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Sources of Hydrogen Sulfide
"On the Location of Hydrogen Sulfide"
Hydrogen sulfide is a kind of gas. Its source is not the same, and there are various kinds of gas.
Between springs, or containing this gas. In the spring veins in the ground, there are those that gush from the depths, and their water may contain hydrogen sulfide. The structure of the cover underground is complicated, and sulfur and hydrogen elements undergo various chemical reactions to form hydrogen sulfide, which comes out with the spring.
Inside the mine, it is also its source. Sulfur-containing substances in the mine, in a specific environment, are subject to temperature, pressure and various chemical reactions, and sulfur and hydrogen combine to produce hydrogen sulfide. The mine tunnel is deep, and the air circulation is not smooth, so this gas is easy to gather.
In the swamp, hydrogen sulfide is often produced. When the organic matter in the swamp decays, anaerobic microorganisms act on it to decompose the sulfur-containing substances and cause hydrogen sulfide to form. The mud and water in the swamp blend, and this gas escapes in the middle.
On the side of the volcano, traces of hydrogen sulfide can also be seen. During volcanic activity, underground magma spews out with sulfur and other elements, and the sulfur reacts with surrounding materials to form hydrogen sulfide under certain conditions, which is dispersed around with the gas from volcanic eruptions.
In summary, the hydrogen sulfide contained in springs, caverns, swamps, and volcanic sides is also there, and its sources have their own reasons, which should be carefully investigated.
Hydrogen sulfide is a kind of gas. Its source is not the same, and there are various kinds of gas.
Between springs, or containing this gas. In the spring veins in the ground, there are those that gush from the depths, and their water may contain hydrogen sulfide. The structure of the cover underground is complicated, and sulfur and hydrogen elements undergo various chemical reactions to form hydrogen sulfide, which comes out with the spring.
Inside the mine, it is also its source. Sulfur-containing substances in the mine, in a specific environment, are subject to temperature, pressure and various chemical reactions, and sulfur and hydrogen combine to produce hydrogen sulfide. The mine tunnel is deep, and the air circulation is not smooth, so this gas is easy to gather.
In the swamp, hydrogen sulfide is often produced. When the organic matter in the swamp decays, anaerobic microorganisms act on it to decompose the sulfur-containing substances and cause hydrogen sulfide to form. The mud and water in the swamp blend, and this gas escapes in the middle.
On the side of the volcano, traces of hydrogen sulfide can also be seen. During volcanic activity, underground magma spews out with sulfur and other elements, and the sulfur reacts with surrounding materials to form hydrogen sulfide under certain conditions, which is dispersed around with the gas from volcanic eruptions.
In summary, the hydrogen sulfide contained in springs, caverns, swamps, and volcanic sides is also there, and its sources have their own reasons, which should be carefully investigated.
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