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沼液沼渣协同作用对土壤水分入渗、蒸发及有机质量影响的试验研究OA

Synergistic effects of biogas slurry and biogas residue applications on soil water movement,thermal regime and organic matter content

中文摘要英文摘要

[目的]揭示沼液沼渣协同作用对土壤水分运动规律影响的机理.[方法]设置 4个沼渣混掺量(沼渣占土壤质量百分比):0%(S0)、1%(S1)、2%(S2)、4%(S4)和 3个沼液配比水平(沼液:水,体积比):0(W0)、1∶8(W1:8)和 1∶4(W1:4),采用室内试验探求不同处理对土壤持水性能、入渗湿润锋、累积入渗量、累积蒸发量、温度日变幅和有机质量的响应规律,并采用幂函数模型、Kostiakov模型和 Rose模型对湿润锋运移、累积入渗量和累积蒸发量的动态变化进行了拟合分析.[结果]①土壤持水能力的提升与沼渣混掺量及沼液施用配比呈正相关,S4W1:4处理的土壤体积含水率较 S0W0处理提高了 15.84%,van-Genuchten模型可以精确拟合各处理土壤水分特征曲线(R2≥0.998 5),二者分别与土壤中较小孔隙、较大孔隙占比呈正、负相关关系.②随沼液配比和沼渣混掺量的增加,延缓水分入渗的效果越明显,相同灌溉量(120 mm)下 S4W1:4 处理所需时间较 S0W0 处理延迟了106.49%,幂函数能够准确描述湿润锋运移距离 Z(cm)与入渗时间 t(min)的关系(R2≥0.993 2;RRMSE≤5.50%;NS≥0.993 4),Kostiakov入渗模型能较好模拟不同处理的累积入渗量 I(mm)和入渗时间 t(min)之间的关系(R2≥0.994 7;RRMSE≤5.95%;NS≥0.992 5).③土壤累积蒸发量随沼渣混掺量的增加呈先升高后降低的趋势,随沼液配比的增大而趋于减小,S4W1:4处理下土壤累积蒸发量最小(32.34 mm),Rose模型可以准确描述累积蒸发量 E(mm)与时间 t(d)的关系(R2≥0.953 5;RRMSE≤4.88%;NS≥0.958 7);各土层温度日变幅随沼渣混掺量的增加呈先增大后减小的趋势,沼液灌溉降低了各土层温度日变幅,沼液配比为 1∶4时各土层内温度日变幅值达到最低;土壤有机质量与沼渣混掺量及沼液施用配比呈正相关.[结论]沼渣混掺量4%、沼液配比1∶4处理能够更好地平衡粉壤土的入渗和蒸发特性.

[Objective]Biogas slurry and residue are rich in nutrients,and their combined application can improve soil quality.This study experimentally investigates the synergistic effect of biogas slurry and biogas residue on soil water movement and soil organic matter.[Method]The laboratory infiltration experiment included four biogas residue application rates(mass of biogas residue/mass of soil):0%(S0),1%(S1),2%(S2)and 4%(S4),and three biogas slurry concentration treatments(volumetric ratio of biogas slurry to water):0(W0),1∶8(W1:8)and 1∶4(W1:4).For each treatment,we measured soil water-holding capacity,wetting front advancement,cumulative infiltration,cumulative evaporation,diurnal soil temperature variation,and soil organic matter content.Temporal variations in wetting front migration distance,cumulative infiltration,and cumulative evaporation were fitted to the power function,Kostiakov model and Rose model,respectively.[Result]①Soil water-holding capacity increased with increasing biogas residue application rate and biogas slurry concentration.The volumetric soil water content under S4W1:4 was 15.84%higher than that under S0W0.The water retention curves of all treatments were well fitted by the van-Genuchten model,with a coefficient of determination(R2)≥0.998 5.②Increasing biogas residue application and biogas slurry concentration remarkably reduced water infiltration.When irrigation was 120 mm,the S4W1:4 treatment prolonged the infiltration duration by 106.49%compared with S0W0.The relationship between wetting front distance and infiltration time can be described by a power-law function(R2≥0.993 2,RRMSE≤0.055 0,NS≥0.993 4).The Kostiakov model well described the temporal change in cumulative infiltration(R2≥0.994 7,RRMSE≤0.059 5,NS≥0.992 5).③With the increase in biogas residue application rate,soil evaporation first increased and then decreased;increasing biogas slurry concentrations reduced soil evaporation.The cumulative evaporation in the S4W1:4 was 32.34 mm,the lowest among all treatments.The Rose model accurately described the temporal change in cumulative evaporation(R2≥0.953 5,RRMSE≤0.048 8,NS≥0.958 7).With increasing biogas residue application,the diurnal temperature amplitude of each soil layer initially increased and then decreased.Biogas slurry irrigation effectively reduced diurnal soil temperature variation.Soil organic matter content was positively correlated with both biogas residue application rate and biogas slurry concentration.[Conclusion]The combined application of 4%biogas residue and 1∶4 biogas slurry dilution can effectively balance soil water infiltration and evaporation in silty loam soil.

郑健;范盼盼;马彪;刘海涛;王俊杰;郭亚军

兰州理工大学 土木与水利工程学院,兰州 730050||甘肃省太阳能与生物质互补多联供系统重点实验室,兰州 730050兰州理工大学 土木与水利工程学院,兰州 730050||甘肃省太阳能与生物质互补多联供系统重点实验室,兰州 730050自然资源部退化及未利用土地整治工程重点实验室,西安 710000||陕西农业发展集团有限公司,西安 710000自然资源部退化及未利用土地整治工程重点实验室,西安 710000||陕西农业发展集团有限公司,西安 710000自然资源部退化及未利用土地整治工程重点实验室,西安 710000||陕西农业发展集团有限公司,西安 710000甘肃省疏勒河流域水资源利用中心,甘肃 玉门 735211

农业科技

沼液沼渣土壤水分特征曲线蒸发量入渗量土壤温度有机质

biogas slurrydigestatesoil moisture characteristic curvecumulative evaporationcumulative infiltration volumesoil temperatureorganic matter

《灌溉排水学报》 2026 (7)

101-113,13

国家自然科学基金项目(52469011)自然资源部退化及未利用土地整治工程重点实验室开放基金项目(SXDJ2024-08)2025年水利科学试验研究及技术推广计划(甘水建管发[2025]24号,25GSLK079)

10.13522/j.cnki.ggps.2025326

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