• EI
    • CSA
    • CABI
    • 卓越期刊
    • CA
    • Scopus
    • CSCD
    • 核心期刊

黄土高原典型区沟谷分布谐波分析

卜 楠, 朱清科, 安彦川, 张 岩, 张 青, 秦 伟

卜 楠, 朱清科, 安彦川, 张 岩, 张 青, 秦 伟. 黄土高原典型区沟谷分布谐波分析[J]. 农业工程学报, 2012, 28(11): 225-231.
引用本文: 卜 楠, 朱清科, 安彦川, 张 岩, 张 青, 秦 伟. 黄土高原典型区沟谷分布谐波分析[J]. 农业工程学报, 2012, 28(11): 225-231.
Bu Nan, Zhu Qingke, An Yanchuan, Zhang Yan, Zhang Qing, Qin Wei. Harmonic analysis of valley distribution in typical areas of Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2012, 28(11): 225-231.
Citation: Bu Nan, Zhu Qingke, An Yanchuan, Zhang Yan, Zhang Qing, Qin Wei. Harmonic analysis of valley distribution in typical areas of Loess Plateau[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2012, 28(11): 225-231.

黄土高原典型区沟谷分布谐波分析

基金项目: “十一五”国家科技支撑项目(2006BAD03A03)

Harmonic analysis of valley distribution in typical areas of Loess Plateau

  • 摘要: 为了研究黄土高原地形起伏的周期性,从而探索支沟沟谷分布规律,为黄土高原的土壤侵蚀评估提出新的思路。该文以甘肃西峰、山西吉县、陕西安塞、宁夏固原为研究区尝试利用谐波分析和周期图分析的方法研究黄土高原不同类型区沟谷分布规律。结果表明,黄土高原不同类型区主沟沟谷的周期大小有明显不同,总体来看,高原沟壑区>过度地区>丘陵沟壑区;黄土高原支沟周期主要分布在400~800 m,其周期个数占总周期数的97.5%。对4个研究区的支沟沟谷周期数据进行t检验,结果表明甘肃西峰、陕西安塞、山西吉县相互之间周期均值差异均无显著性(P>0.05);宁夏固原与陕西安塞、山西吉县、甘肃西峰侵蚀支沟分布周期均值双尾检验概率P值均小于0.01,故可认为均值差异极显著。提取不同类型区大于5°坡度的平均坡度分析发现,研究区平均坡度的大小关系为:甘肃西峰>山西吉县>陕西安塞>宁夏固原,支沟沟谷的平均分布周期随平均坡度的增加而不断减小,说明区域平均坡度的大小直接影响着黄土高原支沟的形成。
    Abstract: In order to study the topographic periodicity of the Loess Plateau, and to explore the distribution law of tributary valleys, so as to explore a new method for assessment of the Loess Plateau soil erosion, the paper briefly describes basic principles of harmonic analysis and periodgram analysis. Taking Xifeng in Gansu、Jixian in Shanxi、Ansai in Shaanxi、Guyuan in Ningxia as study areas, the valley distribution in the Loess Plateau was studied based on harmonic analysis and periodgram analysis. The results indicated that in the Loess Plateau regions of different types, the period of main channel differed significantly. Generally speaking, the period of the gully region of loess plateau was greater than the transitional region, and the period of the transitional region was greater than the hill and gully area of Loess Plateau; The period of branch gully in the Loess Plateau mainly ranged from 400 to 800 m, which accounted for 97.5% of the overall periods. Based on t-test of the period of branch gully in four different research areas, the results showed that the mean periods of Xifeng、Jixian and Ansai had no significant difference (P>0.05), while in the two side test,all the probability of mean period of branch gully in Guyuan、Xifeng、Jixian and Ansai was less than 0.01 (P<0.01), so it can be considered that the difference was extremely significant. On analyzing the average terrain slope greater than 5° in the regions of different types, it was found that Xifeng in Gansu is steeper than Jixian in Shanxi, and Jixian in Shanxi is steeper than Ansai in Shaanxi, which is steeper than Guyuan in Ningxia. It was also found that the average period of branch gully decreased continuously with the increasing of the average slope. Therefore, it can be concluded that the average terrain slope can directly affect the formation of branch gully in the Loess Plateau.
  • [1] 刘增文,李雅素. 黄土残塬区侵蚀沟道分类研究[J]. 中国水土保持,2003(9):28-30.Liu Zengwen, Li Yasu. Study on classification of gully erosion in the remained loess area[J]. Soil and Water Conservation In China, 2003(9):28-30.
    [2] 关君蔚. 水土保持原理[M]. 中国林业出版社,1996:1-10
    [3] 贾志清,宋红竹,陈涛,等. 黄家二岔小流域土壤水分空间分布特征[J]. 北京林业大学学报,1999,21(5):88-91.Jia Zhiqing, Song Hongzhu, Chen Tao, et al.Soil moisture space distribution features in Huangjiaercha small watershed[J]. Journal of Beijing Forestry University, 1999, 21(5): 88-91. (in Chinese with English abstract)
    [4] 何福红,黄明斌,党廷辉. 黄土高原沟壑区小流域土壤水分空间分布特征[J]. 水土保持通报,2002,22(4):6-9.He Fuhong, Huang Mingbin, Dang Tinghui. Soil water distribution characteristics in Wangdongguo watershed in gully region of Loess Plateau[J]. Bulletin of Soil and Water Conservation, 2002, 24(4): 6-9. (in Chinese with English abstract)
    [5] 赵晓光,吴发启,刘秉正. 黄土高原坡耕地土壤水分主要受控因子研究[J]. 水土保持通报,1999,19(1):10-14.Zhao Xiaoguang, Wu Faqi, Liu Bingzheng. Effects of primary factors on soil moisture in cultivated slopeland[J]. Bulletin of Soil and Water Conservation, 1999, 19(1): 10-14. (in Chinese with English abstract)
    [6] 李笑吟,毕华兴,张志,等. 晋西黄土区坡面尺度地形因子对土壤水分状况的影响[J]. 北京林业大学学报,2006,28(4):51-56.Li Xiaoyin, Bi Huaxing, Zhang Zhi, et al. Impact of terrain factors on soil moisture in slopes of western Shanxi Province in loess area[J]. Journal of Beijing Forestry University, 2006, 28(4): 51-56. (in Chinese with English abstract)
    [7] 魏天兴,朱金兆. 黄土残塬沟壑区坡度和坡长对土壤侵蚀的影响分析[J]. 北京林业大学学报,2002,24(1):59-62.Wei Tianxing, Zhu Jinzhao. Effects of slope length and grade on soil erosion in the gully regions in Loess Plateau[J]. Journal of Beijing Forestry University, 2002, 24(1): 59-62. (in Chinese with English abstract)
    [8] 陈浩. 陕北黄土高原沟道小流域形态特征分析[J]. 地理研究,1986(1):82-92.Chen Hao. A preliminary study on geomorphic features of small drainage basins on the Loess Plateau in northern shanxi[J]. Geographical Research, 1986(1): 82-92. (in Chinese with English abstract)
    [9] 李后强,艾南山. 分形地貌学及地貌发育的分形模型[J].自然杂志,1991,15(7):516-519.Li Houqiang, Ai Nanshan. Fractal geomorphology and the model for landform development[J]. Journal of Nature, 1991,15(7): 516-519. (in Chinese with English abstract)
    [10] 何隆华,赵宏. 水系的分形维数及其含义[J]. 地理科学,1996,16(2):124-128.He Longhua, Zhao Hong. The fractal dimension of river networksand its interpretation[J]. Scientia Geographica Sinica, 1996, 16(2): 124-128. (in Chinese with English abstract)
    [11] 雷会珠,武春龙. 黄土高原分形河网研究[J]. 山地学报,2001,19(5):474-477.Lei Huizhu, Wu Chunlong. The fractal study on drainage network in the loess plateau[J]. Journal of Mountain Science, 2001, 19(5): 474-477. (in Chinese with English abstract)
    [12] 高世铭. 陇中黄土丘陵沟壑区生态环境建设与农业可持续发展研究[M]. 黄河水利出版,2003:1.
    [13] 中国森林立地分类编写组. 中国森林立地分类[M]. 中国林业出版社,1989:169.
    [14] 毕华兴,谭秀英,李笑吟. 基于DEM 的数字地形分析[J]. 北京林业大学学报,2005,27(2):49-53.Bi Huaxing, Tan Xiuying, Li Xiaoyin. Digital terrain analysis based on DEM[J]. Journal of Beijing Forestry University, 2005, 27(2): 49-53. (in Chinese with English abstract)
