[1]敬文茂,牛 赟,刘贤德*,等.祁连山大野口流域土壤温度空间变化特征[J].山地学报,2016,(02):142-149.[doi:10.16089/j.cnki.1008-2786.000111]
 JING Wenmao,NIU Yun,LIU Xiande,et al.Spatial Variation Characteristics of Soil Temperature in Dayekou Basin of Qilian Mountains[J].Mountain Research,2016,(02):142-149.[doi:10.16089/j.cnki.1008-2786.000111]
点击复制

祁连山大野口流域土壤温度空间变化特征()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2016年02期
页码:
142-149
栏目:
山地生态与环境
出版日期:
2016-04-01

文章信息/Info

Title:
Spatial Variation Characteristics of Soil Temperature in Dayekou Basin of Qilian Mountains
作者:
敬文茂1牛 赟123刘贤德12*李 新3吕一河4
1.甘肃省祁连山水源涵养林研究院 甘肃省森林生态与冻土水文水资源重点实验室,甘肃 张掖 734000; 2.中国科学院寒区旱区环境与工程研究所,甘肃 兰州 730000; 3.甘肃张掖生态科学研究院 甘肃省祁连山生态科技创新服务平台,甘肃 张掖 734000; 4.中国科学院生态环境研究中心,北京 100085
Author(s):
JING Wenmao1NIU Yun 1 23LIU Xiande 13LI Xin2Lü Yihe4
1.Academy of Water Resource Conservation Forests of Qilian Mountains in Gansu Province, Gansu Province Key Laboratory of Forest Ecology and Frozen-soil Hydrology and Water Resources, Zhangye 734000, Gansu, China; 2.Cold And Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou 730000,China; 3.Academy of Ecology Science of Zhangye, Gansu Science and Technology Innovation Service Platform of Ecology in Qilian Mountains,Gansu Province, Zhangye 734000, Gansu, China; 4.Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences,Beijing 100085,China
关键词:
土壤温度 空间变化 祁连山大野口流域
分类号:
S152.8
DOI:
10.16089/j.cnki.1008-2786.000111
文献标志码:
A
摘要:
选择祁连山大野口为试验流域,研究土壤温度在海拔、坡向、坡度、深度等空间的变化特征。结果表明:1.土壤温度随海拔升高呈波动性降低,降低率约为0.74 ℃/(100 m); 2.阳坡土壤温度比半阳坡高1.3倍、比半阴坡高2.2倍,半阳坡土壤温度比半阴坡高1.6倍; 3.土壤温度随坡度增大而略呈降低趋势; 4.土壤温度与深度关系为Sdt=-0.0536d+9.192(R2=0.994),温度随深度降低率约为0.536 ℃/(10 cm),呈线性函数关系; 5.亚高山灌丛林比乔木林土壤温度低1.6倍、比草地低2.3倍,乔木林土壤温度比草地低1.4倍; 6.从土壤温度的变化程度分析,高海拔半阴坡灌丛林土壤温度变化最剧烈,低海拔阳坡草地土壤温度变化较小; 在0~80 cm土层范围内,表层土壤温度变化最剧烈,40~60 cm土层的温度变化最小。研究可为流域水源涵养功能、水资源管理及利用、林分结构调控及土壤水资源植被承载力等研究提供基础数据和参考资料。

参考文献/References:

