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Scientists are making significant strides toward potentially adding a new element to the periodic table. Currently, the table includes 118 elements, each with a distinct number of protons in its nucleus. For example, hydrogen has one proton, while oganesson has 118. The quest to explore the limits of atomic physics has led researchers to focus on creating element 120. If successful, this new element could be the next addition to the periodic table, marking a significant milestone in our understanding of chemistry and physics.

Exploring the Path to Element 120

The strategy to produce element 120 involves using titanium ions in a particle accelerator. Researchers aim to collide these ions with californium atoms, which have 98 protons. Since titanium has 22 protons and californium has 98, their collision should theoretically result in element 120, which would have a total of 120 protons. This approach is innovative, as titanium beams have not previously been used to create such heavy elements. The success of this method hinges on the ability to manage and direct these high-energy particles precisely.

Testing the Feasibility

In a recent experiment, scientists directed titanium ions at plutonium, which has 94 protons, with the goal of creating livermorium, an element with 116 protons. Over a span of 22 days, the team successfully detected two livermorium atoms in the aftermath of their particle collisions. This result suggests that titanium beams might indeed be a viable tool for creating new heavy elements. However, scientists anticipate that producing element 120 will be significantly more challenging and time-consuming, possibly requiring up to ten times longer than the livermorium experiment.

The Challenge of Creating New Elements

Historically, creating elements beyond the current 118 has involved using calcium-48 beams. Calcium-48, an isotope of calcium with 28 neutrons, has been employed in various experiments to push the boundaries of the periodic table. However, this method has its limitations, particularly with the use of radioactive target materials that decay too quickly for thorough analysis. By switching to titanium-50 beams, researchers aim to use more practical target materials, potentially overcoming the constraints imposed by faster-decaying elements.

Looking Ahead

The process of creating a new element is complex and requires meticulous experimentation. The shift to using titanium ions represents a promising new approach to discovering elements beyond those currently known. As research continues, scientists are hopeful that element 120 will soon join the periodic table, offering new insights into atomic physics and expanding our knowledge of the fundamental building blocks of matter. This advancement would not only enhance our understanding of chemistry but also push the boundaries of what is possible in scientific research.

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NASA’s TRACERS Satellites Begin Solar Wind Study Despite SV1 Glitch

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NASA's TRACERS Satellites Begin Solar Wind Study Despite SV1 Glitch

NASA’s TRACERS mission twin satellites were launched on July 23, 2025, to study how solar activity causes magnetic reconnection in Earth’s atmosphere. After launch, a power subsystem anomaly had affected one of the satellites (Space Vehicle 1, SV1) on July 25, causing periodic communication loss. NASA said satellite 2 (Space Vehicle 2, SV2) is “healthy,” and transition is beginning to the instrument commissioning phase. The idea behind TRACERS was to develop a complete toolkit that would allow us, for the first time, to observe all of these complex solar wind connection processes at once. NASA engineers are actively working to recover SV1. Single vector views (SV2) spacecraft are completing a healthy checkout and readying themselves for their science mission.

Recovery Efforts for SV1 Satellite

According to NASA, controllers detected a problem with SV1’s power subsystem in late July that led to intermittent contacts and a loss of communication. Data suggest SV1 can only remain active when its solar panels receive sufficient sunlight. Because of the spacecraft’s current orientation, engineers plan to wait until later in August — when SV1’s panels will receive more sun — to reestablish contact and continue recovery steps.

Meanwhile, mission teams are reviewing onboard data to diagnose the issue and plan next steps. Any time contact is regained, the team will assess SV1’s status and check for impacts on the mission’s science goals. For now, no significant updates on SV1 are expected for several weeks.

SV2 Operational Status

The mission’s other satellite, SV2, is in good health and fully operational. Mission teams have been testing SV2’s onboard instruments and systems through a standard commissioning process. This checkout is proceeding as expected, with NASA anticipating that commissioning will finish by the end of August.

Once SV2 is fully checked out, it will begin coordinated science operations with its twin to study magnetic reconnection – the process that shapes how solar activity affects Earth’s magnetic environment. For now, SV2 continues its planned tests and will soon be ready to collect valuable science data as part of the TRACERS mission.

