• 《中国科学引文数据库(CSCD)》来源期刊
  • 中国科技期刊引证报告(核心版)期刊
  • 《中文核心期刊要目总览》核心期刊
  • RCCSE中国核心学术期刊

生物质种类和添加量对肥液灌溉土壤入渗特征和养分运移的影响

周英杰, 刘艳伟, 黄一峰, 刘小刚

周英杰, 刘艳伟, 黄一峰, 等. 生物质种类和添加量对肥液灌溉土壤入渗特征和养分运移的影响[J]. 华南农业大学学报, 2023, 44(4): 585-592. DOI: 10.7671/j.issn.1001-411X.202208007
引用本文: 周英杰, 刘艳伟, 黄一峰, 等. 生物质种类和添加量对肥液灌溉土壤入渗特征和养分运移的影响[J]. 华南农业大学学报, 2023, 44(4): 585-592. DOI: 10.7671/j.issn.1001-411X.202208007
ZHOU Yingjie, LIU Yanwei, HUANG Yifeng, et al. Effects of biomass types and additions on soil infiltration characteristics and nutrient transport in fertilizer irrigation[J]. Journal of South China Agricultural University, 2023, 44(4): 585-592. DOI: 10.7671/j.issn.1001-411X.202208007
Citation: ZHOU Yingjie, LIU Yanwei, HUANG Yifeng, et al. Effects of biomass types and additions on soil infiltration characteristics and nutrient transport in fertilizer irrigation[J]. Journal of South China Agricultural University, 2023, 44(4): 585-592. DOI: 10.7671/j.issn.1001-411X.202208007

生物质种类和添加量对肥液灌溉土壤入渗特征和养分运移的影响

基金项目: 云南省基础研究计划(202101AT070125);昆明理工大学分析测试基金重点项目(2021T20110170);云南省高校特色作物高效用水与绿色生产重点实验室项目(KKPS201923009)
详细信息
    作者简介:

    周英杰,硕士研究生,主要从事水肥一体灌溉相关研究,E-mail: 1780415092@qq.com

    通讯作者:

    刘艳伟,副教授,博士,主要从事节水灌溉理论与新技术研究,E-mail: liuyanwei@kust.edu.cn

  • 中图分类号: S152.7

Effects of biomass types and additions on soil infiltration characteristics and nutrient transport in fertilizer irrigation

  • 摘要:
    目的 

    探究添加不同生物质和添加量对肥液灌溉土壤入渗特征与养分运移的影响,为提升肥液灌溉效率提供理论依据。

    方法 

    以生物炭(BC)、咖啡渣(CF)和甘蔗渣(SC)作为生物质添加材料,设置4个添加量(质量分数)水平T1(0.5%)、T2(1.0%)、T3(1.5%)、T4(2.0%)。测量肥液在不同生物质添加土壤中的运移特征及养分分布,评估不同生物质添加对土壤结构的影响。

    结果 

    3种生物质对湿润锋运移与土壤累积入渗量抑制效果均表现为SC>CF>BC,各处理组内抑制效果随生物质添加量增加有所提升;和CK组相比, SCT4、CFT4和BCT4组湿润锋运移距离分别降低了38.33%、37.00%和34.00%;SCT4、CFT4和BCT4组土壤累积入渗量分别降低了31.01%、30.00%和26.60%。和CK组相比,肥液灌溉下3种生物质添加均能提升土壤中3种主要无机养分,且随生物质添加量增加土壤肥力提升;3种生物质对土壤硝态氮截留总体表现为BC>CF>SC,其中,BCT4、CFT4和SCT4组的土壤硝态氮含量分别提升了74.32%、56.00%和51.00%;3种生物质对土壤速效磷截留总体表现为CF>SC>BC,其中,CFT4、SCT4和BCT4组的土壤速效磷含量分别提升了140.70%、139.20%和30.25%;3种生物质对土壤速效钾截留总体表现为CF>BC>SC,其中,CFT4、BCT4和SCT4组的土壤速效钾含量分别提升了143.87%、126.85%和104.03%。

    结论 

    3种生物质对肥液入渗均有抑制效果,其中,生物炭效果最佳;3种生物质对肥力均有截留效果,生物炭对硝态氮截留效果最佳,咖啡渣对速效磷与速效钾截留效果最佳。

    Abstract:
    Objective 

    In order to explore the effects of different biomass additions and amounts on soil infiltration characteristics and nutrient transport in fertilizer irrigation, so as to provide a theoretical basis for improving fertilizer irrigation efficiency.