[1] Toy T J, Kuhaida A J. Munson B E. The prediction of mean monthly soil temperature from mean monthly air temperature[J]. Soil Science, 1978, 126(3):181-189
[2] Meikle R W,Treadway T R. A mathematical method for estimating soil temperature in Canada [J]. Soil Science, 1981, 131(5):320-326
[3] 杨学明.土壤水热状况与土壤系统分类[J].土壤,1988,21(2 ):110-113[Yang Xueming. Soil moisture and temperature regimes and soil taxonomy [J].Soils, 1988, 21(2):110-113]
[4] 冯学民,蔡德利.土壤温度与气温及纬度和海拔关系的研究,土壤学报,2004,41(3):489-491[Feng Xueming, Cai Deli. Soil temperature in related to air temperature, altitude and latitude[J].Acta Pedologica Sinica,2004,41(3):489-491]
[5] 张慧智,史学正,于东升,等.中国土壤温度的空间插值方法比较[J].地理研究,2008,27(6): 1299-1307[Zhang Huizhi,Shi Xuezheng, Yu Dongsheng. Spatial prediction of soil temperatures in China using different method [J].Geographical Research,2008,27(6): 1299-1 307]
[6] 牛赟,刘贤德,敬文茂,等.祁连山排露沟流域气温、冻土冻融与河川径流特征[J].林业科学, 2014, 50(1):27-31[Niu Yun, Liu Xiande,Jing Wenmao. et al. Characteristics of temperature,soil freezing and thawing, and river flow in Pailugou watershed of Qilian Mountains[J].Scientia Silvae Sinicae, 2014, 50(1):27-31]
[7] 罗龙发,牛赟,王艺林, 等. 祁连山青海云杉林温度变化对土壤呼吸的影响[J]. 林业科学,2007,10:117-121[Luo Longfa,Niu Yun, Wang Yilin, et al. The soil respiration influenced on change of temperature in of Picea crassifolia forest of Qilian Mountains[J]. Scientia Silvae Sinicae, 2007,10:117-121]
[8] 祁连山林草复合流域气象因子、土壤特性及其蒸发对比研究[J].中南林业科技大学学报,2014,34(10):90-94[Niu Y, Niu Y, Jing W M, et al.Comparative study on woodland and meadow of meteorological factors, soil properties and its evaporation in composite basin of Qilian mountains[J].Journal of Central South University of Forestry and Technology,2014,34(10): 90-94]
[9] 唐振兴,何志斌,刘鹄. 祁连山中段林草交错带土壤水热特征及其对气象要素的响应[J]. 生态学报,2012,32(4): 32(4):1056-1065[Tang Zhenxing, He Zhibin, Liu Hu. Soil moisture and temperature character is tics of forest-grassland ecotone in middle Qil ian Mountains and the responses to meteorological factors. Act a Ecological Sinica,2012,32(4):1056-1065]
[10] 刘贤德,牛赟,敬文茂,等.祁连山森林内外主要气象因子对比研究[J]. 干旱区地理,2009,32(1):32-36[Liu Xiande,Niu Yun, Jing Wenmao, et al. Comparison of principal meteorology factors inside & outside forest in Qilian Mountains[J].Arid land Geography, 2009,32(1):32-36]
[11] 王金叶,常学向,葛双兰.祁连山(北坡)水热状况与植被垂直分布[J].西北林学院学报, 2001,16(增): 1-3[Wang Jinye, Zhang Xuexiang, Ge Shuanglan, et al. Vertical distribution of the vegetation and water and heat conditions of Qilian mountain(northern slope)[J]. Journal of Northwest Forestry College, 2001,16(Suppl.):1-3]
[12] 王谨,温娅丽,刘思瑞,等.祁连山大野口流域青海云杉林苔藓枯落物及其土壤水热特征分析,甘肃农业大学学报[J]. 2014(6):107-113[Wang Jin, WEN Yali, Liu Shirei. et al.Feature analysis on water and temperature of moss litter and soil of Picea crassifolia in Dayekou basin of Qilian Mountains[J].Journal of Gansu Agricultural University, 2014(6):107-113]
[13] 牛赟,刘贤德,敬文茂,等.祁连山北坡气候梯度变化对比研究[J].甘肃农业大学学报, 2013,48(2):86-91[Niu Yun, Liu Xiande, Jing Wenmao, et al. Comparative study on climate gradient changes in the north slope of Qilian mountains [J]. Journal of Gansu Agricultural University, 2013,48(2):86-91]

相似文献/References:

[1]花可可,王小国,朱波,等.紫色土旱坡地土壤异养呼吸速率及其温度敏感性[J].山地学报,2013,(05):548.
 HUA Keke,WANG Xiaoguo,ZHU Bo.Soil Heterotrophic Respiration Rate and Its Sensitivity to Temperature on Sloping Upland of Purple Soil[J].Mountain Research,2013,(02):548.
[2]杨忠,刘国凡,邓廷秀.马桑根瘤的固氮活性与呼吸强度[J].山地学报,1993,(04):261.
[3]张建辉,唐时嘉.四川盆地紫色土温度状况的确定[J].山地学报,1995,(02):98.
[4]杨梅学,姚檀栋,何元庆,等.藏北高原D110点土壤温度的极值分析[J].山地学报,1999,(03):16.
[5]杨梅学,姚檀栋,小池俊雄.藏北高原土壤温度分布的纬向效应和高度效应[J].山地学报,1999,(04):329.
[6]杨梅学,姚檀栋,ToshioKOIKE.藏北高原土壤温度的变化特征[J].山地学报,2000,(01):13.
[7]王建雷,李英年,杜明远,等.祁连山冷龙岭南坡小气候及植被分布特征[J].山地学报,2009,(04):418.
[8]胡启武,吴琴,郑林,等.青海云杉叶片稳定性碳同位素组成对水分温度变化的响应[J].山地学报,2010,(06):712.

备注/Memo

备注/Memo:
收稿日期(Received date):2015-09-11; 改回日期(Accepted): 2016-01-02。基金项目(Foundation item):由国家自然科学基金项目《祁连山大野口流域水源涵养功能生态水文关系分析》(41461004)、甘肃省基础研究创新群体《祁连山土壤水源涵养功能与森林分布变化响应关系》(145RJIG337)、甘肃省科技创新服务平台《甘肃省祁连山生态科技创新服务平台》(144JTCG254 )联合资助。作者简介(Biography):敬文茂(1976-),男,甘肃榆中人,硕士,主要从事森林生态水文学方面的研究。[Jing Wenmao(1976-),male,Gansu Lanzhou person,master,mainly engaged in study of forest ecological hydrology.] E-mail:maodanjing@126.com,Tel:13993683930
更新日期/Last Update: 1900-01-01