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GYIG OpenIR  > 环境地球化学国家重点实验室
间歇性内陆水域是重要的碳源
陈波; 赵敏
2020
Source Publication科学通报
Volume65Issue:16Pages:1581-1591
DOI10.1360/TB-2019-0868
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Indexed BySCI
Language中文
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Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11733
Collection环境地球化学国家重点实验室
Affiliation1.贵州财经大学公共管理学院, 贵阳 550025
2.中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳 550081
Recommended Citation
GB/T 7714
陈波,赵敏. 间歇性内陆水域是重要的碳源[J]. 科学通报,2020,65(16):1581-1591.
APA 陈波,&赵敏.(2020).间歇性内陆水域是重要的碳源.科学通报,65(16),1581-1591.
MLA 陈波,et al."间歇性内陆水域是重要的碳源".科学通报 65.16(2020):1581-1591.
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