天山北坡绿洲土壤有机碳和养分时空变异特征

doi:10.11821/yj2006060008

地理研究 ›› 2006, Vol. 25 ›› Issue (6): 1013-1021.doi: 10.11821/yj2006060008

天山北坡绿洲土壤有机碳和养分时空变异特征

许文强^1,2, 罗格平¹, 陈曦¹, 肖鲁湘^1,2

1. 中国科学院新疆生态与地理研究所,乌鲁木齐830011;
2. 中国科学院研究生院,北京100039

收稿日期:2006-03-23 修回日期:2006-06-30 出版日期:2006-12-15 发布日期:2006-12-15
作者简介:许文强(1979-),男,甘肃高台人,博士研究生。主要从事土地利用与土地覆被变化、遥感与GIS应用研究。E-mail:xuwq@ms.xjb.ac.cn
基金资助:
国家自然科学基金项目(批准号40471134);“西部之光”联合学者项目‘干旱区绿洲LUCC及其对绿洲稳定性影响’

Spatio-temporal variability of soil organic C and nutrients in the oasis of the northern slope of the Tianshan Mountains

XU Wen-qiang^1,2, LUO Ge-ping¹, CHEN Xi¹, XIAO lu-xiang^1,2

1. Xinjiang Institute of Ecology and Geography,CAS,Urumqi 830011,China;
2. Graduate School of the Chinese Academy of Sciences,Beijing 100039,China

Received:2006-03-23 Revised:2006-06-30 Online:2006-12-15 Published:2006-12-15

摘要/Abstract

摘要：

本文以天山北坡三工河流域绿洲作为研究区,利用1982、1999和2003年土壤养分数据,应用地统计学方法,分析绿洲土壤有机碳和养分的时空变异特征。结果显示:研究区1982、1999和2003年土壤有机碳和养分具有显著的差异性。空间结构上,土壤有机碳和养分具有中等或较弱的空间自相关;受土壤类型、种植作物种类等的影响,研究区土壤有机碳具有较强的各向异性,但碱解氮、速效磷和速效钾各向异性较弱。Kriging和IDW插值分析表明,土壤有机碳和养分总体呈增加的趋势,绿洲土壤表现为“碳汇”,尤其在种植6年以上的多年生作物分布区,土壤“碳汇”趋势更加明显,说明以绿洲农业为主的人类活动基本合理,土壤质量正逐步改善。

关键词: 绿洲, 土壤有机碳, 土壤养分, 地统计, 三工河流域

Abstract:

The relationship between soil organic C and land use change is one of the important fields in the study on global change.In the past 20 years,with the rapid economic development and population increase in China,large-scale land reclamation resulted in oasis expansion and natural desert vegetation decrease,especially in Xinjiang.Taking the oasis of Sangong river watershed as a study case,we have evaluated the spatio-temporal variability of soil organic C and nutrients.The results show that:(1) The soil OC contents was roughly equivalent in 1982 and 2003,but lower in 1999 than in 1982 and 2003.The AN,AP and AK contents tended to increase with cultivation time.(2) The nugget-to-sill ratio of soil OC changed from 53.3% to 70.3%,suggesting that the spatial correlation belongs to moderate class.However,the nugget-to-sill of AN,AP and AK is higher,suggesting that the spatial correlation belongs to low class.Influenced by soil types and planting crops of the study area,the anisotropies of soil OC were obvious,while those of AN,AP and AK were weaker.(3) The results estimated by Kriging and IDW showed that soil OC declined from 1982 to 1999,and then increased from 1999 to 2003.AN,AP and AK increased significantly from 1982 to 1999,while decreased from 1999 to 2003 due to balanced fertilization application.In conclusion,soil OC had been increasing with the cultivation time in the Sangong river watershed,indicating that oasis soil presented C sink.This also indicates that the human activities in the oasis were reasonable and the environment of the oasis was improved.

Key words: oasis, soil organic C, soil nutrients, geostatistic, Sangong river watershed

许文强, 罗格平, 陈曦, 肖鲁湘. 天山北坡绿洲土壤有机碳和养分时空变异特征[J]. 地理研究, 2006, 25(6): 1013-1021.

XU Wen-qiang,LUO Ge-ping,CHEN Xi,XIAO lu-xiang. Spatio-temporal variability of soil organic C and nutrients in the oasis of the northern slope of the Tianshan Mountains[J]. GEOGRAPHICAL RESEARCH, 2006, 25(6): 1013-1021.

