PDF Download

[1]WANG Jie,JIA Wenxiong,ZHAO Zhen,et al.Study on the Relations Between the Above Ground Biomass and the Soil Physicochemical Properties in the North Slope of Qilian Mountains[J].Research of Soil and Water Conservation,2017,24(01):36-42,48.

Copy

Study on the Relations Between the Above Ground Biomass and the Soil Physicochemical Properties in the North Slope of Qilian Mountains

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 24 Number of periods: 2017 01 Page number: 36-42,48 Column: Public date: 2017-02-28

Title:: Study on the Relations Between the Above Ground Biomass and the Soil Physicochemical Properties in the North Slope of Qilian Mountains

Author(s):: WANG Jie, JIA Wenxiong, ZHAO Zhen, CHEN Jinghua, DING Dan; College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, China

Keywords:: Qilian Mountain; meadow steppe; above ground biomass; soil physicochemical properties

CLC:: S812;S153.6

DOI:: -

Abstract:: In order to reveal the relations between the above ground biomass of meadow steppe and the soil physicochemical properties in the north slope of Qilian Mountain. We chose three typical samples in the eastern, central and western parts in the north slope of Qilian Mountains, collected the sampling data in two consecutive growing seasons, analyzed and examined the above ground biomass and soil physiochemical properties. The results show that total above ground biomass of the each sample is greater in 2014 than in 2013, and the mass increases from the east to the west. The soil moisture, soil temperature, soil organic matter, available potassium, pH value are significantly different in different growing seasons and the different layers among the sample sites. However, soil alkali-hydrolysable nitrogen and available phosphorus are relatively stable, and the differences are not signigicant. Correlation analysis shows that total above ground biomass is significantly positively correlated with soil temperature, pH value, and is significantly positively correlated with the available phosphorus, but is not significantly correlated with soil moisture. The results reveal that the major influence factors on total above ground biomass are soil temperature, available phosphorus and pH value. The soil nutrients mainly depend on the physicochemical properties of the soil, which determines the growth of vegetation and affect the biomass of plants.

References:: [1] Scurlock J M O, Hall D O. The global carbon sink:a grassland perspective[J]. Global Change Biology, 1998,4(2):229-233.
[2] 索南措.青藏高原东缘高寒草甸植被特征与土壤性质随海拔变化的响应研究[D].兰州:西北师范大学,2013.
[3] Li Xiaogang, Zhang Meilan, Li Zhuoting, et al. Dynamic s of soil properties and organic carbon pool in topsoil of zokor-made mounds at an alpine site of the Qinghai-Tibetan Plateau[J]. Biol. Fertil. Soils, 2009,45(8):865-872.
[4] Li Xiaogang, Li Fengmin, Bhupinderpal-Singh, et al. Soil management changes organic carbon pools in alpine pastureland soils[J]. Soil and Tillage Research, 2007,93(1):186-196.
[5] 张俊华,李国栋,南忠仁,等.黑河中游不同土地利用类型下土壤碳储量及其空间变化[J].地理科学,2011,31(8):982-988.
[6] 盛海彦.放牧干扰对高寒金露梅灌丛草甸群落和土壤因子影响的研究[D].陕西杨凌:西北农林科技大学,2008.
[7] 孙旭生.库布齐沙漠不同沙地类型植物群落与土壤关系的研究[D].呼和浩特:内蒙古师范大学,2010.
[8] 李恩宇,何贵永.青藏高原高寒草甸不同季节土壤理化性质及酶活性对施肥处理的响应[J].广西植物,2014,34(4):467-472.
[9] 王合领.祁连山东缘高寒草甸区土地利用对土壤有机碳的影响研究:以甘肃连城国家级保护区为例[D].兰州:兰州大学,2014.
[10] Li X G, Li F M, Zed R, et al. Soil physical properties and their relations to organic carbon pools as affected by land use in an alpine pastureland[J]. Geoderma, 2007,139(1):98-105.
[11] 高超.东祁连山不同退化程度高寒草甸草原土壤有机质特性及其对草地生产力的影响[D].兰州:甘肃农业大学,2007.
[12] 杨成德.东祁连山高寒草甸土壤微生物量及其与土壤物理因子相关性特征[J].草业学报,2007,16(4):62-68.
[13] 张禹舜,贾文雄,赵一飞,等.基于CASA模型研究祁连山地区植被净初级生产力的时空变化[J].西北植物学报,2014,34(10):2085-2091.
[14] 侯兆疆,赵成章,李钰,等.不同坡向高寒退化草地狼毒株高和枝条数的权衡关系[J].植物生态学报,2014,38(3):281-288.
[15] 常博.祁连山排露沟流域草地植被特征及其对水分条件的响应[D].兰州:甘肃农业大学,2014.
[16] 贾文雄,刘亚荣,张禹舜,等.祁连山草甸草原物种多样性和生物量与气候要素的关系[J].干旱区研究,2015,32(6):1167-1172.
[17] 马金宝,张培栋,李新荣.旱泉沟流域天然鹳丛退化成因及保育对策[J].草业科学,2007,24(4):23-26.
[18] 张千千.六盘山叠叠沟小流域土壤水分动态变化与植被生长的研究[D].河北保定:河北农业大学,2009.
[19] 陈涛.呼伦贝尔退化羊草草甸物种多样性及土壤理化性质的研究[D].兰州:甘肃农业大学,2008.
[20] 杨成德,龙瑞军,陈秀蓉,等.东祁连山高寒草甸土壤微生物量及其与土壤物理因子相关性特征[J].草业学报,2007,16(4):62-68.
[21] 李绍良,康师安.内蒙古草原土壤退化进程及其评价指标的研究[J].土壤通报,1997,28(6):241-243.
[22] 高超.东祁连山不同退化程度高寒草甸草原土壤有机质特性及其对草地生产力的影响[D].兰州:甘肃农业大学,2007.
[23] 石红霄,侯向阳,师尚礼,等.高山嵩草草甸初级生产力、多样性与土壤因子的关系[J].草业学报,2015,24(10):40-47.
[24] Pal D, Broadbent F E. Influence of moisture on rice straw decomposition in soils[J]. Soil Science Society of America Journal, 1975,39(1):59-63.
[25] 徐跃,姚天全.气候因素对土壤有机质组成和性质的影响[J].山地研究,1994,12(3):163-168.
[26] 王淑平,周广胜,吕育财,等.中国东北样带(NECT)土壤碳、氮、磷的梯度分布及其与气候因子的关系[J].植物生态学报,2002,26(5):513-517.
[27] 王长庭,龙瑞军,王启基,等.高寒草甸不同海拔梯度土壤有机质氮磷的分布和生产力变化及其与环境因子的关系[J].草业学报,2005,14(4):15-20.

Similar References:

Memo

Last Update: 1900-01-01