植物生态学报 ›› 2002, Vol. 26 ›› Issue (6): 689-694.

• 论文 • 上一篇    下一篇

西双版纳热带季节雨林生态系统氮的生物地球化学循环研究

沙丽清,郑征,冯志立,刘玉洪,刘文杰,孟盈,李明锐   

  • 发布日期:2002-06-10
  • 通讯作者: 沙丽清

Biogeochemical Cycling of Nitrogen at a Tropical Seasonal Rain Forest in Xishuangbanna, Sw China

SHA Li-Qing, ZHENG Zheng, FENG Zhi-Li, LIU Yu-Hong, LIU Wen-Jie, MENG Ying, and LI Ming-Rui   

  • Published:2002-06-10
  • Contact: SHA Li-Qing

摘要: 用小流域集水区和物质平衡方法,于1999年对西双版纳热带季节雨林生态系统的氮素循环进行了初步研究。西双版纳季节雨林生态系统的氮库总储量为6 481.2 kg·hm-2,其中活体生物量、凋落物层和土壤(0~30 cm)中的氮储量分别为970.9、37.7、5 481.2 kg·hm-2。土壤中的氮占生态系统氮总储量的84.4%,活体生物量占15.0%,凋落物层仅占0.6%。结果表明季节雨林的氮主要分布在土壤中,而在生物量中只占很少部分。大气降水、林内穿透水、树干流及地表径流的氮含量分别为0.565、0.828、0.983和1.042 mg·dm-3,氮通量则分别为8.89、10.97、3.57、5.95 kg·hm-2·a-1。大气降水输入氮8.89 kg·hm-2·a-1,径流输出氮5.95 kg·hm-2·a-1, 收支平衡(输入—输出)为2.94 kg·hm-2·a-1。氮的生物循环:吸收为149.86 kg·hm-2·a-1,存留为69.30 kg·hm-2·a-1,归还为80.56 kg·hm-2·a-1,循环系数为0.54。结果表明未受干扰的季节雨林生态系统处于氮积累的状态,有利于该生态系统的稳定与持续发展。

Abstract: Xishuangbanna, located in southwest China, bounded by Laos and Myanmar on the upper Mekong River, is on the northernmost edge of tropical Asia. As a result, a mosaic distribution of tropical seasonal rain forest, which mainly appears in the wet valleys, usually with small streams or on the low hills and flats below 1000 m altitude exists in Xishuangbanna. The tropical seasonal rain forest in Xishuangbanna is rich in species and has a complex forest canopy and structure. In 1999, 119 species with DBH>10 cm were recorded in the 1 hm2 study plot. Based on the “small catchment” approach and input-output budgets, we studied on the nitrogen cycling in the seasonal rain forest. The nitrogen stock in the seasonal rain forest ecosystem (6 481.2 kg·hm-2) was higher than that of montane rain forest in Hainan of China (6 345 kg·hm-2), but lower than montane rain forest in New Guinea (20 190 kg·hm-2), lowland rain forest in Brazil (7 537 kg·hm-2), and lowland rain forest in Ghana (7 230 kg·hm-2). The distribution of the nitrogen stock in the seasonal rain forest ecosystem is as follows: 970.9 kg·hm-2 (15.0%) in the living biomass, 37.7 kg· hm-2 (0.6%) in the forest floor, and 5 481.2 kg·hm-2 (84.4%) in the soil (0-30 cm). We found that most of the nitrogen in the seasonal rain forest was stored in the soil, but not in the living biomass. Soil (0-10 cm) net nitrogen mineralization rate was 90.4 kg·hm-2·a-1. Soil played a very important role of stocking and providing N to plants. The nitrogen content in precipitation, throughfall, stemflow and stream flow were 0.565, 0.828, 0.983 and 1.042 mg·dm-3, respectively. The nitrogen input from precipitation, throughfall and stemflow were 8.89, 10.97 and 3.57 kg·hm-2·a-1, respectively. The nitrogen output in stream flow was 5.95 kg·hm-2·a-1. The nitrogen net increase in the seasonal rain forest was 2.94 kg·hm-2·a-1. In the nitrogen biological cycling, 149.86 kg·hm-2·a-1 was taken up by plants,69.30 kg·hm-2·a-1 stored in living biomass,and 80.56 kg·hm-2·a-1 returned to soil. This undisturbed seasonal rain forest had the nitrogen conservation mechanism and remained in the nitrogen accumulation state.