Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Origin of Photosynthesis01:26

Origin of Photosynthesis

Photosynthesis represents a fundamental biological process that transformed Earth's atmosphere and paved the way for complex life. Emerging roughly 3.4–3.8 billion years ago, the earliest photosynthetic organisms harnessed light energy to produce organic compounds. These anoxygenic phototrophs used electron donors like hydrogen sulfide (H₂S) or ferrous iron (Fe²⁺), rather than water, and did not release molecular oxygen (O₂) as a byproduct. Various groups, including green sulfur and purple...
Sulfur Assimilation01:20

Sulfur Assimilation

Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to become...
Flame Photometry: Lab01:16

Flame Photometry: Lab

In a flame photometer, when a solution like potassium chloride is aspirated into the flame, the solvent evaporates, leaving behind dehydrated salt. This salt dissociates into free gaseous atoms in their ground state. Some of these atoms absorb energy from the flame, leading to their excitation. The excited atoms return to the ground state, emitting photons at characteristic wavelengths. Because only electronic transitions are involved, the resulting emission lines are very narrow. The intensity...
Classifying Matter by Composition03:35

Classifying Matter by Composition

Matter: Pure Substances and Mixtures
According to its composition, the matter can be classified into two broad categories — pure substances and mixtures. 
A pure substance is a form of matter that has a constant composition throughout with uniform properties. For example, any sample of sucrose has the same composition and same physical properties, such as melting point, color, and sweetness, regardless of the source from which it is isolated. 
A mixture is composed of two or more types of...
Atomic Emission Spectroscopy: Lab01:29

Atomic Emission Spectroscopy: Lab

AES is a powerful analytical technique, especially effective when used with plasma sources, producing abundant spectra in characteristic emission lines. The Inductively Coupled Plasma (ICP), in particular, yields superior quantitative analytical data due to its high stability, low noise, low background, and minimal interferences under optimal experimental conditions. However, newer air-operated microwave sources are emerging as promising alternatives that could be more cost-effective than...
Emission Spectra02:39

Emission Spectra

When solids, liquids, or condensed gases are heated sufficiently, they radiate some of the excess energy as light. Photons produced in this manner have a range of energies, and thereby produce a continuous spectrum in which an unbroken series of wavelengths is present.

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Electron Microprobe/SIMS Determinations of Al in Olivine: Applications to Solar Wind, Pallasites and Trace Element Measurements.

Geostandards and geoanalytical research·2021
Same author

Magnesium isotopes of the bulk solar wind from Genesis diamond-like carbon films.

Meteoritics & planetary science·2020
Same author

The future of Genesis science.

Meteoritics & planetary science·2019
Same author

DETERMINING THE ELEMENTAL AND ISOTOPIC COMPOSITION OF THE PRESOLAR NEBULA FROM GENESIS DATA ANALYSIS: THE CASE OF OXYGEN.

The astrophysical journal. Letters·2018
Same author

Quantitative Phase Analysis by X-Ray Diffraction.

Analytical chemistry·2017
Same author

The oxygen isotopic composition of the Sun inferred from captured solar wind.

Science (New York, N.Y.)·2011

Related Experiment Video

Updated: Jun 2, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Solar composition from the Genesis Discovery Mission.

D S Burnett1, Genesis Science Team

  • 1Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. burnett@gps.caltech.edu

Proceedings of the National Academy of Sciences of the United States of America
|May 11, 2011
PubMed
Summary

The Genesis Mission returned solar samples, revealing unique oxygen, nitrogen, and noble gas isotopic compositions. These findings, analyzed with advanced instruments, offer crucial insights into solar system origins and planetary comparisons.

More Related Videos

Using Neutron Spin Echo Resolved Grazing Incidence Scattering to Investigate Organic Solar Cell Materials
06:05

Using Neutron Spin Echo Resolved Grazing Incidence Scattering to Investigate Organic Solar Cell Materials

Published on: January 15, 2014

Making Record-efficiency SnS Solar Cells by Thermal Evaporation and Atomic Layer Deposition
14:01

Making Record-efficiency SnS Solar Cells by Thermal Evaporation and Atomic Layer Deposition

Published on: May 22, 2015

Related Experiment Videos

Last Updated: Jun 2, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Using Neutron Spin Echo Resolved Grazing Incidence Scattering to Investigate Organic Solar Cell Materials
06:05

Using Neutron Spin Echo Resolved Grazing Incidence Scattering to Investigate Organic Solar Cell Materials

Published on: January 15, 2014

Making Record-efficiency SnS Solar Cells by Thermal Evaporation and Atomic Layer Deposition
14:01

Making Record-efficiency SnS Solar Cells by Thermal Evaporation and Atomic Layer Deposition

Published on: May 22, 2015

Area of Science:

  • Planetary Science
  • Cosmochemistry
  • Astrobiology

Background:

  • Understanding the Sun's isotopic composition is key to deciphering solar system formation and evolution.
  • Previous solar wind data from lunar samples had discrepancies, particularly for noble gases.
  • Sample return missions offer unparalleled opportunities for in-situ laboratory analysis of extraterrestrial materials.

Purpose of the Study:

  • To leverage the Genesis Mission's returned solar samples for precise isotopic analysis.
  • To resolve discrepancies in noble gas measurements from previous solar wind studies.
  • To compare solar isotopic compositions with other solar system bodies and planetary atmospheres.

Main Methods:

  • Analysis of returned solar wind samples using advanced terrestrial laboratory instrumentation.
  • Application of specialized analytical instruments developed for the Genesis Mission.
  • Replication of key isotopic measurements (Nitrogen) across multiple independent instruments.

Main Results:

  • Determined distinct isotopic compositions for Oxygen, Nitrogen, and noble gases in the Sun compared to inner solar system objects.
  • Established that the Sun's Nitrogen isotopic composition matches that of Jupiter.
  • Resolved prior discrepancies in noble gas data obtained from solar wind implanted in lunar soils.

Conclusions:

  • Genesis Mission sample return significantly advanced our understanding of solar system isotopic heterogeneity.
  • The mission demonstrated the critical value of terrestrial laboratory analysis for unobtainable scientific results.
  • Nitrogen isotope findings provide a crucial link between solar composition and gas giant atmospheres.