    Method 

    Biochar (BC), coffee grounds (CF) and bagasse (SC) were used as biomass additives, and four levels of addition were set including T1 (0.5%), T2 (1.0%), T3 (1.5%), and T4 (2.0%). The transport characteristics of fertilizer solution in different biomass-added soils and their nutrient distributions were measured. The effects of different biomass additions on soil structure were evaluated.

    Result 

    The inhibitory effects of three kinds of biomass on wetting front migration and soil cumulative infiltration were SC>CF>BC, and the inhibitory effects in each treatment group increased with increasing biomass addition. Compared with the CK group, the wetting front migration distances of SCT4, CFT4 and BCT4 decreased by 38.33%, 37.00% and 34.00% respectively. The cumulative soil infiltration amounts of SCT4, CFT4 and BCT4 decreased by 31.01%, 30.00% and 26.60% respectively. Compared with the CK group, the three kinds of biomass additions under the fertilizer irrigation improved the contents of three main inorganic nutrients in soil, and the soil fertility was improved with increasing biomass addition. The overall performance of soil nitrate nitrogen retention by the three kinds of biomass was BC>CF>SC. Among them, the soil nitrate nitrogen contents of BCT4, CFT4 and SCT4 increased by 74.32%, 56.00% and 51.00% respectively. The overall performance of soil available phosphorus retention by the three kinds of biomass was CF>SC>BC. Among them, the soil available phosphorus contents of CFT4, SCT4 and BCT4 increased by 140.70%, 139.20% and 30.25% respectively. The overall performance of soil available potassium retention by the three kinds of biomass was CF>BC>SC. Among them, CFT4, BCT4 and SCT4 increased the soil available potassium contents by 143.87%, 126.85% and 104.03% respectively.

    Conclusion 

    All three kinds of biomass have inhibitory effects on the infiltration of fertilizer solution with biochar being the best. The three kinds of biomass all have interception effects on fertility, meanwhile, biochar has the best interception effect on nitrate nitrogen, and coffee grounds have the best interception effect on available phosphorus and available potassium.

  • 图  1   不同处理组内水肥入渗深度随入渗时间变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  1.   Changing of the infiltration depth of water and fertilizer with infiltration time in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    图  2   不同处理组内水肥累积入渗量随入渗时间变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  2.   Changing of the cumulative infiltration of water and fertilizer with infiltration time in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    图  3   不同处理组内水肥入渗速率随入渗时间变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  3.   Changing of water and fertilizer infiltration rate with infiltration time in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    图  4   不同处理组内硝态氮累积随土壤深度变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  4.   Changing of nitrate nitrogen accumulation with soil depth in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    图  5   不同处理组内速效磷累积随土壤深度变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  5.   Changing available phosphorus accumulation with soil depth in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    图  6   不同处理组内速效钾累积随土壤深度变化关系

    T1、T2、T3和T4分别为生物质添加量(w) 0.5%、1.0%、1.5%和2.0%

    Figure  6.   Changing of available potassium accumulation with soil depth in different treatment

    T1,T2,T3 and T4 represent biomass additions of 0.5%,1.0%,1.5% and 2.0% respectively

