中国农业气象 ›› 2024, Vol. 45 ›› Issue (03): 293-307.doi: 10.3969/j.issn.1000-6362.2024.03.007

• 农业生物气象栏目 • 上一篇    下一篇

增温背景下不同土壤对冬小麦产量品质影响评价

金丽惠,杨海超,王校益,苗淑杰,乔云发   

  1. 南京信息工程大学生态与应用气象学院,南京 210044
  • 收稿日期:2023-05-11 出版日期:2024-03-20 发布日期:2024-03-13
  • 作者简介:金丽惠,E-mail:jinlihui554@163.com
  • 基金资助:
    2022年度江苏省碳达峰碳中和科技创新专项资金(BE2022312;BE2022425);农业农村领域重大关键技术攻关(BE2022425);国家自然科学基金重点项目(42130506)

Evaluation of the Effects of Winter Wheat Yield and Quality in Different Soils under the Background of Warming

JIN Li-hui, YANG Hai-chao, WANG Xiao-yi, MIAO Shu-jie, QIAO Yun-fa   

  1. School of Ecology and Applied Meteorology, Nanjing University of Information Science & Technology, Nanjing 210044, China
  • Received:2023-05-11 Online:2024-03-20 Published:2024-03-13

摘要: 利用冬小麦品种‘镇麦168’,以黄棕壤、砂礓黑土、风沙土、红壤、潮土、黑土、黄土、灰钙土、紫色土、砖红壤、盐碱土和棕壤共12种典型农田土壤为基质,在开放式增温系统开展模拟大气增温框栽试验。试验设置常温对照(CK)和增温1.5℃(eT)两个处理,增温处理为冬小麦全生育期增温。以成熟期冬小麦单穗粒数、千粒重等表征产量变化,籽粒淀粉、蛋白质及其组分等营养指标体现品质构成。结果表明:(1)全生育期增温分别使黄棕壤、风沙土、黑土、黄土、灰钙土和紫色土冬小麦较常温对照减产33.82%、20.96%、16.60%、55.92%、28.45%和21.19%,但潮土冬小麦增产16.13%(P<0.05),其他土壤条件下冬小麦产量无明显变化。(2)就冬小麦营养品质,直链淀粉和支链淀粉含量在增温作用下较常温对照存在不同程度下降,且直链淀粉降幅大于支链淀粉,在红壤、黑土、黄土、灰钙土、紫色土、盐碱土和棕壤条件下冬小麦总淀粉含量显著降低(P<0.05)。籽粒蛋白质及其组分,清蛋白和球蛋白呈显著增加趋势,而醇溶蛋白和谷蛋白显著下降,且降幅大于前两者增幅,除红壤冬小麦总蛋白含量无显著变化以外,其他11种土壤条件下冬小麦总蛋白含量均较常温对照显著降低(P<0.05)。冬小麦可溶性总糖仅在潮土、灰钙土和紫色土条件下显示出显著增加趋势(P<0.05)。(3)利用隶属函数对常温对照和增温各处理进行综合品质排名,表现最好的为常温组黑土冬小麦(U=0.707),常温组中棕壤(U=0.691)、灰钙土(U=0.647)、紫色土(U=0.644)和黄土冬小麦(U=0.644)次之,品质最差的是常温下红壤冬小麦(U=0.364)和增温下红壤冬小麦(U=0.368)。除潮土冬小麦以外,其他11种土壤冬小麦品质均表现为增温劣于对照。(4)常温条件下冬小麦产量最大影响因素为单穗粒数,直接通径系数为0.630,其次为有效穗数和球蛋白,均体现为直接作用,直接通径系数分别为0.538和−0.118;增温条件下冬小麦产量最大影响因素也是单穗粒数,直接通径系数为0.603,其次为有效穗数、千粒重和总淀粉,有效穗数和总淀粉通过与单穗粒数的间接作用对冬小麦产量产生影响,间接通径系数分别为0.322和0.381。综合而言,增温通过对冬小麦产量构成和籽粒营养成分的综合作用影响品质,12种典型农田土壤中,潮土冬小麦对增温表现为正效应,其他土壤为负效应,冬小麦产量品质形成对气候变暖响应受到土壤类型的调控。

关键词: 冬小麦, 全生育期增温, 土壤类型, 产量, 品质评价

Abstract: To explore the changes in winter wheat yield and quality under global warming. The winter wheat variety ‘Zhenmai 168’ and twelve typical farmland soils, including yellow brown soil, sandy black soil, aeolian sandy soil, red soil, fluvo-aquic soil, black soil, loess, sierozem, purple soil, latosol, saline-alkali soil and brown soil were used as test materials. An open temperature increase system was carried out a simulated atmospheric warming frame experiment. The experiment established normal temperature control (CK) and warming of 1.5°C (eT) treatment, and the warming treatment throughout the whole growth period. The changes in production during the ripening stage was reflected by indicators such as the number of kernels per panicle and the weight of 1000 grains, and nutritional indicators such as the grain starch, protein and its components reflect the quality composition. The results showed as follows: (1) the open warming during the whole growth period decreased the yield of winter wheat grown in yellow-brown soil, sandy soil, black soil, loess, sierozem and purple soil by 33.82%, 20.96%, 16.60%, 55.92%, 28.45% and 21.19%, respectively. While the winter wheat yield in fluvo-aquic soil increased by 16.13% (P<0.05), and had no significant effect in other soils. (2) In terms of nutritional quality of winter wheat, for starch and its components, the contents of amylose and amylopectin decreased to varying degrees under the effect of warming, and the decrease in amylose was greater than that of amylopectin. The total starch content of winter wheat in red soil, black soil, loess, sierozem, purple soil, saline-alkali soil and brown soil decreased significantly (P<0.05). For grain protein and its components, albumin and globulin showed a significant increase trend, while gliadin and glutenin decreased significantly, and the decrease was greater than the increase of the first two. Except for the total protein content of winter wheat in red soil, which had no significant change, the winter wheat under other eleven types of soil all decreased significantly (P<0.05). The total soluble sugar of winter wheat showed a significant increasing trend only under fluvo-aquic soil, sierozem and purple soil conditions (P<0.05). (3) The membership function was used to comprehensively rank the quality of the normal temperature control and warming treatments. The best performers were black soil winter wheat in the normal temperature group (U=0.707), followed by the brown soil (U=0.691), sierozem (U=0.647), purple soil(U=0.644) and loess(U=0.644) winter wheat in the normal temperature control group, and the worst quality is the red soil in the normal temperature group (U=0.364) and warming group (U=0.368). Except for the fluvo-aquic soil, the quality of winter wheat in the other eleven types of soils showed that warming was worse than the control. (4) The path analysis results show that under normal temperature conditions, the biggest influencing factor on winter wheat yield is the number of kernels per panicle, with a direct path coefficient of 0.630, followed by the effective number of panicles and globulin, both of which have direct effects, with path coefficients of 0.538 and -0.118, respectively. Under warming conditions, the largest influence on factor of winter wheat is the number of kernels per panicle, with a direct path coefficient of 0.603, followed by the effective panicle number, the weight of 1000 grains and total starch. The effective panicle number and total starch have an indirect effects through the number of kernels per panicle, with path coefficients of 0.322 and 0.381, respectively. In summary, warming affected the quality of winter wheat through the combined effects of yield composition and grain nutritional composition. Among the twelve typical farmland soils, winter wheat in fluvo-aquic soil had a positive effect on warming, while in other soils had a negative effect, suggesting that the response of winter wheat yield and quality formation to climate warming was regulated by soil types.

Key words: Winter wheat, Warming throughout the growth period, Soil types, Yield, Quality evaluation