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晋西北沙区不同耕作方式土壤水分及效益研究
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摘要
通过对土壤容重、土壤田间持水量、饱和含水量、剖面土壤含水量以及玉米产量的测定分析,研究不同耕作方式对土壤物理性状及玉米经济效益的影响。结果表明:相对于传统耕作不覆盖(CT),在0~5cm土层深度,免耕秸秆覆盖(NTS)可以显著降低土壤容重,传统耕作喷洒保水剂(CTA)和传统耕作塑料地膜覆盖(CTF)对降低土壤容重也有一定效果;NTS处理可以提高0~10cm土层的田间持水量,CTA处理对田间持水量的变化有一定的稳定作用,CTF处理对田间持水量的影响较为不利;不同耕作处理的饱和含水量变化与田间持水量变化相似,NTS处理具有较好的饱和含水能力,而CTF处理饱和含水能力最弱;在10~50cm土层,CTF处理的土壤含水量最高,CTA处理较高,生长期内NTS处理土壤含水量变化较稳定;经济效益为CTF>CT>CTA>NTS。
Based on the measurement and analysis of soil bulk density,field capacity,saturated water content and profile soil water content and maize production.The results showed that,compared to conventional tillage(CT),NTS significantly reduced the soil bulk density in 0~5cm soil depth.To some extent,CTF and CTA treatments could reduce the soil bulk density as well.NTS could increase 0 ~ 10 cm soil field capacity,CTA have a stabilizing effect on the field capacity variations.However,the field capacities under CTF were lower.Similarly,saturated water contents under different tillage treatments had similar changes as the field capacity,NTS had the best saturated and water-holding capacity,whereas the CTF with the worst capacity.The soil water contents at 10 ~ 50 cm soil depth under CTF and CTA were higher than other tillage managements.The soil water contents under NTS were more stable in the whole corn growing season than other tillage managements.The economic benefits followed the order;CTF>CT>CTA>NTS.
引文
[1]高焕文,李问盈,李洪文.中国特色保护性耕作技术[J].农业工程学报,2003,19(3):1-4
    [2]鲁向晖,隋艳艳,王飞,等.保护性耕作技术对农田环境的影响研究[J].干旱地区农业研究,2007,25(3):66-72
    [3]谢瑞芝,李少昆,李小君,等.中国保护性耕作研究分析-保护性耕作与作物生产[J].中国农业科学,2007,40(9):1914-1924
    [4]张仁陟,黄高宝,蔡立群,等.几种保护性耕作措施在黄土高原旱作农田的实践[J].中国生态农业学报,2013,21(1):61-69
    [5]辛平,黄高宝,张国盛,等.耕作方式对表层土壤饱和导水率及紧实度的影响[J].甘肃农业大学学报,2005,40(2):203-207
    [6]刘爽,张兴义.保护性耕作下黑土水热动态研究[J].干旱地区农业研究,2010,28(6):16-21
    [7]刘建忠,师江澜,雷金银,等.毛乌素沙地南缘不同免耕农田土壤理化性质及玉米产量差异分析[J].干旱地区农业研究,2006,24(6):29-34
    [8]CasselDK,RaczkowskiC W,DentonHP.Tillage effects on comproductionand soil physical conditions[J].Soil Sciences Society ofAmericaJournal,1995,59(5):1436-1443
    [9]Dao T H.Tillage and crop residue effects on carbon dioxide evolutionand carbon storage in a paleustoll[J].Soil Sciences Society of America Journal,1998,62(1):250-256
    [10]孙利军,张仁陟,黄高宝,等.保护性耕作对黄土高原旱地地表土壤理化性状的影响[J].干旱地区农业研究,2007,25(6):207-212
    [11]王建政.旱地小麦保护性耕作对土壤水分的影响[J].中国水土保持科学,2007,5(5):71-74
    [12]黄高宝,郭清毅,张仁陟,等.保护性耕作条件下旱地农田麦豆双序列轮作体系的水分动态及产量效应[J].生态学报,2006,26(4):1176-1185
    [13]李玲玲,黄高宝,张仁陟,等.不同保护性耕作措施对旱作农田土壤水分的影响[J].生态学报,2005,25(9):2326-2332
    [14]杨爱民,刘孝盈.发展保护性耕作技术有效防治耕地土壤侵蚀[J].中国水土保持科学,2010,8(6):47-52
    [15]罗珠珠,黄高保,张国盛.保护性耕作对黄土高原旱地表面土容重和水分入渗的影响[J].干旱地区农业研究,2005,23(4):7-11

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