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环境科学与地理学

城市河岸带夏季土壤表层温度的多时间尺度特征及其影响因素

  • 郑潇柔 ,
  • 张娜
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  • 中国科学院大学资源与环境学院, 北京 101408

收稿日期: 2016-01-14

  网络出版日期: 2016-11-15

基金资助

北京市自然科学基金(8132045)和中国科学院知识创新工程重要方向项目(Y225016EA2)资助

Variation in top soil temperature on multiple temporal scales and its influencing factors for an urban riparian zone in summer

  • ZHENG Xiaorou ,
  • ZHANG Na
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  • College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 101408, China

Received date: 2016-01-14

  Online published: 2016-11-15

摘要

探讨城市河岸带夏季土壤表层5 cm温度(以下简称土温)的多时间尺度变化,并据此分析影响不同时间尺度域内土温发生波动的因素.小波分析结果表明,土温可在多个时间尺度域上变化,具有5个时间特征尺度.土温在日、旬和两旬尺度上的波动主要受总太阳辐射量变化的影响;在月和季节尺度上的波动主要受下垫面植被配置的影响.其中,在月和季节尺度上,地上植物生长状况对土温的影响较大,且不同植被类型(针叶大乔木、阔叶小乔木、阔叶大乔木和草灌植物)的草灌层覆盖度和高度及乔木层叶生物量对土温变化的影响程度不尽相同.植被类型和冠层结构对土温变化也有一定影响:冠层株型为圆锥形的针叶乔木下的土温显著低于株型为球形的阔叶乔木下的土温.另外,相比阔叶乔木,针叶乔木的降温效应更为明显:当针叶乔木下的草灌层覆盖度达到30%时,表现出明显的降温效应;而对于阔叶乔木,覆盖度需达到60%.

本文引用格式

郑潇柔 , 张娜 . 城市河岸带夏季土壤表层温度的多时间尺度特征及其影响因素[J]. 中国科学院大学学报, 2016 , 33(6) : 758 -768 . DOI: 10.7523/j.issn.2095-6134.2016.06.007

Abstract

This study investigated the variation in the soil temperature in the top 5 cm of the soil on multiple temporal scales and its driving factors for an urban riparian zone in summer. Wavelet analysis showed that the top soil temperature varied within multiple domains of temporal scale. The variation in the top soil temperature on small temporal scales (daily, ten-day, and twenty-day) was mainly due to the variation in total solar radiation, while on large temporal scales (monthly and seasonal) it was mainly influenced by vegetation composition and configuration. Firstly, plant growth had significant effects on top soil temperature. Vegetation coverage and height and tree leaf biomass played different roles in variation in the top soil temperature when vegetation types were different. Secondly, the top soil temperature was also influenced by vegetation type and canopy structure as vegetation coverages were similar. In addition, compared with the broad-leaved trees, the coniferous trees had more noticeable cooling effect.

参考文献

[1] Lowrance R, Altier L S, Newbold J D, et al. Water quality functions of riparian forest buffers in Chesapeake Bay watersheds[J]. Environmental Management, 1997, 21(5):687-712.
[2] Osborne L L, Kovacic D A. Riparian vegetated buffer strips in water-quality restoration and stream management[J]. Freshwater Biology, 1993, 29(29):243-258.
[3] 李婉, 张娜, 吴芳芳. 北京转河河岸带生态修复对河流水质的影响[J]. 环境科学, 2011, 32(1):80-87.
[4] 吴芳芳, 张娜, 陈晓燕. 北京北护城河河岸带的温湿度调节效应[J].生态学报, 2013, 33(7):2292-2303.
[5] Collier K J, Smith B J. Interactions of adult stoneflies (Plecoptera) with riparian zones. I. Effects of air temperature and humidity on longevity[J]. Aquatic Insects, 2000, 22(4):275-284.
[6] 宋长春, 王毅勇. 湿地生态系统土壤温度对气温的响应特征及对CO2排放的影响[J]. 应用生态学报, 2006, 17(4):625-629.
[7] Walker J M. One-degree increments in soil temperatures affect maize seedling behavior[J]. Soil Science Society of America Proceedings, 1969, 33(5):729-736.
[8] 冯玉龙, 孙国斌. 根系温度对植物的影响(Ⅰ):根温对植物生长及光合作用的影响[J]. 东北林业大学学报, 1995, 23(3):63-69.
[9] 冯玉龙, 刘恩举, 孟庆超. 根系温度对植物的影响(Ⅱ):根温对植物代谢的影响[J]. 东北林业大学学报, 1995, 23(4):94-99.
[10] 斯迪. 土温与气温[J]. 农村实用科技信息, 1999, 4(5):8.
[11] Jackson T, Mansfield K, Saafi M, et al. Measuring soil temperature and moisture using wireless MEMS sensors[J]. Measurement, 2008, 41(4):381-390.
[12] Lal R, Shukla M K. Principles of soil physics[M]. New York:Principles of Soil Physics, 2004.
[13] 邵明安, 王全九, 黄明斌. 土壤物理学[M]. 北京:高等教育出版社, 2006.
[14] Paul K I, Polglase P J, Smethurst P J, et al. Soil temperature under forests:a simple model for predicting soil temperature under a range of forest types[J]. Agricultural & Forest Meteorology, 2004, 121(3/4):167-182.
[15] Tabari H, Sabziparvar A A, Ahmadi M. Comparison of artificial neural network and multivariate linear regression methods for estimation of daily soil temperature in an arid region[J]. Meteorology & Atmospheric Physics, 2011, 110(3/4):135-142.
[16] 朱文星, 邓卓智. 简述永定河城市段的生态修复[J]. 水利科技与经济, 2012, 18(2):19-21.
[17] 罗天祥. 中国主要森林类型生物生产力格局及其数学模型[D]. 北京:中国科学院自然资源综合考察委员会, 1996.
[18] 陈灵芝, 任继凯, 鲍显诚,等. 北京西山(卧佛寺附近)人工油松林群落学特性及生物量的研究[J]. 植物生态学与地植物学丛刊, 1984, 8(3):173-181.
[19] 张娜. 景观生态学[M]. 北京:科学出版社, 2014.
[20] 张娜. 生态学中的尺度问题:内涵与分析方法[J]. 生态学报, 2006, 26(7):2340-2355.
[21] 任惠茹, 李国胜, 崔林林,等. 近60年来黄河入海水沙通量变化的阶段性与多尺度特征[J]. 地理学报, 2014, 69(5):619-631.
[22] 吴创收, 杨世伦, 黄世昌,等. 1954-2011年间珠江入海水沙通量变化的多尺度分析[J]. 地理学报, 2014, 69(3):422-432.
[23] 姚俊强, 刘志辉, 杨青, 等. 近130年来中亚干旱区典型流域气温变化及其影响因子[J]. 地理学报, 2014, 69(3):291-302.
[24] 尤卫红. 气候变化的多尺度诊断分析和预测的多种技术方法研究[M]. 北京:气象出版社, 1998.
[25] 张小飞, 王仰麟, 吴健生, 等. 城市地域地表温度-植被覆盖定量关系分析:以深圳市为例[J]. 地理研究, 2006, 25(3):369-377.
[26] 张娜, 赵英时. 植株冠层几何形状对草地反射率的影响[J]. 遥感学报, 2007, 11(1):9-19.

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