点,并组成一个理论书面模型。这一新理论希望能够满足以往在热液喷口现场获得的研究数据,并试图在某种程度上解决热液喷口照明这一不可预测和神秘的问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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