中国农业气象 ›› 2023, Vol. 44 ›› Issue (08): 675-684.doi: 10.3969/j.issn.1000-6362.2023.08.003

• 农业生态环境栏目 • 上一篇    下一篇

温度升高和CO2浓度增加对冬小麦田土壤氮磷含量的影响

苑嘉承,陈粲,虞凯浩   

  1. 1.南京信息工程大学滨江学院,无锡 214105;2.南京信息工程大学应用气象学院,南京 210044;3. 南京农业大学资源与环境科学学院,南京 210095
  • 收稿日期:2022-09-09 出版日期:2023-08-20 发布日期:2023-08-14
  • 通讯作者: 陈粲,讲师,博士,主要从事气候变化与土壤环境研究。 E-mail:chencan2010203@sohu.com
  • 作者简介:苑嘉承,E-mail:yuanjiacheng2020 @sina.com
  • 基金资助:
    国家自然科学基金项目(42107478)

Impact of Increasing Atmospheric Temperature and CO2 Concentration on Soil Nitrogen and Phosphorus Content in Winter Wheat Field

YUAN Jia-cheng, CHEN Can, YU Kai-hao   

  1. 1.Binjiang College, Nanjing University of Information Science and Technology, Wuxi 214105, China;2.College of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044;3. College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095
  • Received:2022-09-09 Online:2023-08-20 Published:2023-08-14

摘要: 采用T-FACE(Temperature-free air carbon dioxide enrichment)试验平台,设置田间常规温度和CO2浓度(CK)、田间常规温度和增加CO2浓度至575μmol·L−1(C)、升高温度(高于大气温度2℃)和田间常规CO2浓度(T)以及升高温度(高于大气温度2℃)和增加CO2浓度至575μmol·L−1(CT)共4个处理,对田间冬小麦进行控制实验。在小麦播种期、越冬期、分蘖期和成熟期分别采集不同层次的土壤样品(耕作层0−14cm、犁底层14−33cm、潴育层33−59cm和潜育层59−80cm),分析大气CO2浓度增加和温度升高后农田土壤N、P含量及其有效性的动态变化,以揭示气候变化对农田土壤中养分含量的时空影响。结果表明:(1)冬小麦在越冬期CO2浓度增加的情况下,常规或升高温度可使潴育层土壤中硝态氮含量出现下降趋势,在越冬期除T处理外,CK、C和CT处理的硝态氮含量在播种期低于耕作层。在越冬期的各处理中,硝态氮含量以CK处理增加最为明显。(2)在增加CO2浓度和升高温度的情况下,耕作层土壤中铵态氮含量在越冬期和分蘖期显著低于田间正常的CO2浓度和温度处理,且在不同土壤层次中未表现出明显的上升或下降的现象;铵态氮含量在小麦整个生长期相对稳定,但CT、C和T三种不同处理条件下,小麦成熟期铵态氮含量明显增加,且温度升高处理下的增加趋势显著(P<0.05);在小麦整个生育期内,C处理下铵态氮表现出先上升后下降的趋势,而CK、CT和T处理则表现出上升—下降—上升的趋势。(3)小麦全生育期内CK处理的速效磷含量明显高于其它处理,且在播种期、越冬期和分蘖期,CK处理与CT和T处理速效磷含量差异显著(P<0.05)。未来气候变化引起的CO2浓度增加和温度升高情况下,应合理施用N、P肥,减少不必要的养分流失。

关键词: 气候变化, 温度升高, CO2浓度升高, 冬小麦生育期, 土壤N、P含量

Abstract: T-FACE (temperature-free air carbon dioxide enrichment)experimental platform was adopted. Four field treatments of winter wheat were set: field conventional temperature and CO2 concentration (CK), field conventional temperature and increase CO2 concentration to 575μmol·L−1 (C), field increase temperature (i.e., 2℃ above atmospheric temperature) and field conventional CO2 concentration (T), and field increase temperature (i.e., 2℃ above atmospheric temperature) and increase CO2 concentration to 575μmol·L−1 (CT) . Soil samples were collected at different soil layers (plough layer 0−14cm, plough bottom 14−33cm, pond layer 33−59cm and glebe layer 59−80cm) at sowing stage, overwintering stage, tillering stage and maturity stage of winter wheat, respectively, to analyze the effects of increasing atmospheric CO2 concentration and temperature on N and P content and availability in the soil. The results were as follows: (1)under the condition that CO2 concentration increased in the overwintering stage of winter wheat, the nitrate nitrogen content in pond layer of soil showed a tendency to decrease by increasing temperature. In the overwintering stage of winter wheat, except for T treatment, the nitrate nitrogen content of CK, C and CT treatment was lower than that of tilling layer during sowing stage. In the overwintering stage of winter wheat, the nitrate nitrogen content increased most obviously in CK treatment. (2) Under the condition of increasing CO2 concentration and temperature, the content of ammonium nitrogen in the soil at tillering stage and overwintering stage of winter wheat was significantly lower than that under normal CO2 concentration and temperature treatment. There was no obvious upward or downward trend in different soil layers. The content of ammonium nitrogen was relatively stable during the whole growing stage of winter wheat. However, under CT, C and T treatments, the content of ammonium nitrogen increased significantly at maturity stage of winter wheat, and the increasing trend of nitrate nitrogen was more significant under increasing temperature (P<0.05). During the whole growth stage of winter wheat, the ammonium nitrogen showed a trend of increasing first and then decreasing under C treatment, while CK, CT and T treatments showed a trend of increasing, decreasing and increasing. (3) The content of available P in CK treatment was significantly higher than other treatments in the whole growth stage of winter wheat. There was a significant difference in available P content between CK treatment and CT and T treatments at sowing stage, overwintering stage and tillering stage of winter wheat (P<0.05). The results can provide some scientific basis for rational application of N and P fertilizer, reducing unnecessary nutrient loss and preventing non-point source pollution under the condition of CO2 concentration and temperature increase caused by climate change in the future.

Key words: Climate change, Increase temperature, Increase CO2 concentration, Winter wheat growth period, N and P contents in the soil