不同含水率条件下土壤中赤霉酸自然衰减规律研究

李京芳, 胡晓蕾, 陈亮. 不同含水率条件下土壤中赤霉酸自然衰减规律研究[J]. 水文地质工程地质, 2024, 51(2): 50-57. doi: 10.16030/j.cnki.issn.1000-3665.202310046
引用本文: 李京芳, 胡晓蕾, 陈亮. 不同含水率条件下土壤中赤霉酸自然衰减规律研究[J]. 水文地质工程地质, 2024, 51(2): 50-57. doi: 10.16030/j.cnki.issn.1000-3665.202310046
LI Jingfang, HU Xiaolei, CHEN Liang. Study on the natural attenuation mechanism of gibberellic acid in soil under different water content conditions[J]. Hydrogeology & Engineering Geology, 2024, 51(2): 50-57. doi: 10.16030/j.cnki.issn.1000-3665.202310046
Citation: LI Jingfang, HU Xiaolei, CHEN Liang. Study on the natural attenuation mechanism of gibberellic acid in soil under different water content conditions[J]. Hydrogeology & Engineering Geology, 2024, 51(2): 50-57. doi: 10.16030/j.cnki.issn.1000-3665.202310046

不同含水率条件下土壤中赤霉酸自然衰减规律研究

  • 基金项目: 国家自然科学基金项目(41772245;42277046)
详细信息
    作者简介: 李京芳(2000—),女,硕士研究生,主要研究方向为水资源、水环境保护与修复。E-mail:lijingfang0121@163.com
    通讯作者: 陈亮(1985—),男,博士,副教授,主要研究方向为渗流过程水量水质变化及污染物治理新技术。E-mail:liangchen@tju.edu.cn
  • 中图分类号: P641.69

Study on the natural attenuation mechanism of gibberellic acid in soil under different water content conditions

More Information
  • 作为一种施用范围广、用量大的微毒农药,赤霉酸(GA3)的高溶解度会造成其在土壤中的弱吸附和强迁移并伴随强烈的自然衰减,且受到间歇性灌溉过程中变化土壤含水率的影响,因此有必要系统研究不同含水率条件下土壤中GA3的自然衰减规律。通过设置10%、20%、30%的3种土壤含水率,研究了不同土壤含水率条件下GA3的自然衰减规律,分析了土壤微生物对GA3自然衰减过程的影响,定性识别了GA3自然衰减产物。结果表明:(1)实验结束(34 d)时初始含水率为10%、20%和30%的灭菌组和未灭菌组土壤中GA3的自然衰减率分别为87.77%、89.70%、90.70%和87.70%、94.47%、95.87%,其自然衰减半衰期分别为12.38,12.16,12.60 d和8.56,6.80,7.07 d;(2)含水率对灭菌组土壤GA3的自然衰减速率无显著影响,未灭菌组在不同土壤含水率条件下GA3自然衰减速率有差异(20%土壤含水率最大);(3)在水解作用的基础上,土壤微生物降解进一步促进了GA3的自然衰减,且生物降解贡献率为39.62%±7.58%;(4)GA3主要自然衰减产物为异构赤霉酸与赤霉烯酸(其中异构赤霉酸占比更大),未来需要进一步关注GA3自然衰减产物在环境中的生物毒性与环境风险。上述研究结果有助于进一步深入理解农业生产过程土壤中GA3的环境行为,并为其环境毒性及潜在风险评估与管控提供数据支撑。

  • 加载中
  • 图 1  灭菌组和未灭菌组土壤含水率随时间的变化

    Figure 1. 

    图 2  不同土壤含水率条件下灭菌组和未灭菌组土壤中GA3的自然衰减

    Figure 2. 

    图 3  实验过程总GA3及其自然衰减产物的HPLC谱图

    Figure 3. 

    图 4  不同土壤含水率条件下灭菌组和未灭菌组土壤中GA3的自然衰减速率

    Figure 4. 

    表 1  蓟县土壤的基本理化性质

    Table 1.  Basic physical and chemical properties of soils in Jixian County

    指标 含量 指标 含量
    pH值 7.9 ${\mathrm{PO}}^{3-}_4 $/(mg·kg−1 7.2
    有机碳(干基)/% 1.2 粒径1.0~2.0 mm占比/% 29.9
    N(干基)/(mg·kg−1 1213.7 粒径0.5~<1.0 mm占比/% 20.3
    P(干基)/(mg·kg−1 1652.2 粒径0.25~<0.5 mm占比/% 17.4
    K(干基)/(mg·kg−1 18524.3 粒径0.1~<0.25 mm占比/% 11.4
    Ca(干基)/(mg·kg−1 5223.7 粒径0.075~<0.1 mm占比/% 5.4
    ${\mathrm{NH}}^+_4 $/(mg·kg−1 5.5 粒径<0.075 mm占比/% 15.6
    ${\mathrm{NO}}^-_3 $/(mg·kg−1 2
    下载: 导出CSV

    表 2  灭菌组和未灭菌组土壤中GA3的自然衰减率、衰减速率及半衰期

    Table 2.  Degradation rate, degradation rate, and half-life of GA3 in the soil of sterilized group and non-sterilized group

    参数 实验组 含水率10% 含水率20% 含水率30%
    初始浓度
    /(mg·L−1
    灭菌0.0150.0150.015
    未灭菌0.0150.0150.015
    自然
    衰减率/%
    灭菌87.7789.7090.70
    未灭菌87.7094.4795.87
    实验
    周期/d
    灭菌343434
    未灭菌343434
    一级动力学
    方程
    灭菌ct = 0.0158e−0.056tct= 0.013e−0.057tct= 0.0112e−0.055t
    R²=0.90R²=0.94R² = 0.92
    未灭菌ct= 0.0122e−0.081tct= 0.0154e−0.102tct= 0.0159e−0.098t
    R²=0.93R²=0.96R² = 0.93
    自然衰减
    速率/d−1
    灭菌0.0560.0570.055
    未灭菌0.0810.1020.098
    半衰期/d灭菌12.3812.1612.60
    未灭菌8.566.807.07
    下载: 导出CSV
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出版历程
收稿日期:  2023-11-14
修回日期:  2023-12-27
刊出日期:  2024-03-15

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