Arid
DOI10.1016/j.geoderma.2016.07.004
CaCO3 recrystallization in saline and alkaline soils
Zhao, Xiaoning1,4,5; Zhao, Chengyi2; Wang, Jinyang3; Stahr, Karl1; Kuzyakov, Yakov4,5,6
通讯作者Zhao, Xiaoning
来源期刊GEODERMA
ISSN0016-7061
EISSN1872-6259
出版年2016
卷号282页码:1-8
英文摘要

Are desert ecosystems a stable sink for atmospheric CO2? Although the uptake of atmospheric CO2 by soil during the nighttime is detected in deserts and some semi-deserts, the underlying mechanisms remain elusive. In order to determine the factors affecting the CO2 fluxes into soil and to reveal the relationship between CO2 fluxes and carbonate formation and recrystallization in saline and alkaline soils, four soils with contrasting salinity from two sites, Aksu and Yingbazar, along the Tarim River were analysed. Soils were incubated in (CO2)-C-14 labelled atmosphere for 90 days at three CO2 concentrations: 0.04%, 0.4% and 4%. The C-14 activity was measured in soil water and air, as well as in carbonates after 2,14 and 90 days. The C-14 incorporation in CaCO3 increased with corresponding C-14 decrease remaining in the CO2. The highest C-14 incorporation into CaCO3 (54%) was observed in the Yingbazar saline soil. The carbonate recrystallization rates increased logarithmically (r(2) > 0.97) with the CO2 concentration. The average carbonate recrystallization rate from three sampling times was highest in the Yingbazar saline soil under 4% CO2 (8.45 x 10-6 day(-1)) and lowest in the Aksu alkaline soil under 0.04% CO2 (0.03 x 10(-6) day(-1)). The average carbonate recrystallization rate increased with electric conductivity (corresponding to soil salinity) but decreased with pH (R-2 = 0.99 for 4% CO2). The alkaline soils incorporated less C-14 into CaCO3 than the saline soils. At the highest CO2 concentration of 4%, the full recrystallization period of the remaining primary carbonates was 10- to 100-fold shorter than at the lower CO2 concentrations. Therefore, besides soil chemical parameters (e.g. pH, CaCO3 content), CO2 concentration (respiration of microorganisms and roots) is an important factor for CaCO3 recrystallization and formation of pedogenic carbonates in desert soils. It is the most important factor for CaCO3 recrystallization and so, for the formation of pedogenic carbonates. (C) 2016 Elsevier B.V. All rights reserved.


英文关键词Carbonate recrystallization CO2 C-14 Saline and alkaline soil Pedogenic carbonate Tarim River Basin
类型Article
语种英语
国家Germany ; Peoples R China ; Russia
收录类别SCI-E
WOS记录号WOS:000381837100001
WOS关键词CARBON ; CO2 ; ROOT ; GEOCHEMISTRY ; RESPIRATION ; TEMPERATURE ; SENSITIVITY
WOS类目Soil Science
WOS研究方向Agriculture
来源机构中国科学院新疆生态与地理研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/193196
作者单位1.Univ Hohenheim, Inst Soil Sci & Land Evaluat, Emil Wolff Str 27, D-70593 Stuttgart, Germany;
2.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Key Lab Oasis Ecol & Desert Environm, Urumqi 830011, Peoples R China;
3.Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China;
4.Univ Gottingen, Dept Soil Sci Temperate Ecosyst, Busgenweg 2, D-37077 Gottingen, Germany;
5.Univ Gottingen, Dept Agr Soil Sci, Busgenweg 2, D-37077 Gottingen, Germany;
6.Kazan Fed Univ, Inst Environm Sci, Kazan, Russia
推荐引用方式
GB/T 7714
Zhao, Xiaoning,Zhao, Chengyi,Wang, Jinyang,et al. CaCO3 recrystallization in saline and alkaline soils[J]. 中国科学院新疆生态与地理研究所,2016,282:1-8.
APA Zhao, Xiaoning,Zhao, Chengyi,Wang, Jinyang,Stahr, Karl,&Kuzyakov, Yakov.(2016).CaCO3 recrystallization in saline and alkaline soils.GEODERMA,282,1-8.
MLA Zhao, Xiaoning,et al."CaCO3 recrystallization in saline and alkaline soils".GEODERMA 282(2016):1-8.
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