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田间试验增温对传统耕作和免耕系统下小麦根系分布的影响。

Effects of field experimental warming on wheat root distribution under conventional tillage and no-tillage systems.

作者信息

Hou Ruixing, Ouyang Zhu, Han Daorui, Wilson Glenn V

机构信息

Key Laboratory of Ecosystem Network Observation and Modeling Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China.

Yucheng Comprehensive Experiment Station China Academy of Science Beijing China.

出版信息

Ecol Evol. 2018 Jan 29;8(5):2418-2427. doi: 10.1002/ece3.3864. eCollection 2018 Mar.

Abstract

Despite the obvious importance of roots to agro-ecosystem functioning, few studies have attempted to examine the effects of warming on root biomass and distribution, especially under different tillage systems. In this study, we performed a field warming experiment using infrared heaters on winter wheat, in long-term conventional tillage and no-tillage plots, to determine the responses of root biomass and distribution to warming. Soil monoliths were collected from three soil depths (0-10, 10-20, and 20-30 cm). Results showed that root biomass was noticeably increased under both till and no-till tillage systems (12.1% and 12.9% in 2011, and 9.9% and 14.5% in 2013, in the two tillage systems, respectively) in the 0-30 cm depth, associated with a similar increase in shoot biomass. However, warming-induced root biomass increases occurred in the deeper soil layers (i.e., 10-20 and 20-30 cm) in till, while the increase in no-till was focused in the surface layer (0-10 cm). Differences in the warming-induced increases in root biomass between till and no-till were positively correlated with the differences in soil total nitrogen ( = .863, <.001) and soil bulk density ( = .853, <.001). Knowledge of the distribution of wheat root in response to warming should help manage nutrient application and cycling of soil C-N pools under anticipated climate change conditions.

摘要

尽管根系对农业生态系统功能的重要性显而易见,但很少有研究试图考察升温对根系生物量和分布的影响,尤其是在不同耕作系统下。在本研究中,我们在长期传统耕作和免耕地块上,使用红外加热器对冬小麦进行了田间升温实验,以确定根系生物量和分布对升温的响应。从三个土壤深度(0 - 10厘米、10 - 20厘米和20 - 30厘米)采集土壤整段标本。结果表明,在0 - 30厘米深度,传统耕作和免耕系统下根系生物量均显著增加(2011年,两种耕作系统分别增加12.1%和12.9%;2013年,分别增加9.9%和14.5%),地上生物量也有类似增加。然而,传统耕作中升温导致的根系生物量增加出现在较深土层(即10 - 20厘米和20 - 30厘米),而免耕中的增加集中在表层(0 - 10厘米)。传统耕作和免耕中升温导致的根系生物量增加差异与土壤全氮差异(r = 0.863,P < 0.001)和土壤容重差异(r = 0.853,P < 0.001)呈正相关。了解小麦根系对升温的分布响应,应有助于在预期的气候变化条件下管理养分施用和土壤碳氮库的循环。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6205/5838074/7cf1d3eda1c1/ECE3-8-2418-g001.jpg

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