参考文献

[1] Wat s on R T,R odh e H,Oeschger H,et al. Gr een house gas es and aerosols. In:Climat e Ch ange:t he IPCC Scient ificAs sessment,IPCC. Cambr idge:Cambridge U niversi ty Pres s,1990. 1~40.

[2] IGBP T errest rial Carbon Working Group. T he t errest rial carbon cy cle:im plicat ions for t he Kyoto Prot oco.l Scien ce,1998,280:1393~1394.

[3] Wast on R T,Noble I R,Bolin B,et al. Land Us e,Land Us e Ch ange and Forest ry. A Special Report of t he Int ergov-ernment al Pan el on Climat e Change. Cambridge:Cam bridge Uni versit y Pres s,2000. 377.

[4] 李忠,孙波,林心雄.我国东部土壤有机碳的密度及转化的控制因素.地理科学,2001,21(4):301~307.

[5] Thu ille A,Buch man n N,Schulze E D. Carbon st ocks and soil r espirat ion rat es during defor est ati on,grassland u seand subs equent Norway s pruce afforest at ion in t he sout hern Alps,T taly. T ree Ph ysiology,2000,20:849~857.

[6] Guo L B,Gifford R M1 Soil carb on st ocks and land use chan ge:a meta analysi s1 Gl obal Change Biology,2002,8:345~360.

[7] 许文强,罗格平,陈曦,等.干旱区绿洲土地利用方式和强度对土壤粒度分布的影响1干旱区地理,2005,28(6):800~804.

[8] Maihi Y,Bald occhi D D,J avis P G. Th e carbon balance of t ropical,t em perat e and boreal forest s. Plant Cel l Envi-ron.,1999,22:715~740.

[9] 王军,傅伯杰,邱扬,等1黄土高原小流域土壤养分的空间分布格局)))Kriging插值分析1地理研究,2003,22(3):373~379.

[10] 刘付程,史学正,于东升,等.太湖流域典型地区土壤全氮的空间变异特征.地理研究,2004,23(1):63~70.

[11] 许文强,罗格平,陈曦.干旱区绿洲土壤养分对不同作物系统的响应.科学通报,2006,51(I):37~141.

[12] Achard F,Eva H D,St ibig H J,et al. Det erminat ion of deforest at ion rat es of t he world.s hum id t ropicalforest s. Sci ence,2002,297:999~1002.

[13] De Camarg o P B,T rumb or e S E,M art inelli L A,et al1 Soi l carb on dynamics in reg rowing forest of east er n Amazo2nia1 Global C hang e Bi ol ogy,1999,5:693~702.

[14] 贾宝全.绿洲景观若干理论问题的探讨.干旱区地理,1996,19(3):58~65.

[15] 罗格平,陈曦,周可法,等.三工河流域绿洲时空变异及其稳定性研究.中国科学(D辑),2002,32(6):521~528.

[16] 樊自立,穆桂金,马英杰,等.天山北麓灌溉绿洲的形成和发展.地理科学,2002,22(2):184~189.

[17] M ann L K. Changes in soil carbon st orage aft er cul ti vat ion. Soil Sci ence,1986,142:279~288.

[18] 王政权.地统计学及在生态学中的应用.北京:科学出版社,1999. 86~88.

[19] 孙波,赵其国,闾国年.低丘红壤肥力的时空变异.土壤学报,2002,39(2):190~198.

[20] 朱会义,刘述林,贾绍凤1自然地理要素空间插值的几个问题1地理研究,2004,23(4):425~432.

[21] 李晓燕,张树文,王宗明,等.吉林省德惠市土壤特性空间变异特征与格局.地理学报,2004,59(6):989~997.

[22] C hien Y J,Lee D Y,Guo H Y1 Geos tat ist ical anal ysis of soil propert ies of mid2 west T aiwan soil s1 Soil Scien ce,1997,162:291~298.

[23] C ambardella C A,Moorman T B,Novak J M,et a l. Field2scal e variab ilit y of soil pr op ert ies in cent ral l owa soil s. SoilScien ce Societ y of Ameri ca Journ al,#1994,58:1501~1511.

[24] 杨景成,韩兴国,黄建辉,等.土壤有机质对农田管理措施的动态响应.生态学报,2003,23(4):787~796.

[25] R eeves D W1 T he rol e of organ ic mat t er in main taining soil qual ity in cont inuous cropping syst ems1 Soil&T illageR es earch,1997,43:31~167.