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Scientists Explore Role of Space Radiation in Powering Alien Microbial Life

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Scientists Explore Role of Space Radiation in Powering Alien Microbial Life

The search for alien life traditionally focuses on planets in the “Goldilocks zone” — the orbital band where surface water can exist. But new research suggests life might thrive far from starlight in a so-called “radiolytic habitable zone,” where penetrating cosmic rays break buried water molecules (a process called radiolysis) into hydrogen, oxygen and energy-rich electrons. Simulations of icy worlds like Mars, Europa and Saturn’s moon Enceladus show cosmic rays can reach subsurface water. Researchers suggest these electrons could fuel microbes in hidden reservoirs, effectively creating underground oases of life.

Radiation as a Power Source

According to the new study, cosmic rays are fast-moving particles (electrons, protons or nuclei) blasted out by supernovas and distant stars. On Earth, most are stopped by our magnetic field and thick atmosphere. But Mars and the icy moons (which lack such shields) get hit directly; their thin air or vacuum allows rays to penetrate deep into ice and rock. When these particles strike water or ice, they trigger radiolysis – shattering molecules and freeing hydrogen, oxygen and electrons. Some Earth microbes already exploit this: for example, a bacterium 2.8 km underground in a gold mine lives entirely on hydrogen produced by radioactive decay.

Expanding the Search for Life

Dubbed the “Radiolytic Habitable Zone,” this hidden-energy band lies beneath ice or rock where cosmic rays can sustain life. Simulations show Saturn’s icy moon Enceladus has the highest radiolytic potential, followed by Mars and then Jupiter’s moon Europa. NASA’s upcoming Europa Clipper mission and telescopes like ALMA will probe these frozen worlds for chemical signs of life. Even more intriguingly, cosmic-ray impacts can directly create complex organic molecules (for example, amino-acid precursors) in ice. Because cosmic rays pervade the galaxy, even a rogue planet adrift in space would be bathed in intense radiation.

As Dimitra Atri, an astrophysicist and co-author of the new study puts it, “life might be able to survive in more places than we ever imagined”, suggesting hidden biospheres could exist in many cold, dark niches.

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Massive Russia Earthquake Triggers Rare ‘Parade’ of 7 Kamchatka Volcanoes

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Massive Russia Earthquake Triggers Rare 'Parade' of 7 Kamchatka Volcanoes

In late July 2025, a magnitude 8.8 earthquake struck off Russia’s Kamchatka Peninsula, triggering a rare series of volcanic eruptions. Scientists report that within days six or seven of the region’s volcanoes erupted in succession—an occurrence not seen in nearly 300 years. Experts described the event as an “extremely rare phenomenon” or “parade of volcanic eruptions”. These volcanoes lie along the Pacific “Ring of Fire,” a zone known for frequent seismic and volcanic activity. The area is sparsely populated, so the immediate risk to local communities is low, although ash plumes could disrupt air travel. Experts are monitoring the situation.

Confirmed Eruptions in Kamchatka

According to the Far Eastern Branch of the Russian Academy of Sciences’ Institute of Volcanology and Seismology, the 8.8-magnitude quake set off eruptions in seven Kamchatka volcanoes. The agency noted this was the first time in nearly 300 years that so many had erupted simultaneously, and its director Alexey Ozerov called it a rare “parade of volcanic eruptions”.

Active vents include major peaks such as Russia’s Klyuchevskaya Sopka, Shiveluch, Bezymianny, Karymsky and Avachinsky. Notably, Krasheninnikov — dormant for about 500 years — erupted after the quake, and heat anomalies at Mutnovsky hint at a possible seventh eruption. The Kamchatka Volcanic Eruption Response Team also reported ash plumes from Klyuchevskoy Volcano. The peninsula hosts about 29 active volcanoes.

Scientific Perspective on Cause

Geophysicist Paul Segall noted that large subduction-zone quakes can trigger eruptions – for example, the 1960 Chile quake was followed by multiple volcanoes erupting. He said such quakes alter crustal stresses, making magma easier to reach the surface. Segall cautioned that it is “still too soon to characterize” the recent events. Kamchatka is normally very active: 40–50 volcanoes erupt worldwide at any time, and Kamchatka has 29 active volcanoes. Klyuchevskoy had been restless before the quake, and the event likely “increased the vigor” of its eruption.

Harold Tobin told Live Science in an email that even the first Krasheninnikov eruption in centuries may be “a very strong coincidence” or triggered by the quake’s seismic waves.

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