[1]帕里达·马给拉,张登清,吉力力·阿不都外力.博尔塔拉河流域土壤有机碳的空间结构分析[J].水土保持研究,2015,22(01):100-104.
　Palida·Mageila,ZHANG Dengqing,Jilili·Abuduwaili.Spatial Structure Analysis of Soil Organic Carbon in Bortala River Basin[J].Research of Soil and Water Conservation,2015,22(01):100-104.
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博尔塔拉河流域土壤有机碳的空间结构分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 22 期数: 2015年01期 页码: 100-104 栏目: 出版日期: 2015-02-28
Title:
Spatial Structure Analysis of Soil Organic Carbon in Bortala River Basin
作者:
帕里达·马给拉1,2, 张登清2, 吉力力·阿不都外力2
1. 新疆大学 资源与环境科学学院, 乌鲁木齐 830046;
2. 中国科学院 新疆生态与地理研究所 荒漠与绿洲生态国家重点实验室, 乌鲁木齐 830011
Author(s):
Palida·Mageila1,2, ZHANG Dengqing2, Jilili·Abuduwaili2
1. College of Resources and Environment Sciences, Xinjiang University, Urumqi 830046, China;
2. State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
关键词:
博尔塔拉河流域; 土壤有机碳; 地统计分析; 空间分布
Keywords:
Boertala River Basin; soil organic carbon; geostatistical analysis; spatial distribution
分类号:
S153.6+21
摘要:
利用描述性统计分析和地统计分析，对博尔塔拉河流域0—20 cm深度土壤有机碳的空间分布特征进行了研究。结果表明：博尔塔拉河流域土壤有机碳符合正态分布；半方差函数分析表明，博河上部和下部有机碳较好地符合高斯模型分布，中部有机碳符合线型模型分布。块金值与基台值的比值表明博河上部土壤有机碳含量的空间相关性很弱，说明随机性因素（如施肥、耕作措施、种植制度等各种人为活动）引起的空间变异起主要作用；中部和下部土壤有机碳含量表现为中等空间相关性，表明结构性（如气候、母质、地形、土壤类型、自然因素等）因素和随机因素共同起作用。Kriging插值表明：（1）博尔塔拉河流域土壤有机碳的空间分布特征主要以斑块状为主，基本与耕地分布相吻合；（2）全流域最大值出现在下游，可能与耕作模式以及河流从上游携带大量营养物质，通过灌溉在下游土壤沉淀累积有关；（3）博乐市周边土壤有机碳含量最低，这可能主要与博乐市周围为城市和工业用地有关。
Abstract:
Using statistical analysis and geostatistical analysis, spatial distribution of soil organic carbon in depth of 0—20 cm in the Bortala River Basin was investigated. The results showed that the semivariance analysis indicated that soil organic carbon change process had obvious size difference. Organic carbon distribution in the upper and lower reaches of Boratala River Basin can be well described by Gaussian model, and the organic carbon distribtution in the middle reaches can be fitted by the linear model. The ratio of nugget value and base value indicates that the spatial correlation of soil organic carbon content in the Bo River upper is very weak, the random factors (such as fertilization, tillage, cropping systems and other human activities cause spatial variability) play the major role; soil organic carbon contents in the middle and lower reaches exhibited moderate spatial correlation, indicating that structural factors (such as climate, parent material, topography, soil type, natural factors) and random factors play the roles. The Kriging interpolation showed that: (1) the spatial distribution characteristics of soil organic carbon present as the plaque in Bortala River Valley, which is consistent with the distribution of cultivated land; (2) the maximum value of the whole basin appeared in the downstream because of the cultivation mode and large amounts of nutrients moved from the upstream of river, soil deposition in the lower reaches due to irrigation; (3) soil organic carbon content around Bole City is the minimum, which may be related to the city and industry land around Bole.