    [15] Jenson S K, Domin G J. Extracting topographic structure from digital elevation data for geographical information system analysis[J]. Photogrammetric Engineering and Remote Sensing, 1988, 54(11): 1593-1600.
    [16] 徐涛,胡光道. 基于数字高程模型自动提取水系的若干问题[J]. 地理与地理信息科学,2004,20(5):11-14.Xu Tao, Hu Guangdao. Several problems and their solutions in dem-based automatic drainage network extraction[J]. Geography and Geo-Information Science, 2004, 20(5): 11-14. (in Chinese with English abstract)
    [17] 安彦川,张岩,朱清科,等. 基于谐波分析的黄土高原小流域沟谷分布规律研究[J]. 北京林业大学学报,2009,31(4):84-89.An Yanchuan, Zhang Yan, Zhu Qingke. Quantifying valley topographic distribution using harmonics analysis in the Loess[J]. Journal of Beijing Forestry University, 2009, 31(4): 84-89. (in Chinese with English abstract)
    [18] 周俊,张鹏,刘成良. 基于时间序列分析的卡尔曼滤波组合导航算法[J]. 农业工程学报,2010,26(12):254-258.Zhou Jun, Zhang Peng, Liu Chengliang. Kalman filtering for integrated navigation based on time series analysis[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2010, 26(12): 254-258. (in Chinese with English abstract)
    [19] 张霞,焦全军,张兵,等. 利用MODIS_EVI图像时间序列提取作物种植模式初探[J]. 农业工程学报,2008,24(5):161-165.Zhang Xia, Jiao Quanjun, Zhang Bing, et al. Preliminary study on cropping pattern mapping using MODIS_EVI image time series[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2008, 24(5): 161-165. (in Chinese with English abstract)
    [20] 吴文斌,杨鹏,唐华俊,等. 两种NDVI 时间序列数据拟合方法比较[J]. 农业工程学报,2009,25(11):183-188.Wu Wenbin, Yang Peng, Tang Huajun. Comparison of two fitting methods of NDVI time series datasets[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2009, 25(11): 183-188. (in Chinese with English abstract)
    [21] 林忠辉,莫兴国. NDVI时间序列谐波分析与地表物候信息获取[J]. 农业工程学报,2006,22(12):138-144.Lin Zhonghui, Mo Xingguo. Phenologies from harmonics analysis of AVHRR NDVI time series[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2006, 22(12): 138-144. (in Chinese with English abstract)
    [22] Sellers P J, Los S O, Tucker C J, et a1. A revised land surface parameterization (SiB2)for atmospheric GCMs. Part 2: The generation of global fields of terrestrial biophysical parameters from satellite data[J]. Journal of Climate, 1996, 9: 706-737.
    [23] Sellers P J, Tucker C J, Collatz S O, et a1. A global 1 by 1 NDVI data set for climate studies. Part 2: The generation of global fields of terrestrial biophysical parameters from the NDVI[J]. International Journal of Remote Sensing, 1994, 15: 3519-3545.
    [24] Roerink G J, Menenti M, Verhoef W. Reconstructing cloudfree NDVI composites using Fourier analysis of time series[J]. International journal of Remote Sensing, 2000, 21(9): 1911-1917.
    [25] 陆文杰,李正浩. 植被指数序列中的天气影响评估[J]. 中国农业气象,1996,17(2):36-40.
    [26] 王丹,姜小光,唐伶俐,等. 利用时间序列傅立叶分析重构无云NDVI图像[J]. 国土资源遥感,2005(2):29-32.Wang Dan, Jiang Xiaoguang. The application of time-series Fourier analysis to reconstructing cloud-free NDVI images[J]. Remote Sensing for Land and Resources, 2005(2): 29-32.
    [27] 韦玉春,陈锁忠. 地理建模原理与方法[M]. 科学出版社,2005:214-216.
计量
  • 文章访问数:  1633
  • HTML全文浏览量:  0
  • PDF下载量:  723
  • 被引次数: 0
出版历程
  • 收稿日期:  2011-11-01
  • 修回日期:  2012-03-31
  • 发布日期:  2012-05-31

目录

    /

    返回文章
    返回