生态与农村环境学报 ›› 2021, Vol. 37 ›› Issue (5): 611-618.doi: 10.19741/j.issn.1673-4831.2020.0794

• 自然保护与生态 • 上一篇    下一篇

增温和生物炭添加对麦田土壤养分和微生物生物量的影响

郭万庆, 徐小逊, 鲁兰, 扈茹静, 杨占彪   

  1. 四川农业大学环境学院, 四川 成都 611130
  • 收稿日期:2020-09-22 出版日期:2021-05-25 发布日期:2021-05-21
  • 通讯作者: 杨占彪 E-mail:yzb126.com
  • 作者简介:郭万庆(1997-),女,四川乐山人,主要研究方向为土壤生态修复。E-mail:814486036@qq.com
  • 基金资助:
    四川省重点研发项目(2020YFN0058)

Effects of Warming and Biochar Addition on Soil Nutrients and Microbial Biomass in Wheat Fields

GUO Wan-qing, XU Xiao-xun, LU Lan, HU Ru-jing, YANG Zhan-biao   

  1. College of Environment, Sichuan Agricultural University, Chengdu 611130, China
  • Received:2020-09-22 Online:2021-05-25 Published:2021-05-21

摘要: 研究全球变暖和生物炭添加对农田土壤养分和土壤微生物生物量的影响,可为生物炭在农业生产中的应用提供理论参考。采用开顶式(open-top chamber, OTC)模拟增温方法,设置CK(未增温)、T1、T2和T3不同温度梯度处理,分别添加竹质生物炭20 t·hm-2(BC1)和不添加(BC0)处理。结果表明,OTC法使T1、T2和T3处理平均气温较CK分别增加0.5、1.0和1.6 ℃。不加生物炭单独增温条件下,与CK相比,土壤有机质(SOM)、全氮(TN)、全钾(TK)、碱解氮(AN)、速效磷(AP)和速效钾(AK)含量均极显著增加,T1、T2和T3处理微生物生物量碳(MBC)含量分别增加70%、72.4%和114.39%,微生物生物量氮(MBN)含量分别增加45.02%、71.71%和72.23%,微生物生物量磷(MBP)含量分别增加39.43%、73.71%和202.31%,均达到极显著水平(P<0.01)。未增温单独添加生物炭条件下,与未添加生物炭相比,土壤SOM、TN、TK和AK含量极显著增加,全磷(TP)含量显著增加,MBC、MBN和MBP含量均呈显著增加趋势(P<0.05)。与未增温未添加生物炭相比,增温与生物炭共同作用处理土壤MBC、MBN和MBP含量均增加,最大增加量分别达到154.34%、87.85%和197.60%。增温和生物炭共同作用可极显著增加土壤pH以及TN、AN和AP含量,可显著增加土壤SOM含量,同时也可极显著增加MBN/TN比值。相关分析和冗余分析表明,土壤性质对微生物生物量变化的影响由高到低为SOM>AP>AK>AN>TK>PH>TP>TN,其中土壤养分中SOM、AP和AK含量是影响土壤微生物生物量的主要因素。在全球变暖背景下,添加生物炭通过加速土壤元素循环过程而增加土壤微生物生物量。

关键词: 增温, 生物炭, 微生物生物量, 土壤养分

Abstract: The effects of global warming and biochar addition on farmland soil nutrients and microbial biomass were studied to provide a theoretical reference for the application of biochar in agricultural production. An open-top chamber (OTC) was used to simulate warming. Different temperature gradients-CK (no warming ), T1, T2 and T3-were set, with the addtion of bamboo biochar at 20 t·hm-2 (BC1) and no addition (BC0). The results show that compared with the average temperature of CK the OTC average temperature of T1, T2 and T3 increased by 0.5, 1.0 and 1.6 ℃, respectively, As temperature rose alone (without the addition of bamboo biochar), soil organic matter (SOM), total nitrogen (TN), total potassium (TK), alkaline hydrolysis nitrogen (AN), available phosphorus (AP), rapidly available potassium (AK) increased at extremely significant level. The microbial biomass carbon (MBC) of T1, T2 and T3 increased by 70%, 72.4% and 114.39%, respectively, compared with CK. As temperature rose alone, the microbial biomass nitrogen (MBN) of T1, T2 and T3 increased by 45.02%, 71.71% and 72.23%, respectively, compared with CK. Compared with the microbial biomass P (MBP) of CK, as temperatures rose alone, the microbial biomass P of T1, T2 and T3 increased by 39.43%, 73.71% and 202.31%, respectively All the above increases were at extremely significant level (P<0.01). When biochar was added alone (without increasing of temperature), SOM, TN, TK, and AK reached extremely significant level, and the total phosphorus (TP ) reaching to significant level. MBC, MBN and MBP all showed an increasing trend at significant level (P<0.05). When warming and biochar addition were combined, the contents of soil MBC, MBN and MBP increased by 154.34%, 87.85% and 197.60%, respectively, compared with treatment without warming and biochar addition. The combined action of warming and biochar can increase the soil pH, TN, AN, AP and the MBN/TN ratio at extremely significant level, and the increase of SOM at significant level. Correlation analysis and redundancy analysis show that the effect of soil properties on changes of microbial biomass was in the order of SOM>AP>AK>AN>TK>PH>TP>TN. SOM, AP and AK are the main factors affecting soil microbial biomass. Under the stress of global warming, adding biochar can increase soil microbial biomass by accelerating the cycling of soil elements.

Key words: warming, biochar, soil microbial biomass, soil nutrient

中图分类号: