中国农业气象 ›› 2022, Vol. 43 ›› Issue (08): 633-643.doi: 10.3969/j.issn.1000-6362.2022.08.004

• 农业气象灾害 栏目 • 上一篇    下一篇

越冬期埋土防寒层厚度对贺兰山东麓葡萄园土壤温度的影响

王静,张晓煜,张磊,胡宏远,李娜,李红英   

  1. 中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室/宁夏气象防灾减灾重点实验室/宁夏气象科学研究所,银川 750002
  • 收稿日期:2021-10-29 出版日期:2022-08-20 发布日期:2022-08-16
  • 通讯作者: 张晓煜,研究员,主要从事酿酒葡萄气象研究。 E-mail:zhang_xynet@163.com
  • 作者简介:王静,E-mail:wj19870122@163.com
  • 基金资助:
    国家自然科学基金面上项目(41675114);宁夏自然科学基金(2020AAC03466);科技部科技助力经济2020重点专项(KJZLJJ 202003);中国气象创新发展专项(CXFZ2021J066)

Effects of the Thickness of Buried Soil for Cold Prevention on the Vineyard Soil Temperature during the Overwintering Period at the Eastern Foot of Helan Mountain

WANG Jing, ZHANG Xiao-yu, ZHANG Lei, HU Hong-yuan, LI Na, LI Hong-ying   

  1. Key Laboratory for Meteorological Disaster Monitoring and Early Warning and Risk Management of Characteristic Agriculture in Arid Regions, China Meteorological Administration/Ningxia Key Lab for Meteorological Disaster Prevention and Reduction/Ningxia Meteorological Science Institute, Yinchuan 750002, China
  • Received:2021-10-29 Online:2022-08-20 Published:2022-08-16

摘要: 2019/2020年和2020/2021年冬季于贺兰山东麓葡萄园开展不同埋土防寒层厚度试验,结合不同深度土壤温度监测结果,研究越冬期葡萄园埋土防寒层覆盖下根区土壤温度变化规律,明确不同埋土防寒层厚度对根区土壤温度和葡萄越冬冻害的影响,为葡萄越冬冻害监测、评估及葡萄园冬季埋土管理提供参考。结果表明:(1)酿酒葡萄越冬期(12月−翌年2月)土壤温度呈先下降后上升的趋势;土壤温度随土层深度的增加而增加,波动随深度增加而缩小,埋土防寒层的覆盖,进一步减少了土壤温度的波动。(2)土壤温度随着埋土防寒层厚度的增加而增加,与不埋土处理(H0)相比,埋土防寒层厚度60cm(H60)处理, 20cm日最低土壤温度冬季可提高0.2~2.7℃,冬季平均可提高1.1℃;40cm土壤温度冬季可提高0.1~1.3℃,冬季平均可提高0.6℃。(3)0cm、20cm、40cm土壤温度日较差随着埋土防寒层厚度增加而减小,且极值出现时间依次滞后,60cm土壤温度几乎恒定。(4)20cm土壤温度,根干(C0)处显著高于距根干50cm(C50)、距根干100cm( C100)和距根干150cm(C150)(P<0.05),距离根干越远土壤温度越低。土壤温度最低日,埋土防寒层厚度30cm、40cm、50cm三个处理根干(C0)处20cm土层温度较C50、C100和C150分别提高1.7~2.2℃、1.7~3.3℃、2.4~3.4℃。可见,根系受冻风险随土壤深度增加而降低,增加埋土防寒层厚度可提高土壤温度,减少土壤温度的波动,最低温度出现的时间随着埋土防寒层厚度增加而出现滞后。越冬冻害发生程度随埋土厚度增加而减少,其中副根受冻率高于主根。

关键词: 土壤温度, 酿酒葡萄, 埋土防寒层厚度, 越冬冻害, 影响

Abstract: During the two 2019–2020 and 2020–2021 winters, field experiments with different thicknesses of buried soil for cold prevention were carried out in the vineyard at the eastern foot of Helan Mountain region. Combined with the monitoring results of soil temperature at different depths during the overwintering period, changes in root-zone soil temperature in the buried soil area of the vineyard were analyzed in this study. Understanding the effects of different thicknesses of buried soil on soil temperature could help the local grape community to assess freezing injury and manage buried soil during the overwintering period. The results showed that: (1) during the overwintering period of wine grapes, the soil temperature firstly decreased and then increased, and increased with the increase of soil depth, but the fluctuation decreased with the increase of soil depth. As the thickness of buried soil for cold prevention increased, the fluctuation of soil temperature was reduced. (2) The daily minimum soil temperature increased with the thickness of buried soil increased. Compared with no-buried soil (H0), buried soil that is 60cm thick (H60) improved the winter soil temperature at the depths of 20 cm and 40 cm by 0.2–2.7℃ (with an average of 1.1℃) and 0.1–1.3℃ (with an average of 0.6℃), respectively. (3) As the thickness of buried soil increased, at the three depths of 0cm, 20cm, and 40cm, the diurnal soil temperature range showed a decrease and the occurrence of the lowest soil temperature showed a time lag. By contrast, soil temperature at the depth of 60 cm was close to being constant. (4) Soil temperature was significantly (P<0.05) higher at the taproot zone (C0) than at the root zones that are 50cm, 100cm, and 150cm away from the taproot (C50, C100, and C150). The further away from the taproot, the lower the soil temperature was. On days when soil temperature was the lowest during the overwintering period, for the three treatments of 30 cm, 40 cm, and 50 cm thick buried soil, soil temperature at the depth of 20cm at C0 was 1.7–2.2℃, 1.7–3.3℃, and 2.4–3.4℃ higher than at the root zones of C50, C100, and C150, respectively. Overall, the risk of root being damaged by freezing decreased with the increase of soil depth. Thicker buried soil could improve the soil temperature by more and hence reduce the fluctuations of soil temperature. As the thickness of buried soil increased, the occurrence of the lowest soil temperature was delayed during the overwintering period. The chance of winter freezing injury occurrence was reduced with the increase of the thickness of buried soil; the winter freezing injury was more likely to affect the secondary roots than the taproot.

Key words: Soil temperature, Wine grapes, Thickness of buried soil for cold prevention, Freezing injury, Effects