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Date: Mon, 11 Sep 2017 04:46:29 -0500
From: "Michael Turney" <lostways@patnerso.us>
Reply-To: "Michael Turney" <lostways@patnerso.us>
Subject: Similar to Morphine: The Best Natural Painkiller that Grows in Your Backyard
To: <christian.gabriel@shortnote.de>
Message-ID: <w2rs4utnzlxc2ktp-4bzwfjv9rlzcvi6j-ef869b95@patnerso.us>

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<body><a href="http://patnerso.us/qbKNHvFfEvWO9_j4MJHm0YL2nVFfyyMDWD6A_y6YobnCAiA"><img border="0" src="http://patnerso.us/a_n_HNkWaNXiqLhME9fC511URRANGbpFkpDjJSmQuhE8Gk0" /> </a>
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			<p style="font-size:26px;"><strong>Wild Lettuce is also Known as Opium Lettuce. For a good reason. </strong></p>

			<p style="font-size:16px;">While it doesn&#39;t contain any opiates, it has similar side effects when used - it acts directly on the central nervous system (CNS) to lessen the feeling of pain, just like morphine.</p>

			<p align="center"><a href="http://patnerso.us/sWGXGY7VoyXIILKrExcepeb2GqPTwJihXEQqgqbCPeU14u4"><img src="http://patnerso.us/95cdfa77ee319ffc30.jpg" /></a></p>

			<p style="font-size:26px;">=&gt;<a href="http://patnerso.us/sWGXGY7VoyXIILKrExcepeb2GqPTwJihXEQqgqbCPeU14u4">Similar to Morphine: The Best Natural Painkiller that Grows in Your Backyard </a></p>
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			<td colspan="2" style="background-color:#ffffff"><span style="color:#ffffff; font-family:constantia,lucida bright,dejavu serif,georgia,serif;">The spectroscopy of molecular oxygen is associated with the atmospheric processes of aurora, airglow and nightglow. The absorption in the Herzberg continuum and Schumann&ndash;Runge bands in the ultraviolet produces atomic oxygen that is important in the chemistry of the middle atmosp. Excited state singlet molecular oxygen is responsible for red chemiluminescence in . Isotopes and stellar origin<br />
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			Main article: Isotopes of oxygen A concentric-sp diagram, shog, from the core to the outer shell, iron, silicon, oxygen, neon, carbon, helium and hydrogen layers. Late in a massive star&#39;s life, 16O concentrates in the O-shell, 17O in the H-shell and 18O in the He-shell.<br />
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			Naturally occurring oxygen is composed of three stable isotopes, 16O, 17O, and 18O, with 16O being the most abundant (99.762% natural abundance).<br />
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			Most 16O is synthesized at the end of the helium fusion process in massive stars but some is me in the neon burning process. 17O is primarily me by the burning of hydrogen into helium during the CNO cycle, making it a common isotope in the hydrogen burning zones of stars. Most 18O is produced when 14N (me abundant from CNO burning) captures a 4He nucleus, making 18O common in the helium-rich zones of evolved, massive stars. Fourteen rioisotopes have been characterized. The most stable are 15O with a half-life of 122.24 seconds and 14O with a half-life of 70.606 seconds. All of the remaining rioactive isotopes have half-lives that are less than 27 s and the majority of these have half-lives that are less than 83 milliseconds. The most common decay mode of the isotopes lighter than 16O is &szlig;+ decay to yield nitrogen, and the most common mode for the isotopes heavier than 18O is beta decay to yield fluorine.Oxygen is the most abundant chemical element by mass in the Earth&#39;s biosp, air, sea and land. Oxygen is the third most abundant chemical element in the universe, after<br />
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			hydrogen and helium. About 0.9% of the Sun&#39;s mass is oxygen. Oxygen constitutes 49.2% of the Earth&#39;s crust by mass as part of oxide compounds such as silicon dioxide and is the most abundant element by mass in the Earth&#39;s crust. It is also the major component of the world&#39;s oceans (88.8% by mass). Oxygen gas is the second most common component of the Earth&#39;s atmosp, taking up 20.8% of its volume and 23.1% of its mass (some 1015 tonnes). Earth is unusual among the planets of the Solar System in having such a high concentration of oxygen gas in its atmosp: Mars (with 0.1% O 2 by volume) and Venus have much less. The O 2 surrounding those planets is produced solely by the action ultraviolet riation on oxygen-containing molecules such as carbon dioxide.<br />
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			The unusually high concentration of oxygen gas on Earth is the result of the oxygen cycle. This biogeochemical cycle describes the movement of oxygen within and between its three main reservoirs on Earth: the atmosp, the biosp, and the lithosp. The main driving factor of the oxygen cycle is photosynthesis, which is responsible for modern Earth&#39;s atmosp. Photosynthesis releases oxygen into the atmosp, while respiration, decay, and combustion it from the atmosp. In the present equilibrium, production and consumption occur at the same rate. World map shog that the sea-surface oxygen is depleted around the equator and increases towards the poles. Cold water holds more dissolved O 2. </span></td>
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