土地资源与利用

土地利用方式对西藏东部河谷山地土壤肥力性质的影响

展开
  • 1. 中国科学院水利部成都山地灾害与环境研究所,成都610041;
    2. 西藏自治区水土保持局,拉萨850000;
    3. 中国科学院研究生院, 北京100049

范建容(1969-),女,四川井研人,博士,副研究员。主要从事山地土壤侵蚀、遥感应用研究。 E-mail:fjrong@imde.ac.cn

收稿日期: 2009-12-01

  修回日期: 2010-04-12

  网络出版日期: 2010-08-25

基金资助

国家"十一五"科技支撑计划项目课题(2007BAC06B06-01);中国科学院"西部之光"人才培养计划西部博士科研启动项目

Effect of land use on soil properties in river valleys of eastern Tibet

Expand
  • 1. Institute of Mountainous Hazards and Environment, CAS, Chengdu 610041, China;
    2. Soil and Water Conservation Bureau of Tibet Autonomous Region, Lhasa 850000, China;
    3. Graduate University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2009-12-01

  Revised date: 2010-04-12

  Online published: 2010-08-25

摘要

通过现场调查取样和室内理化分析,研究了西藏东部主要河谷地区不同土地利用方式下土壤肥力性质及其随土地利用方式变化的机制。结果表明:不同土地利用方式下土壤理化性质有明显的差异,耕地和裸地土壤砂粒含量高于其他利用方式,本区域土壤砂质特征明显;受有机质积累影响,乔木林地、灌丛地土壤具有相对较高N素养分;受施肥等因素影响,农耕地土壤具有相对较高P、K养分;在所有利用方式中,裸地土壤尽管具有相对较高的粉粒含量,但所有养分指标均最低,显著低于林地土壤。总之,对于西藏脆弱生境而言,耕作使得有机质更易于消耗。由于有机质与植被之间存在明显互相促进的作用,因此维持土壤有机质平衡对于恢复植被、保护青藏高原东缘生态屏障具有重要的意义。

本文引用格式

范建容, 宫奎方, 唐家良, 郭祥, 郭芬芬, 尼玛占堆, 格桑卓玛 . 土地利用方式对西藏东部河谷山地土壤肥力性质的影响[J]. 地理研究, 2010 , 29(8) : 1528 -1536 . DOI: 10.11821/yj2010080018

Abstract

The Qinghai-Tibet Plateau is the most ecologically critical region as it is the source area of some large rivers, such as Yangtze, Huanghe, Lancang, and Yarlung Tsangbo rivers. Based on the field investigation and laboratory analysis of soil samples, this paper discussed the soil physical and chemical properties under different types of land use in main river valley areas in eastern Tibet. The results suggested that distinct differences of soil physical properties among soils under various types of land use were found, cropland and bare land had the higher content of sand compared with other types of land uses, while all the soils in this region tended to be desertified in texture; Due to the accumulation of organic matter, the soil in north-facing slopes contained higher nitrogen; While cropland soil contained higher P and K contents after the agricultural practices mainly owing to fertilization; Among all the types of land use, the bare land soil had the lowest nutrient contents, which were significantly lower than woodland soils despite of its relatively high silt content. The soil organic matter content influenced all the other N, P, K nutrients,which was positively correlated with total N, available N total P, available P and available K (R>0.527, N=97). The correlation between soil nutrients and silt content also disclosed the susceptibility of nutrient losses of disturbed soil by tillage, especially on steep hillslopes during rainfall events. Above all, organic matter management, in terms of land use scenario, is crucial for the significant protection of the regional ecology.

参考文献


[1] 李新平, 张猛, 杨正礼,等. 西藏耕种山地灌丛草原土发生特性. 西北农林科技大学学报,1995, 23(4): 21~25.

[2] 刘刚才, 王小丹, 刘淑珍. 西藏自治区的土壤理化特性探讨.山地学报,2003, 21(增刊): 54~57.

[3] 张宗锦, 刘世全, 张世熔, 等. 西藏酸性土壤的分布和酸度特征. 四川农业大学学报, 2003, 21(4): 322~327.

[4] 蔡晓布, 张永青, 钱成, 等. 西藏中部退化土壤在不同培肥措施下的肥力特征. 生态学报, 2003, 21(4): 322~327.

[5] 刘世全, 高丽丽, 蒲玉琳, 等. 西藏土壤有机质和氮素状况及其影响因素分析. 水土保持学报, 2004, 18(6): 54~57, 67.

[6] 刘世全, 高丽丽, 蒲玉琳, 等. 西藏土壤磷素和钾素养分状况及其影响因素. 水土保持学报, 2005,19(1): 75~78, 88.

[7] 刘翠花, 朱永官. 西藏青稞主产区土壤肥力现状与施肥对策. 土壤肥料,2005,(3): 23~25.

[8] Wang X D, Zhong X H, Liu S Z, et al. Regional assessment of environmental vulnerability in the Tibetan Plateau: Development and application of a new method. Journal of Arid Environmenst, 2008, 72: 1929~1939.

[9] 邵景安, 邵全琴, 刘纪远. 三江源地区各类生态系统土壤的性状及其形成能力. 地理研究, 2009, 28(3): 613~624.

[10] 钟国辉, 钟政昌, 田发益, 等. 西藏米拉山区土壤主要养分元素垂直分布特征. 山地学报,2007, 25(1): 108~113.

[11] 周利勋, 刘永春. 西藏高寒地区森林土壤资源及其开发利用. 东北林业大学学报,2003,31(6): 73~74.

[12] 鲁如坤. 土壤农业化学分析方法. 北京:中国农业科技出版社,2000.

[13] 唐家良, 张斌, 王明珠, 等. 低丘红壤区小流域土壤肥力性质空间分布特征. 土壤, 2006,38 (4): 384~389.

[14] 姜培坤, 周国模, 钱新标. 侵蚀型红壤植被恢复后土壤养分含量与物理性质的变化.水土保持学报, 2004, 18(1): 12~14.

[15] 高丽丽, 刘世全, 张世熔. 西藏土壤钾素状况及其影响因素分析. 四川农业大学学报, 2004, 22(2): 165~169, 178.

[16] Koutika L S, Sanginga N, Vanlauwe B, et al. Chemical properties and soil organic matter assessment under fallow systems in the forest margins benchmark. Soil Biology & Biochemistry, 2002, 34(6), 757~765.

[17] Vaezi A R, Sadeghi S H R, Bahrami H A, et al. Modeling the USLE K-factor for calcareous soils in northwestern Iran. Geomorphology, 2008, 97(3~4), 414~423.

[18] Wischmei W H, Mannerin JV. Relation of soil properties to its erodibility. Soil Science Society of America Proceedings, 1969, 33(1): 121~137.

[19] 姚华荣, 杨志峰, 崔保山. GIS支持下的澜沧江流域云南段土壤侵蚀空间分析. 地理研究, 2006, 25(3): 421~429.

文章导航

/