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保护性耕作对丘陵区水稻土团聚体稳定性的影响
引用本文:唐晓红, 魏朝富, 吕家恪, 罗友进, 谢德体, 潘根兴, 曾希柏. 保护性耕作对丘陵区水稻土团聚体稳定性的影响[J]. 农业工程学报, 2009, 25(11): 49-54.
作者姓名:唐晓红  魏朝富  吕家恪  罗友进  谢德体  潘根兴  曾希柏
作者单位:1.四川农业大学都江堰校区城乡建设学院,都江堰 611830;2.西南大学资源环境学院,重庆400716;3.南京农业大学农业资源与生态环境研究所,南京 210095;4.中国农业科学院农业环境与可持续发展研究所,北京 100081
基金项目:国家科技支撑计划课题(2006BAD05801);国家自然科学基金资助项目(40231016);四川农业大学青年科技基金项目(N200903)
摘    要:长期保护性耕作通过增加土壤有机碳而成为稻田土壤结构改良的一项有效措施,而保护性耕作对土壤团聚体稳定机制的影响尚未完全清楚。本文供试土样采自耕作制定位试验水旱轮作、冬水免耕、垄作免耕和厢作免耕耕层(0~ 20 cm)土壤,土样经过糊化作用、湿润作用和再次糊化作用等预处理,用以阐明稻田土壤团聚体的破碎机制。研究结果表明:糊化作用和湿润作用后紫色水稻土团聚体稳定性差异不明显,而保护性耕作显著影响团聚体的稳定性。糊化作用后团聚体水稳性强弱顺序为:垄作免耕>厢作免耕>冬水免耕>水旱轮作,湿润作用后团聚体水稳性强弱顺序为:厢作免耕>垄作免耕>冬水免耕>水旱轮作。糊化作用下团聚体稳定性与有机碳浓度相关性不显著(r=0.432,p>0.05),湿润作用下团聚体稳定性与有机碳浓度呈极显著正相关(r=0.626,p<0.01)。因此,研究结果说明保护性耕作有利于紫色水稻土大团聚体有机碳含量提高,进而增强团聚体的水稳性。

关 键 词:团聚体  稳定性  有机碳  保护性耕作  水稻土
收稿时间:2007-10-29
修稿时间:2008-08-16

Effects of conservation tillage on aggregate stability of paddy soil in hilly region
Tang Xiaohong, Wei Chaofu, Lü Jiake, Luo Youjin, Xie Deti, Pan Genxing, Zeng Xibai. Effects of conservation tillage on aggregate stability of paddy soil in hilly region[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(11): 49-54.
Authors:Tang Xiaohong  Wei Chaofu  Lü Jiake  Luo Youjin  Xie Deti  Pan Genxing  Zeng Xibai
Affiliation:1.College of Urban and Rural Development, Sichuan Agricultural University Dujiangyan Campus, Dujiangyan 611830, China;2.College of Resource and Environment, Southwest University, Chongqing 400716, China;3.Institute of Resources, Ecosystem and Environment of Agriculture, Nanjing Agric. Univ. , Nanjing 210095, China;4.Institute of Environment and Sustainable Development for Agriculture, Chinese Academy of Agricultural Science, Beijing 100081, China
Abstract:Long-term conservation tillage is an effective agricultural management to improve soil structure in severely destroyed paddy soil by increase of soil organic carbon (SOC). More work is still needed to understand the impacts of conservation tillage on the mechanisms of aggregates stability. Soil samples in 0-20 cm layer were adopted from the long-term tillage experiment: (1) paddy-upland rotation and plain culture (rice- rape) (PU-R-RR), (2)no-tillage and ridge culture (rice-fallow) (NT-R-RF), (3) no-tillage and ridge culture (rice-rape) (NT-R-RR) and (4) no-tillage and plain culture (rice- rape) (NT-P-RR). Different pretreatments, such as slaking in fast wetting, wetting and subsequent slaking, were applied to simulate the breakdown mechanisms of aggregates in paddy soil. The results showed that no significant difference of aggregate stability between slaking and wetting pretreatments was observed, while tillage patterns affected greatly aggregate stability. The aggregate stability under slaking and wetting pretreatment ranked in the order of NT-R-RR > NT-P-RR > NT-R-RF > PU-R-RR and NT-P-RR > NT-R-RR > NT-R-RF > PU-R-RR, respectively. The organic carbon concentrations in aggregates were significantly positive related to the aggregates stability under wetting(r=0.626, p<0.01), while low correlation linear relationships were observed under slaking treatment (r=0.432, p>0.05). The results suggest that long-term conservation tillage favorably led to the increase of SOC concentrations in aggregates and the enhancement of aggregates water stabilization.
Keywords:aggregates   stability   organic carbon   conservation tillage   paddy soil
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