[26] 徐阳春,沈其荣,冉炜.长期免耕与使用有机肥对土壤微生物生物量碳、氮、磷的影响.土壤学报,2002,39(1):89~96.

[27] 罗格平,许文强,陈曦1天山北坡绿洲不同土地利用对土壤特性的影响1地理学报,2005,60(5):779~790.

[28] J aiyeoba I A. Changes in soil p ropert ies due t o cont inu ous cult ivat ion in Nigerian semiarid Savann ah. Soil&T illageR es earch,2003,70:91~98.

[29] Lal R. M ech anized til lage syst em s effect s on propert ies of a t ropical Alfisol in wat ersh ed cropped t o maize. Soil&T illage R es earch,1985,6:149~162.

[30] 蒋平安,盛建东,李宁,等.新疆测土配方施肥技术研究及应用现状.新疆农业大学学报,2003,26(1):13~16.

天山北坡绿洲土壤有机碳和养分时空变异特征

Spatio-temporal variability of soil organic C and nutrients in the oasis of the northern slope of the Tianshan Mountains

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	赵海鹏, 宋宏权, 刘鹏飞, 李霄阳, 王团徽. 1980—2015年风蚀影响下中国北方土壤有机质与养分流失时空特征[J]. 地理研究, 2019, 38(11): 2778-2789.
[2]	赵明松, 李德成, 张甘霖, 王世航. 1980-2010年安徽省土壤有机碳密度及储量时空变化分析[J]. 地理研究, 2018, 37(11): 2206-2217.
[3]	马振邦, 陈兴鹏, 贾卓, 吕鹏. 人穷还是地穷?空间贫困陷阱的地统计学检验[J]. 地理研究, 2018, 37(10): 1997-2010.
[4]	吕娜娜, 白洁, 常存, 李均力, 罗格平, 吴世新, 丁建丽. 近50年基于农作物种植结构的新疆绿洲农田蒸散发时空变化分析[J]. 地理研究, 2017, 36(8): 1443-1454.
[5]	董立宽, 方斌. 茶园土壤重金属乡镇尺度下空间异质性分析——以江浙优质名茶种植园为例[J]. 地理研究, 2017, 36(2): 391-404.
[6]	王新新, 罗格平, 叶辉, 张琪, 蔡鹏, 张苗. 天山北坡绿洲—荒漠区高时空分辨率日均气温数据集构建——以三工河流域为例[J]. 地理研究, 2017, 36(1): 49-60.
[7]	师满江, 颉耀文, 曹琦. 干旱区绿洲农村居民点景观格局演变及机制分析[J]. 地理研究, 2016, 35(4): 692-702.
[8]	刘海猛, 方创琳, 毛汉英, 石培基. 基于复杂性科学的绿洲城镇化演进理论探讨[J]. 地理研究, 2016, 35(2): 242-255.
[9]	张海霞, 牛叔文, 齐敬辉, 叶丽琼, 李娜. 基于乡镇尺度的河南省人口分布的地统计学分析[J]. 地理研究, 2016, 35(2): 325-336.
[10]	李晓东, 塔西甫拉提·特依拜, 范卓斌, 范丽丽, 谢霞, 李偲. 基于适宜性和安全性评价的干旱区绿洲后备耕地资源开发——以渭干河—库车河三角洲绿洲为例[J]. 地理研究, 2016, 35(1): 163-172.
[11]	葛淼, 薛然尹, 何进伟, 胡燕宇. 中国男性儿童呼气高峰流量参考值地理分布[J]. 地理研究, 2014, 33(3): 451-466.
[12]	玉苏甫·买买提, 买合皮热提·吾拉木, 满苏尔·沙比提. 气候变暖对渭干河-库车河三角洲绿洲棉花生产的影响[J]. 地理研究, 2014, 33(2): 251-259.
[13]	李典友, 陈良松, 李军, 倪建华, 李小刚, 潘根兴, 陆保国, 黄登林, 孙贤斌. 霍山县县域范围内不同空间尺度下农田土壤有机碳变异分析[J]. 地理研究, 2012, 31(9): 1571-1579.
[14]	张俊华, 李国栋, 南忠仁, 肖洪浪. 黑河绿洲区耕作影响下的土壤粒径分布及其与有机碳的关系[J]. 地理研究, 2012, 31(4): 608-618.
[15]	毛学刚, 李明泽, 范文义, 姜欢欢. 近30年来小兴安岭地区生物量变化及地统计分析[J]. 地理研究, 2011, 30(6): 1110-1120.