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沙地樟子松人工林土壤磷素转化的根际效应
引用本文:赵琼,曾德慧,于占源,邓斌,范志平.沙地樟子松人工林土壤磷素转化的根际效应[J].应用生态学报,2006,17(8):1377-1381.
作者姓名:赵琼  曾德慧  于占源  邓斌  范志平
作者单位:1. 中国科学院沈阳应用生态研究所大青沟沙地生态实验站,沈阳,110016;中国科学院研究生院,北京,100039
2. 中国科学院沈阳应用生态研究所大青沟沙地生态实验站,沈阳,110016
基金项目:国家自然科学基金;中国科学院知识创新工程项目;中国科学院前沿领域研究基金
摘    要:对大青沟自然保护区内不同年龄樟子松人工林根际和非根际土壤中不同形态磷素含量和酸性磷酸单酯酶(AP)活性进行了比较.结果表明,樟子松根系活动显著地提高了根际土壤有机碳含量及有机质的C/P比,增强了土壤微生物活动和AP活性,促进了有机磷的可利用性与矿化;显著地降低了土壤pH值,促进了Ca-P的溶解;从而提高了土壤磷素的有效性,促进了有机磷和Ca-P向Fe-P、Al-P的转化.与AP活性的根际效应相反,随林龄增加,樟子松对各形态磷素的根际效应逐渐增强,根际和非根际土壤中各形态磷素的变化趋势基本一致,土壤全磷和有机磷含量逐渐下降,而活性磷含量升高.为了保持土壤有机磷库和磷素的持续供应,必须对地被物予以保护.

关 键 词:樟子松人工林  根际效应  有机磷矿化  土壤酸化  磷素有效性
文章编号:1001-9332(2006)08-1377-05
收稿时间:2005-08-22
修稿时间:2006-06-06

Rhizosphere effects of Pinus sylvestris var. mongolica on soil phosphorus transformation
ZHAO Qiong,ZENG Dehui,YU Zhanyuan,DENG Bin,FAN Zhiping.Rhizosphere effects of Pinus sylvestris var. mongolica on soil phosphorus transformation[J].Chinese Journal of Applied Ecology,2006,17(8):1377-1381.
Authors:ZHAO Qiong  ZENG Dehui  YU Zhanyuan  DENG Bin  FAN Zhiping
Institution:1 Daqmggou Ecological Station , Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100039, China
Abstract:To understand the phosphorus (P) mobilization mechanism of Mongolian pine (Pinus sylvestris var. mongolica) on a P-deficient semi-arid sandy soil of northern China, this paper compared the P fractions and acid phosphomonoesterase (AP) activity in the bulk and rhizosphere soils under different age Mongolian pine plantations. The results showed that when compared with the bulk soil, the organic C, labile organic P, and organic C/P ratio increased significantly, microbial and AP activities improved, and organic P mineralization accelerated in the rhizosphere soil. Root activity of the Mongolian pine significantly increased the bioavailability of soil P, and accelerated the shift of organic P and Ca-P to Fe-P and Al-P. The rhizosphere effects on soil P in different forms enhanced with stand age, whereas in adverse on AP activity. The bulk and rhizosphere soil had the similar trend in the dynamics of its P fractions with stand age. Soil total P pool reduced gradually while labile P pool increased with stand age. It should be essential to protect forest floor to replenish soil P pool and guarantee a long-term soil P supply.
Keywords:Mongolian pine plantation  Rhizosphere effects  Mineralization of organic phosphorus  Soil acidification  Soil phosphorus bioavailability  
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