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不同耕作方式对广西旱坡地土壤粒径分布特征的影响

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[目的]针对南方旱坡地犁底层上移、土壤水肥流失严重、产量不稳等问题,通过探讨不同耕作方式对旱坡地土壤粒径分布特征的影响,为构建和改善土壤耕层结构、促进作物根系生长、选择有效的耕作方式和作物提质增效提供理论依据。[方法]以广西旱坡地主栽甘蔗品种"桂糖44号"为供试作物,在广西钦州市开展大田试验,设置3种耕作方式(粉垄耕作、旋耕、免耕),采用激光粒度仪测定甘蔗地0~40 cm土层中土壤的粒径分布。通过对土壤粒径组成、土壤质地、粒度参数特征和粒度频率分布的研究,阐明不同耕作措施对调控土壤粒径分布的作用。[结果](1)不同耕作处理中土壤主要以中砂粒、细砂粒和粉粒为主,占比高达75。10%~87。59%;土壤质地类型可以划分为砂土、壤质砂土和砂质壤土。(2)各土层土壤整体分选效果极好,土壤平均粒径在2。66~4。58 mm;偏度表现为极负偏,表明土壤粒度中粗粒物质占比远大于细粒物质;土壤峰度等级在很宽平和中等之间,且随着土壤深度的增加土壤峰度等级趋于宽平。(3)与旋耕和免耕相比,粉垄耕作增加土壤耕层深度,降低了表层土壤中粘粒、粉粒和细砂粒含量,使其在耕作底层累积;同时土壤粒径分布频率曲线由双峰分布变为单峰分布,且峰值高度、峰值范围对应粒径大小和土壤粒度累计频率曲线斜率也远大于旋耕和免耕处理,表明粉垄耕作使得土壤粒径分布更加集中。[结论]不同的土壤耕作方式可以显著的改变土壤粒径分布,进而促进构建合理的土壤耕层结构和作物根系生长发育。粉垄耕作处理对构建土壤耕层结构效果较好,土壤粒径整体趋于粗粒化,促进土壤的不均匀性,增加土壤结构稳定性。研究结果可进一步在广西地区旱坡地种植管理中推广应用,确保农作物增产稳产。
Effect of different tillage methods on soil particle size distribution characteristics in dry sloping fields of Guangxi
[Objective]This study aimed to address the challenges of subsoil compaction,significant soil and nutrient loss,and unstable crop yields in the dry sloping of southern China.It investigated the impacts of various tillage methods on soil particle size distribution to provide a theoretical foundation for optimizing soil tillage layer structure,promote crop root development,and select efficient tillage practices to enhance crop quality and yield.[Method]Using the sugarcane variety"Gui Sugar 44"as the test crop,field experiments were conducted on dry slopes in Qinzhou City,Guangxi,China.Three tillage methods(Fen-long tillage,rotary tillage,and no-tillage)were implemented,with no-tillage as the control treatment.A laser particle size analyzer was used to determine the soil particle size distribution within the 0-40 cm soil layer.The effects of different tillage practices on soil particle size distribution were elucidated by analyzing soil particle size composition,soil texture,particle size parameter characteristics,and particle size frequency distribution.[Result]The soil in different tillage treatments was mainly composed of medium sand,fine sand and silt,accounting for 75.10%-87.59%.Soil textures were classified as sandy soil,sandy loam,and loamy sand.The overall sorting effect of soil in each soil layer is excellent,with mean particle sizes ranging from 2.66 to 4.58 mm.The skewness was strongly negative,indicating a greater proportion of coarse particles than fine ones.Kurtosis values ranged from broad-flat to moderate,with a tendency toward broad-flat as soil depth increased.Compared with rotary tillage and no-tillage,Fen-long tillage significantly increased the depth of the tillage layer,reduced the clay,silt,and fine sand content in the topsoil,thus leading to their accumulation in the subsoil.Moreover,the soil particle size distribution frequency curve shifted from a bimodal to an unimodal distribution.The peak height,peak width corresponding to particle size,and the cumulative frequency curve slope were much higher under Fen-long tillage compared with those of rotary tillage and no-tillage.This suggests that Fen-long tillage resulted in a more concentrated soil particle size distribution.[Conclusion]Various soil tillage methods can profoundly influence soil particle size distribution,thereby fostering the development of an optimal tillage structure and stimulating robust crop root growth.The Fen-long tillage technique is especially effective in establishing an optimal tillage structure,which leads to a notable coarsening of soil particles,thus enhancing soil heterogeneity,and improving soil structural stability.It can be further applied in the planting management of dry slope land in Guangxi to ensure the increase and stable yield of crops.

tillage methodsdry slopessoil particle size distributionsoil texturesoil particle size parameters

张文龙、邵金华、黄凯、陈立民、韦本辉、黄国勤

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江西农业大学 生态科学研究中心/作物生理生态与遗传育种教育部重点实验室,江西 南昌 330045

广西壮族自治区水利科学研究院 广西水工程材料与结构重点实验室,广西 南宁 530023

广西壮族自治区钦州市灌溉试验站,广西 钦州 535000

广西壮族自治区农业科学院 经济作物研究所,广西 南宁 530007

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耕作方式 旱坡地 土壤粒径分布 土壤质地 土壤粒度参数

2024

江西农业大学学报
江西农业大学

江西农业大学学报

CSTPCD北大核心
影响因子:0.748
ISSN:1000-2286
年,卷(期):2024.46(6)