参考文献/References:

[1] Schlesinger W H. Evidence from chronosequence studies for a low carbon-storage potential of soils[J]. Nature,1990,348(6298):232-234.
[2] 刘允芬,欧阳华,曹广民,等.青藏高原东部生态系统土壤碳排放[J].自然资源学报,2001,16(2):152-160.
[3] 林丽,曹广民,徐世晓,等.青海盐湖碳源/汇功能初探[J].干旱区资源与环境,2010,24(8):22-26.
[4] 王其兵,李凌浩.内蒙古锡林河流域草原土壤有机碳及氮素的空间异质性分析[J].植物生态学报,1998,22(5):409-414.
[5] 赵锐锋,张丽华,赵海莉,等.黑河中游湿地土壤有机碳分布特征及其影响因素[J].地理科学,2013,33(3):363-370.
[6] 王玉刚,肖笃宁,李彦,等.三工河流域绿洲土壤有机碳的空间分布[J].中国沙漠,2011,31(1):101-107.
[7] 唐晓红,黄雪夏,魏朝富.不同尺度土壤有机碳空间分布特征研究综述[J].中国农学通报,2005,21(3):224-228.
[8] 孙慧兰,李卫红,杨佘辉,等.伊利山地不同海拔土壤有机碳的分布[J].地理科学,2012,32(5):603-608.
[9] 李林海,郜二虎,梦梦,等.黄土高原小流域不同地形下土壤有机碳分布特征[J].生态学报,2013,33(1):179-187.
[10] 王成己,潘根兴,田有国.保护性耕作下农田表土有机碳含量变化特征分析:基于中国农业生态系统长期试验资料[J].农业环境科学学报,2009,28(12):2464-2475.
[11] 苏建红,朱新萍,王新军,等.长期围栏封育对高山草原土壤有机碳空间变异的影响[J].干旱区研究,2012,29(6):997-1002.
[12] 余涛,杨忠芳,候青叶,等.我国主要农耕区水稻土壤有机碳含量分布及影响因素研究[J].地学前缘,2011,18(6):11-19.
[13] 李龙,吴丽芝,姚云峰,等.小流域土壤有机碳含量的空间变异特征研究:以内蒙古赤峰市黄花甸子流域为例[J].水土保持研究,2013,20(5):18-23.
[14] 刘珊珊,宫渊波,向香勇,等.雅安紫色土小流域土壤有机碳及碳组分分布特征[J].水土保持研究,2012,19(3):63-66.
[15] 陈志军,张晶,卡米拉,等.博尔塔拉河流域水文特性[J].水资源研究,2007,28(1):25-28.
[16] 王勇辉,马蓓,海米提·依米提.艾比湖主要补给河流下游河岸带土壤盐分特征[J].干旱区研究,2013,30(2):196-202.
[17] 张建锋,张旭东,周金星,等.世界盐碱地资源及其改良利用的基本措施[J].水土保持研究,2005,12(6):32-34.
[18] 鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000:25-38.
[19] 阿依古丽·买买提,吉力力·阿不都外力,葛拥晓.玛纳斯河流域绿洲土壤养分空间变异特征与格局[J].干旱区资源与环境,2013,27(9):153-159.
[20] 马黄群,胡玉福,徐柱,等.运用地统计学的土壤有机碳含量空间分布研究[J].地理空间信息,2012,10(3):75-80.
[21] 王政权.地统计学及在生态学中的应用[M].北京:科学出版社,1999.
[22] 张甘霖,龚子同.土壤调查实验室分析方法[M].北京:科学出版社,2012.
[23] 李建辉,李晓秀,张汪寿,等.基于地统计学的北运河下游土壤养分空间分布[J].地理科学,2011,31(8):1001-1006.
[24] 杨秀清,韩有志.关帝山森林土壤有机碳和氮素的空间变异特征[J].林业科学研究,2011,24(2):223-229.
[25] Gambardella C A, Moorman T B, Novak J M, et al. Field-scale variability of soil properties in central Iowa soils[J]. Soil Science Society of America Journal,1994,58(5):1501-1511.
[26] 李有威,刘源,于娜,等.不同放牧强度下荒漠草原土壤有机碳的空间变异特征[J].内蒙古农业科技,2012(1):58-60.

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备注/Memo

收稿日期:2014-03-29;改回日期:2014-05-05。
基金项目:国家自然科学资助项目（41101190）；中国科学院西部之光项目（XBBS201106）。
作者简介:帕里达·马给拉(1989-),女(哈萨克族),新疆哈密人,硕士,研究方向:气候与环境。E-mail:paridasan@126.com
通讯作者:吉力力·阿不都外力(1964-),男(维吾尔族),新疆拜城县人,研究员,主要从事干旱区资源环境,生态安全和景观变化以及与俄罗斯和中亚国家的合作研究。E-mail:jilil@ms.xjb.ac.cn

更新日期/Last Update: 1900-01-01