人工恢复黄河三角洲湿地土壤碳氮含量变化特征
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人事部博士后基金资助项目(200902569; 20070421082);山东省自然科学基金项目(ZR2009DM028);水体污染控制与治理重大专项(2009ZX07212-003);济南市软科学项目(200817057)


Change characteristics of soil carbon and nitrogen contents in the Yellow River Delta soil after artificial restoration
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    摘要:

    为阐明湿地恢复对土壤碳氮含量的影响,以黄河三角洲芦苇湿地为研究对象,比较了退化区与连续淡水恢复区土壤pH值、盐分、有机碳、全氮、氨态氮、硝态氮的含量变化,研究结果表明,(1)随着恢复年限的增加,各样地各层土壤pH值总体上降低,电导率显著降低(P < 0.05),表明退化湿地的人工恢复可明显降低其盐度;恢复区上层(0-20cm)土壤盐分均低于下层(20-40cm),未恢复区则相反;(2)随着恢复年限的增加,0-20cm土壤有机碳、全氮含量增加,分别由恢复前的(7.710±0.756)g/kg、(0.66±0.021)g/kg增加到恢复7a后的(16.96±0.213)g/kg、(1.277±0.027)g/kg,恢复区有机碳、全氮含量在空间上的变化表现为上层大于下层;(3)各样地硝态氮含量均低于氨态氮含量,碳氮比值介于4-8之间;(4)相关分析表明,湿地恢复后土壤各因子间有显著的相关性,有机碳与全氮两者显著正相关,氨态氮与pH、盐分、有机碳、全氮均达到极显著正相关关系(P < 0.01)。该研究结果对于评估湿地恢复效应,指导湿地恢复的实践具有重要作用。

    Abstract:

    The Yellow River Delta wetland is the largest wetland ecosystem in the warm temperate zone of China and it is one of the most active regions of land-ocean interaction among the large river deltas in the world.. To restore the degraded wetlands in the Yellow River Delta, freshwater was supplied during the flood season from June to July. In order to explore the effect of wetlands restoration on the soil organic carbon and nitrogen, the changes of pH value, electricity conductivity, soil organic carbon (SOC), total nitrogen (TN), NH4+-N and NO3--N in the degraded and restored reed wetlands of Yellow River Delta were anlysed. The results showed that: (1) pH values generally decreased in the two soil layers and the electrical conductivity significantly declined (P<0.05) with the increasing practice time. It indicated that providing freshwater reduced the salt obviously. Soil electricity conductivity in the lower soil layer (20-40cm) was lower than upper soil layer (0-20cm) in restored area. But it is the opposite trend in degraded sites comparing to the restored sites. (2) The SOC and TN in the 0-20cm soil layer increased with recovery time. The SOC and TN were (7.710±0.756) g/kg, (0.66±0.021) g/kg and (16.96±0.213) g/kg, (1.277±0.027) g/kg before and after seven years artificial restoration, respectively. The upper soil layer (0-20cm) had more SOC and TN than the lower soil layer (20-40cm) in the restored sites. But the concentrations of SOC and TN had no significant change (P > 0.05) in the two soil depth in degraded sites. (3) The NH4+-N was higher than NO3--N in all sample sites. The concentrations of NO3--N in 3 years restored sites and NH4+-N in 5 years restored sites was obviously lower than that in the degraded area (P<0.01). The ratios of C/N were between 4 and 8, suggesting that N concentration was not limiting soil decomposition rates. (4) Meanwhile, the correlation analysis showed that there were significant correlations among soil properties. SOC had significantly positive correlation with TN (r=0.947, P < 0.01). It suggested that the N was from the soil organic matter (SOM). The soil C ∶ N was significantly correlated with SOM. The significant positive correlations between NH4+-N and pH value, electricity conductivity, SOC, TN were also found (P<0.01), while NO3--N and TN having negative correlations (P<0.05). The research provide base information for the evaluation of wetlands restoration and the degraded wetlands restoration practice. But further studies are needed to determine long-term changes in soil processes within the wetlands in the Yellow River Delta.

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董凯凯,王惠,杨丽原,杨宝山,解伏菊.人工恢复黄河三角洲湿地土壤碳氮含量变化特征.生态学报,2011,31(16):4778~4782

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