袁俊吉, 彭思利, 蒋先军, 谢德体. 稻田垄作免耕对土壤团聚体和有机质的影响[J]. 农业工程学报, 2010, 26(12): 153-160.
    引用本文: 袁俊吉, 彭思利, 蒋先军, 谢德体. 稻田垄作免耕对土壤团聚体和有机质的影响[J]. 农业工程学报, 2010, 26(12): 153-160.
    Yuan Junji, Peng Sili, Jiang Xianjun, Xie Deti. Effects of combing ridge and no-tillage on aggregates and organic matter in a rice-based cropping system[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2010, 26(12): 153-160.
    Citation: Yuan Junji, Peng Sili, Jiang Xianjun, Xie Deti. Effects of combing ridge and no-tillage on aggregates and organic matter in a rice-based cropping system[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2010, 26(12): 153-160.

    稻田垄作免耕对土壤团聚体和有机质的影响

    Effects of combing ridge and no-tillage on aggregates and organic matter in a rice-based cropping system

    • 摘要: 该文以1990年建立的耕作制定位试验田紫色水稻土为研究对象,分析了冬水田(FPF)、水旱轮作(CR)和垄作免耕(RNT)3种耕作方式对土壤团聚体组成和有机质的影响。结果表明,垄作免耕减少了对土壤大团聚体的破坏,在0~10 cm土层,垄作免耕大团聚体含量分别是冬水田和水旱轮作的1.48和1.32倍,微团聚体含量则显著降低;在 >10~20 cm土层有相同的趋势。3种耕作条件下,有机碳和氮在团聚体中的分布模式类似,均有向大团聚体富集的趋势,但垄作免耕条件下土壤有机碳和氮质量分数显著高于冬水田和水旱轮作。对土壤颗粒有机质(POM)的分析结果表明,垄作免耕0~10 cm土层轻质组分(LF)的质量分数(1.92 g/kg)与水旱轮作(1.70 g/kg)差异不显著,但显著高于冬水田(1.42 g/kg)。冬水田、水旱轮作和垄作免耕的0~10 cm土层,团聚体内总颗粒有机质(total iPOM)质量分数分别为0.96,1.12,2.14 g/kg;垄作免耕土壤团聚体内细颗粒有机质(fine iPOM)分别为冬水田和水旱轮作土壤的3.02和2.46倍,占总POM差异的57%和66%。垄作免耕土壤团聚体内粗颗粒有机质(coarse iPOM)分别为冬水田和水旱轮作土壤的1.56和1.40倍,占总POM差异的18%和19%。在>10~20 cm土层有相似的趋势,但在>10~20 cm层土壤粗iPOM的差异对总POM差异的贡献较0~10 cm层大。垄作免耕减少了对大团聚体的破坏并促进微团聚体向大团聚体团聚;降低了团聚体的周转速率,促进了细iPOM的固定,利于紫色水稻土对碳的固定和积累。

       

      Abstract: In this study the effects of tillage methods (flooded paddy field, FPF; conventional paddy-upland rotation tillage, CR; combing ridge with no-tillage, RNT) on soil aggregates as well as on the soil organic matter (SOM) fractions protected by soil aggregates were investigated in a long-term experimental site established in 1990, Chongqing City, China. The results showed that compared with FPF and CR, RNT reduced the disruption of macro-aggregates. In 0–10 cm layer, the content of macro-aggregates in RNT was 1.48 and 1.32 times greater than that in FPF and CR, respectively, while the content of micro-aggregates decreased in RNT, and there was a similar trend in >10–20 cm layer. Under these three tillage methods, the distribution pattern of soil organic carbon (SOC) and soil organic nitrogen (SON) in aggregates were similar, and both of them had an enrichment trend to macro-aggregates, but concentration of SOC and SON was significantly higher under RNT than that in FPF and CR. The results of particulate organic matter (POM) showed that the amount of light fraction (LF) had no significant difference between RNT (1.92 g/kg) and CR (1.70 g/kg), but they were both higher than that in FPF (1.42 g/kg). Total intro-particulate organic matter (iPOM) concentration in FPF, CR, and RNT was 0.96, 1.12, and 2.14 g/kg, respectively. The level of fine iPOM in RNT was 3.06 and 2.46 times greater than that in FPF and CR, which accounted for 57% of the difference in total POM between RNT and FPF (66%, CR). The amount of coarse iPOM was only 1.56 and 1.40 times greater than that in FPF and CR, which accounted for only 18% and 19% of the difference in total POM. Though there was a similar trend in >10–20 cm layer, the difference of coarse iPOM held more share of the difference in total POM than that in 0–10 cm layer. In conclusion, RNT reduced macro-aggregates breakdown, and improved the formation of aggregates from micro-aggregates, which decreased the turnover rate of soil aggregates, favored the sequestration of fine iPOM and promoted the purple paddy soil ability to fix and accumulate carbon.

       

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