    表  1   不同入渗模型拟合关系

    Table  1   Fitting relationships of different infiltration models

    生物质
    Biomass
    处理组
    Treatment group
    KostiakovPhilip
    $ K $$ n $$ {R}^{2} $$ A $$ B $$ {R}^{2} $
    生物炭
    Biochar
    (BC)
    CK 5.577 0.260 0.998 3.129 −0.115 0.913
    BCT1 3.810 0.323 0.997 2.529 −0.077 0.968
    BCT2 3.478 0.320 0.997 2.217 −0.064 0.966
    BCT3 3.685 0.281 0.981 2.030 −0.061 0.910
    BCT4 3.125 0.291 0.974 1.685 −0.434 0.922
    咖啡渣
    Coffee grounds
    (CF)
    CK 5.577 0.260 0.998 3.129 −0.115 0.913
    CFT1 3.088 0.361 0.999 2.245 −0.057 0.991
    CFT2 3.035 0.342 0.997 2.008 −0.049 0.983
    CFT3 3.088 0.316 0.995 1.880 −0.050 0.970
    CFT4 3.084 0.295 0.993 1.781 −0.052 0.951
    甘蔗渣
    Bagasse
    (SC)
    CK 5.577 0.260 0.998 3.129 −0.115 0.913
    SCT1 2.665 0.382 0.996 2.063 −0.048 0.985
    SCT2 2.197 0.404 0.997 1.827 −0.040 0.990
    SCT3 2.030 0.401 0.997 1.615 −0.031 0.990
    SCT4 1.491 0.447 0.997 1.420 −0.003 0.997
    下载: 导出CSV
  • [1] 李冬初, 黄晶, 马常宝, 等. 中国农耕区土壤有机质含量及其与酸碱度和容重关系[J]. 水土保持学报, 2020, 34(6): 252-258.
    [2] 刘振杰, 李鹏飞, 黄世威, 等. 小麦秸秆生物质炭施用对不同耕作措施土壤碳含量变化的影响[J]. 环境科学, 2021, 42(6): 3000-3009.
    [3] 王艳群, 彭正萍, 薛世川, 等. 过量施肥对设施农田土壤生态环境的影响[J]. 农业环境科学学报, 2005, 24(S1): 81-84.
    [4]

    ZHU X, CHEN B, ZHU L, et al. Effects and mechanisms of biochar-microbe interactions in soil improvement and pollution remediation: A review[J]. Environmental Pollution, 2017, 227: 98-115. doi: 10.1016/j.envpol.2017.04.032

    [5]

    LEHMANN J, GAUNT J, RONDON M. Bio-char sequestration in terrestrial ecosystems: A review[J]. Mitigation and Adaptation Strategies for Global Change, 2006, 11(2): 395-419.

    [6] 刘书田, 窦森, 郑伟, 等. 基于配方施肥数据集的有机碳含量与温度和降水量相关性研究[J]. 农业环境科学学报, 2016, 35(7): 1413-1420.
    [7] 魏阳, 彭勃, 汪元南, 等. 利用复合菌系处理甘蔗渣及城市污泥堆肥效果[J]. 科学技术与工程, 2019, 19(7): 316-320.
    [8] 田丹, 屈忠义, 李波, 等. 生物炭对砂土水力特征参数及持水特性影响试验研究[J]. 灌溉排水学报, 2013, 32(3): 135-137.
    [9] 廉辰, 于嘉佳, 高婷, 等. 3种壳类生物质炭对南方红壤理化性质的动态影响[J]. 华南农业大学学报, 2022, 43(1): 20-27.
    [10] 周建民, 沈仁芳. 土壤学大辞典[M]. 北京: 科学出版社, 2013.
    [11] 鲍士旦. 土壤农化分析[M]. 3版. 北京: 中国农业出版社, 1981.
    [12] 范严伟, 赵文举, 冀宏. 膜孔灌溉单孔入渗Kostiakov模型建立与验证[J]. 兰州理工大学学报, 2012, 38(3): 61-66.
    [13]

    PHILIP J R. The theory of infiltration: 1: The infiltration equation and its solution[J]. Soil Science, 1957, 83(5): 345-358. doi: 10.1097/00010694-195705000-00002

    [14] 刘春成, 李毅, 任鑫, 等. 四种入渗模型对斥水土壤入渗规律的适用性[J]. 农业工程学报, 2011, 27(5): 62-67.
    [15]

    SONE J S, OLIVEIRA P T S, EUCLIDES V P B, et al. Effects of nitrogen fertilisation and stocking rates on soil erosion and water infiltration in a Brazilian Cerrado farm[J]. Agriculture, Ecosystems & Environment, 2020, 304: 107159.

