• 中文核心期刊
  • CSCD来源期刊
  • 中国科技核心期刊
  • CA、CABI、ZR收录期刊

武夷山垦荒植茶对表层土壤生态化学计量特征的影响

Ecological Stoichiometry of Surface Soil in Wuyi Mountain Affected by Tea Cultivation

  • 摘要:
    目的 明确垦荒植茶对表层土壤生态化学计量特征的影响。
    方法 在武夷山地区选取种植年限为0~10年、20~30年和40~50年的茶园,分别采集茶园及相邻杂草覆盖空地0~15 cm深度土壤样品。测定土壤的有机碳(soil organic carbon, SOC)、全氮(total nitrogen, TN)、全磷(total phosphorus, TP)和全钾(total potassium, TK)含量,以及土壤的pH值和电导率(electrical conductivity, Ec),并计算土壤的C/N、C/P、C/K、N/P、N/K、P/K比值,以及SOC、TN的库容。
    结果 (1)与相邻空地相比,种植年限为20~30年茶园土壤的SOC含量变化不显著,而0~10年和40~50年茶园土壤的SOC含量分别显著降低了24.55%和30.37%。此外,茶园土壤的TN、TP、TK含量均有不同程度的增加,其中20~30年茶园的土壤TK含量增幅最大,达199.97%。(2)与相邻空地相比,3种种植年限茶园土壤的电导率增幅分别为0、121.72%和73.43%,而土壤pH却分别下降了0.7、0.3和0.4个单位,降幅分别为10.46%,5.52%和7.55%。(3)茶园土壤的C/N、C/P、C/K、N/K以及P/K比值较相邻空地均显著降低,降幅范围为0.76%~56.38%。
    结论 垦荒植茶显著提高表层土壤的全量N、P、K含量,并增加了土壤氮库库容,其中植茶年限为20~30年的茶园提升效果最为显著。然而,垦荒植茶同时导致表层土壤碳库损失,加剧土壤酸化,并降低了土壤生态化学计量值(N/P除外)。

     

    Abstract:
    Objective Fertility and ecological stoichiometric characteristics of surface soil at the land converted for tea cultivation in Wuyi Mountain were studied.
    Methods Surface soil specimens at 0-15cm depth were collected at the plantations with a history of cultivating tea for 0-10, 20-30, and 40-50 years in Wuyi Mountain. For comparison, soil samples were also collected in the weed-covered virgin lands adjacent to the tea plantations. Contents of organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), and total potassium (TK) as well as pH and electrical conductivity (Ec) of the soil samples were determined. C/N, C/P, C/K, N/P, N/P, and reservoir capacity of SOC and TN were calculated.
    Results (1) Compared with neighboring virgin land of each sampling site, the plantation SOC were lower by 24.55-30.37% with significantly reduced reservoir, while the TN, TP, and TK were higher in varying degrees. The surface soil at the 0-10-year-old plantations had the least with no change on TN on average; and at the 20-30-year-old plantations, TK rose the most by 199.97%. (2) The Ec of the 20-30-year-old tea plantation soil was 121.72% higher than that of the neighboring control lots, and that of the 40-50-year-old plantation soil, 73.43% higher. The soil pH of the 0-10-year-old plantations was 0.7 below control with a 10.46% reduction, 0.3 at the 20-30-year-old plantations (5.52% reduction), and 0.4 at the 40-50-year-old plantations (7.55% reduction). (3) The ratios of C/N, C/P, C/K, N/K, and P/K of the plantation soils were significantly lowered ranging from 0.76% to 56.38%.
    Conclusion  Tea cultivation on the mountain lands significantly raised the surface soil TN, TP, TK, and nitrogen storage. The increase was most significant for the 20-30-year-old plantations. Along with it, there was a loss of carbon storage/pools in the soil which exacerbated acidification and induced decline on the ecological stoichiometry (except for N/P).

     

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