@article{oai:nipr.repo.nii.ac.jp:00002976,
 author = {Iizuka, Yoshinori and Fujita, Koji and Matoba, Sumito and Fujii, Yoshiyuki and Matsuki, Kenichiro and Kohno, Mika and Aizen, Vladimir B.},
 journal = {Polar meteorology and glaciology},
 month = {Nov},
 note = {P(論文), To better understand how the chemical composition of a glacier in an inland continental region relates to the local climate, we collected ice core samples from the Belukha Glacier, Russia, in July 2001. We analyzed the samples for pH, anions, and cations. The primary soluble ions were SO42-, NO3-, NH4+, Ca2+, and HCOO-. Moreover, we argue the following. 1) Ca2+ and its equivalent SO42-+ NO3- likely originated from terrestrial dust such as soil. 2) HCOO- and its equivalent NH4+ likely originated from vegetation and/or biomass burning. 3) The remaining SO42-+NO3- and NH4+ likely originated from livestock, commercial fertilizers, and natural fertilizers. 4) The NH4+ concentration was low when there was no contribution from vegetation and/or biomass burning.},
 pages = {114--120},
 title = {Chemical characteristics in a 22-m ice core on the Belukha Glacier, Russia},
 volume = {18},
 year = {2004}
}