Soil freeze-thaw with root litter alters N transformations during the dormant season in soils under two temperate forests in northern Japan

被引:33
|
作者
Hosokawa, Nanae [1 ]
Isobe, Kazuo [2 ]
Urakawa, Rieko [2 ,3 ]
Tateno, Ryunosuke [4 ]
Fukuzawa, Karibu [5 ]
Watanabe, Tsunehiro [4 ,5 ]
Shibata, Hideaki [5 ]
机构
[1] Hokkaido Univ, Grad Sch Environm Sci, Kita Ku, N10 W5, Sapporo, Hokkaido 0600810, Japan
[2] Univ Tokyo, Grad Sch Agr & Life Sci, Bunkyo Ku, 1-1-1 Yayoi, Tokyo 1138657, Japan
[3] Japan Environm Sanitat Ctr, Asia Ctr Air Pollut Res, Nishi Ku, 1182 Sowa, Niigata 9502144, Japan
[4] Kyoto Univ, Field Sci Educ & Res Ctr, Sakyo Ku, Oiwake Cho, Kyoto 6068502, Japan
[5] Hokkaido Univ, Field Sci Ctr Northern Biosphere, Kita Ku, N9 W9, Sapporo, Hokkaido 0600809, Japan
来源
SOIL BIOLOGY & BIOCHEMISTRY | 2017年 / 114卷
基金
日本学术振兴会;
关键词
Root litter; Snow removal manipulation; DOC; Nitrification; Vegetation; WINTER CLIMATE-CHANGE; MICROBIAL BIOMASS CALIBRATION; FUMIGATION-EXTRACTION METHOD; NET NITROGEN MINERALIZATION; DISSOLVED ORGANIC-MATTER; DIFFERENT VEGETATION; INORGANIC NITROGEN; DYNAMICS; NITRATE; LOSSES;
D O I
10.1016/j.soilbio.2017.07.025
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Extreme soil freeze thaw regimes caused by winter climate change can alter nitrogen (N) transformations through plant root mortality. In this study, we conducted a snow removal experiment to simulate extreme soil freeze thaw to understand the effect of soil freeze thaw on N transformations in soils under two northern temperate forests (oak and larch) in northern Japan. We also investigated the effect of root input on microbial biomass and transformations of dissolved organic carbon (DOC) and N by experimentally adding root litter to obtain mechanistic insight. Snow removal significantly reduced net nitrification and N mineralization, while it increased net ammonification in both soils. Root litter addition provided contrasting effects of vegetation type on net DOC change; it significantly decreased net DOC production in the oak soil, while it was increased in the larch soil. The contrasting responses of DOC change with vegetation were possibly related to specific microbial composition and physiology of the vegetation. Further, root addition eliminated the differences in net N mineralization and microbial biomass between the two vegetation types in the snow removal plots. Our results indicated that soil freeze thaw could reduce the differences in vegetation type on soil N dynamics through root litter input. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:270 / 278
页数:9
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