The solar flare proton fluxes, averaged over different periods of time, have been determined from Al-26 measured in five selected lunar rocks. The time of exposure of these rocks, ranging from 0.5 to 3.8 million years, were deduced from track profiles due to galactic-cosmic-ray heavy nuclei and from rare-gas data. The observed production rates of Al-26 in all the rocks is in close agreement, implying little variation in average solar flare proton intensity during the past 0.5-, 1-, and 1.5-million-year periods. If the fluxes of solar flare protons and thermal radiation are related, these data exclude any significant changes in solar luminosity during the Pleistocene
We determined concentration profiles of Ne-21, Ne-22, and Ar-38 produced by solar protons as a funct...
A nondestructive beta-gamma coincidence technique was used to measure the radioactivity of lunar roc...
The event-integrated fluences of energetic solar protons up to 2004 at the Earth have been determine...
Solar proton fluxes have been deduced from Al-26 depth profile resulting mainly from their interacti...
Abstract. A statistical analysis of the contemporary (1954–1975) solar flare particle events has bee...
Aims. Lunar soil and rocks are not protected by a magnetic field or an atmosphere and are continuous...
Abstract Direct measurements of solar energetic particles (SEP) cover the space era of several deca...
The long term variations of the intensity of solar cosmic rays, galactic cosmic rays, and the solar ...
Abstract Aims: Lunar soil and rocks are not protected by a magnetic field or an atmosphere and are c...
Recent results on cosmic ray interactions in lunar samples and meteorites resulting in productio...
Methods were developed earlier to deduce the composition of solar flare neon and to determine the so...
Cosmic rays penetrate the lunar surface and interact with the lunar rocks to produce both radionucli...
Several sets of measurements of the fluxes of solar energetic particles (SEPs) above 10 MeV have bee...
Modern solar energetic particles (SEPs) have been studied for about 50 years by satellites and groun...
In this study we compare the mean annual sunspot numbers for the six most recent solar cycles (19 to...
We determined concentration profiles of Ne-21, Ne-22, and Ar-38 produced by solar protons as a funct...
A nondestructive beta-gamma coincidence technique was used to measure the radioactivity of lunar roc...
The event-integrated fluences of energetic solar protons up to 2004 at the Earth have been determine...
Solar proton fluxes have been deduced from Al-26 depth profile resulting mainly from their interacti...
Abstract. A statistical analysis of the contemporary (1954–1975) solar flare particle events has bee...
Aims. Lunar soil and rocks are not protected by a magnetic field or an atmosphere and are continuous...
Abstract Direct measurements of solar energetic particles (SEP) cover the space era of several deca...
The long term variations of the intensity of solar cosmic rays, galactic cosmic rays, and the solar ...
Abstract Aims: Lunar soil and rocks are not protected by a magnetic field or an atmosphere and are c...
Recent results on cosmic ray interactions in lunar samples and meteorites resulting in productio...
Methods were developed earlier to deduce the composition of solar flare neon and to determine the so...
Cosmic rays penetrate the lunar surface and interact with the lunar rocks to produce both radionucli...
Several sets of measurements of the fluxes of solar energetic particles (SEPs) above 10 MeV have bee...
Modern solar energetic particles (SEPs) have been studied for about 50 years by satellites and groun...
In this study we compare the mean annual sunspot numbers for the six most recent solar cycles (19 to...
We determined concentration profiles of Ne-21, Ne-22, and Ar-38 produced by solar protons as a funct...
A nondestructive beta-gamma coincidence technique was used to measure the radioactivity of lunar roc...
The event-integrated fluences of energetic solar protons up to 2004 at the Earth have been determine...