    [16]

    XIAO Y, HUANG Z, YANG F, et al. Dynamics of soil moisture and salt content after infiltration of saline ice meltwater in saline-sodic soil columns[J]. Pedosphere, 2017, 27(6): 1116-1124. doi: 10.1016/S1002-0160(17)60465-X

    [17]

    ALAOUL A. Modelling susceptibility of grassland soil to macropore flow[J]. Journal of Hydrology, 2015, 525: 536-546. doi: 10.1016/j.jhydrol.2015.04.016

    [18] 包维斌, 白一茹, 赵云鹏, 等. 生物炭添加对宁夏中部旱区土壤水分入渗及持水性的影响[J]. 土壤通报, 2018, 49(6): 1326-1332.
    [19]

    HUSSAIN R, KUMAR GHOSH K, RAVI K. Impact of biochar produced from hardwood of mesquite on the hydraulic and physical properties of compacted soils for potential application in engineered structures[J]. Geoderma, 2021, 385: 114836. doi: 10.1016/j.geoderma.2020.114836

    [20]

    LIM T J, SPOKAS K A, FEYEREISEN G, et al. Predicting the impact of biochar additions on soil hydraulic properties[J]. Chemosphere, 2016, 142: 136-144. doi: 10.1016/j.chemosphere.2015.06.069

    [21]

    JEFFERY S, MEINDERS M B J, STOOF C R, et al. Biochar application does not improve the soil hydrological function of a sandy soil[J]. Geoderma, 2015, 251-252: 47-54. doi: 10.1016/j.geoderma.2015.03.022

    [22] 李帅霖, 王霞, 王朔, 等. 生物炭施用方式及用量对土壤水分入渗与蒸发的影响[J]. 农业工程学报, 2016, 32(14): 135-144.
    [23]

    LIANG B Q, LEHMANN J, SOHI S P, et al. Black carbon affects the cycling of non-black carbon in soil[J]. Organic Geochemistry, 2010, 41(2): 206-213. doi: 10.1016/j.orggeochem.2009.09.007

    [24]

    PUGET P, CHENU C, BALESDENT J. Dynamics of soil organic matter associated with particle size fractions of water-stable aggregates[J]. European Journal of Soil Science, 2000, 51(4): 595-605. doi: 10.1111/j.1365-2389.2000.00353.x

    [25] 管瑶, 雷廷武, 刘芳芳, 等. 土壤点源入渗自动测量系统监测滴头下土壤湿润过程[J]. 农业工程学报, 2016, 32(14): 1-7.
    [26] 刘目兴, 聂艳, 于婧. 不同初始含水率下粘质土壤的入渗过程[J]. 生态学报, 2012, 32(3): 871-878.
    [27]

    LEHMANN J. Bio-energy in the black[J]. Frontiers in Ecology and the Environment, 2007, 5(7): 381-387. doi: 10.1890/1540-9295(2007)5[381:BITB]2.0.CO;2

    [28]

    CRUZ R, MENDES E, TORRINHA Á, et al. Revalorization of spent coffee residues by a direct agronomic approach[J]. Food Research International, 2015, 73: 190-196. doi: 10.1016/j.foodres.2014.11.018

    [29] 黄绍文, 金继运. 土壤钾形态及其植物有效性研究进展[J]. 土壤肥料, 1995(5): 23-29.
    [30] 王亚琼, 牛文全, 段晓辉, 等. 生物炭对关中塿土不同形态钾素含量的影响[J]. 东北农业科学, 2021, 46(2): 43-46.
图(6)  /  表(1)
计量
  • 文章访问数:  123
  • HTML全文浏览量:  7
  • PDF下载量:  12
  • 被引次数: 0
出版历程
  • 收稿日期:  2022-08-02
  • 网络出版日期:  2023-09-03
  • 发布日期:  2023-05-24
  • 刊出日期:  2023-07-09

目录

    /

    返回文章
    返回