离子交换树脂法在天童森林内外氮素湿沉降观测中的应用

李丹丹; 苏渝钦; 周陶冶; 郑泽梅; 王希华

doi:10.3969/j.issn.1000-5641.2015.06.015

离子交换树脂法在天童森林内外氮素湿沉降观测中的应用

doi: 10.3969/j.issn.1000-5641.2015.06.015

李丹丹^1,2,
苏渝钦^1,2,
周陶冶^1,3,
郑泽梅^1,2, ,,
王希华^1,2

1.
华东师范大学生态与环境科学学院,上海200241;
2.
华东师范大学浙江天童森林生态系统国家野外科学观测研究站,上海200241;
3.
华东师范大学生态与环境科学学院上海市城市化生态过程与恢复重点实验室, 上海200241

详细信息

通讯作者:
郑泽梅，女，副研究员，硕士生导师，研究方向森林碳氮循环与全球变化.

中图分类号: Ｘ５１７
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出版历程
- 收稿日期: 2014-10-16
- 刊出日期: 2015-11-25

Application of ionexchange resin method on the observation of wet nitrogen deposition fluxes inside and outside Tiantong forest

LI Dan-Dan^1,2,
SU Yu-Qin^1,2,
ZHOU Tao-Ye^1,3,
ZHENG Ze-Mei^{1,2
, ,},
WANG Xi-Hua^1,2

摘要

摘要: 为了解天童地区森林内外氮素湿沉降的组分分配及其季节动态特征，基于离子交换树脂法对其森林内外氮素湿沉降量进行了为期2年（2011年3月至2013年2月）的观测.研究发现：（1）天童森林内外硝态氮沉降月总量分别在0.22~3.73 kgN/(hm2月)和0.13~2.85 kgN/(hm2月)之间波动，均呈现出秋冬季较高、夏季较低的季节动态特征；森林内外铵态氮沉降月总量在0.17~1.35 kgN/(hm2月)和0.21~1.44 kgN/(hm2月)之间波动，春季沉降量略低于其他季节；（2）天童森林内外氮素湿沉降量的季节动态受到研究区域所属季风气候、夏季台风和农事活动的综合影响；（3）森林内外硝态氮与铵态氮沉降量比例的年平均值均为0.9，表明化石燃料燃烧与农事活动对本地区氮素湿沉降的影响相当；（4）天童森林内外氮素湿沉降年总量分别为18.86 kgN/(hm2年) 和17.51 kgN/(hm2年)，氮素湿沉降年总量符合中国东部森林氮沉降量由北向南逐渐增加的趋势.
- 氮沉降 /
- 离子交换树脂法 /
- 天童 /
- 森林
Abstract: The fluxes of wet nitrogen deposition inside and outside Tiantong forest were observed for 2 years (from March 2011 to February 2013), basing on Ionexchange resin method, to examine the composition and the seasonal dynamics of wet nitrogen deposition in Tiantong forest. The results showed that: (1) The monthly fluxes of nitrate nitrogen inside and outside forest were 0.22~3.73 kgN/(hm2month) and 0.13~2.85 kgN/(hm2month), respectively, which both had higher fluxes in autumn and winter, while lower fluxes in summer. The 〖JP3〗monthly fluxes of ammonium nitrogen inside and outside forest were 0.17~1.35 kgN/(hm2month) 〖JP〗and 0.21~1.44 kgN/(hm2month), respectively. The monthly fluxes of ammonium nitrogen were lower in spring than in other seasons. (2)The nitrate nitrogen deposition fluxes were lower than ammonium nitrogen deposition fluxes in spring and summer, while higher in autumn and winter. Moreover, the average ratio of nitrate nitrogen to ammonium nitrogen was 0.9, whatever inside and outside forest. (3) The wet nitrogen deposition fluxes were higher in autumn and winter inside and outside forest, respectively, resulted from the influences of monsoon climate, typhoons in summer and the farming activities in Tiantong region.(4) The annual wet nitrogen deposition fluxes inside and outside forest were 18.86 kgN/(hm2a) and 17.51 kgN/(hm2a), respectively.
- nitrogen depositionionexchange resin methodTiantongforest /

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