杉木林土壤碳氮磷储量及化学计量特征对氮添加的响应

Responses of stocks and stoichiometric characteristics of soil carbon, nitrogen and phosphorus to nitrogen addition in a Cunninghamia lanceolata plantation

  • 摘要: 以亚热带杉木(Cunninghamia lanceolata)人工林为研究对象,设计对照(N0,0 kg·hm−2·a−1)、低氮(N1,60 kg·hm−2·a−1)、中氮(N2,120 kg·hm−2·a−1)和高氮(N3,240 kg·hm−2·a−1)4种模拟氮沉降处理,探究长期(10 a)氮添加处理后土壤有机碳(SOC)、全氮(TN)和全磷(TP)质量比、储量及化学计量特征的变化. 结果表明氮添加(N1、N2和N3)显著提高了TN质量比和储量,与N0相比TN质量比分别增加17.31%、21.59%和25.01%;TN储量分别增加22.16%、31.64%和39.47%. 氮添加处理对TP质量比和储量影响无明显规律. 氮添加处理下土壤w(C):w(N)(C:N)介于8.29~14.23,w(C):w(P)(C:P)介于54.12~95.17,w(N):w(P)(N:P)介于5.16~8.91,土壤碳、氮、磷储量与土壤化学计量特征有显著相关性,SOC储量与C:N和C:P显著正相关,与N:P显著负相关;TN储量与C:P显著负相关;TP储量与C:P和N:P显著负相关. 研究结果表明长期氮添加后土壤表层碳氮磷储量受土壤化学计量特征调控. 该研究可为氮沉降背景下杉木人工林的可持续经营管理提供一定的科学参考.

     

    Abstract: In this study, four nitrogen (N) addition treatments, i.e., control (N0, 0 kg·hm−2·a−1), low (N1, 60 kg·hm−2·a−1), medium (N2, 120 kg·hm− 2·a−1) and high (N3, 240 kg·hm−2·a−1) were designed to simulate nitrogen deposition in a subtropical Cunninghamia lanceolata plantation. Changes in soil organic carbon (SOC), total nitrogen (TN) and total phosphorus (TP) contents, stocks and their stoichiometric characteristics were investigated after 10-year-long N addition. The results showed that N addition significantly increased the TN content and stock. Compared to control treatment, TN contents in N1, N2 and N3 increased by 17.31%, 21.59% and 25.01%; TN stocks increased by 22.16%, 31.64% and 39.47%, respectively. N addition had no significant effect on TP contents and stocks. Soil C:N under N addition varied from 8.29 to 14.23, C:P ranged from 54.12 to 95.17 and N:P ranged from 5.16 to 8.91. Stocks of soil C, N and P were significantly correlated with soil stoichiometric characteristics. SOC stocks were positively correlated with C:N and C:P and negatively correlated with N:P; TN stocks were negatively correlated with C:P; TP stocks were negatively correlated with C:P and N:P. Our findings suggest that soil surface carbon, nitrogen and phosphorus stocks are regulated by soil stoichiometric characteristics after long-term N addition, and provide a scientific guidance for the forest management in Cunninghamia lanceolata plantations.

     

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