| 河西走廊中段荒漠绿洲土壤生态化学计量特征 |
| 摘要点击 1205 全文点击 413 投稿时间：2022-04-20 修订日期：2022-08-19 |
| 查看HTML全文
查看全文 查看/发表评论 下载PDF阅读器 |
| 中文关键词 张掖临泽 荒漠绿洲 荒漠过渡带 生态化学计量 空间异质性 |
| 英文关键词 Zhangye Linze desert oasis desert-oasis transition zone ecological stoichiometry spatial heterogeneity |
| 作者 | 单位 | E-mail | | 孙雪 | 西北师范大学生命科学学院, 微型生物学研究室, 兰州 730070 | 2020212608@nwnu.edu.cn | | 龙永丽 | 西北师范大学生命科学学院, 微型生物学研究室, 兰州 730070 | | | 刘乐 | 西北师范大学生命科学学院, 微型生物学研究室, 兰州 730070 | | | 刘继亮 | 中国科学院西北生态环境资源研究所临泽内陆河流域研究站, 兰州 730000 | | | 金丽琼 | 甘肃省分析测试中心, 兰州 730000 | | | 杜海峰 | 甘肃省陇南生态环境监测中心, 陇南 746000 | | | 陈凌云 | 西北师范大学生命科学学院, 微型生物学研究室, 兰州 730070 | lychen@nwnu.edu.cn |
|
| 中文摘要 |
| 为探究荒漠绿洲土壤C、N、P和K的含量变化及生态化学计量特征,阐明其对环境因子的生态学响应,选择河西走廊中段张掖临泽荒漠绿洲10块样地,采集表层土壤样品,测定土壤C、N、P和K含量,揭示不同生境中土壤养分含量变化和化学计量比的分布特征以及与其他环境因子间的相关关系.结果表明:①土壤C在各样点分布不均匀且具有明显的异质性(R=0.761,P=0.06).其中,ω(C)在绿洲平均值最高,为12.85 g·kg-1,过渡带次之,为8.65 g·kg-1,荒漠最低,为4.1 g·kg-1;②土壤K含量除在盐碱地含量较低外,在荒漠、过渡带和绿洲之间均无显著变化且含量较高;③土壤C ∶N平均值为12.92,C ∶P平均值为11.69,N ∶P平均值为0.9,均低于全球土壤平均水平(13.33、72.0、5.9)和中国土壤平均水平(12、52.7、3.9);④土壤含水量为影响荒漠绿洲土壤C、N、P、K和生态化学计量特征的最大影响因子,贡献率为86.9%,其次为土壤酸碱度和土壤孔隙度,贡献率分别为9.2%和3.9%.研究结果为荒漠和绿洲生态系统的恢复和保护提供基础资料,也为后期研究该地区生物多样性维持机制及其与环境间的相关关系提供科学依据. |
| 英文摘要 |
| To investigate the changes in C, N, P, and K contents and ecological stoichiometry of desert oasis soils and to elucidate their ecological responses to environmental factors, 10 sample plots were selected in the Zhangye Linze desert oasis in the middle part of the Hexi Corridor, and surface soil samples were collected to determine the C, N, P and K contents of soils and to reveal the distribution characteristics of soil nutrient contents and stoichiometric ratios in different habitats and the correlation with other environmental factors. The results showed that:① the distribution of soil carbon was uneven and heterogeneous across sites (R=0.761, P=0.06). The highest mean value was 12.85 g·kg-1 in the oasis, followed by 8.65 g·kg-1 in the transition zone and 4.1 g·kg-1 in the desert. ② The content of total soil potassium did not vary significantly and was high among deserts, transition zones, and oases and low in saline areas. ③ The mean soil C:N value was 12.92, the mean C:P value was 11.69, and the mean N:P value was 0.9, all of which were lower than the global average soil content (13.33, 72.0, and 5.9) and the Chinese soil average (12, 52.7, and 3.9). ④ Soil water content was the most influential factor affecting C, N, P, K, and ecological stoichiometry characteristics of desert oasis soils, with a contribution of 86.9%, followed by soil pH and soil porosity, with contributions of 9.2% and 3.9%, respectively. The results of this study provide basic information for the restoration and conservation of desert and oasis ecosystems and establish a basis for future study of the biodiversity maintenance mechanism in the region and its correlation with the environment. |
|
|
|
