准噶尔荒漠区域尺度浅层土壤化学计量特征及其空间分布格

doi:10.11686/cyxb2016009

草业学报 ›› 2016, Vol. 25 ›› Issue (7): 13-23.DOI: 10.11686/cyxb2016009

准噶尔荒漠区域尺度浅层土壤化学计量特征及其空间分布格

陶冶^{1, 2}, 刘耀斌³, 吴甘霖¹, 张元明^{2, *}

1.安庆师范大学生命科学学院, 皖西南生物多样性研究与生态保护安徽省重点实验室,安徽安庆 246133；
2.中国科学院新疆生态与地理研究所,中国科学院干旱区生物地理与生物资源重点实验室,新疆乌鲁木齐 830011；
3.固原市工业和信息化局,宁夏固原 756000

收稿日期:2016-01-06 修回日期:2016-03-15 出版日期:2016-07-20 发布日期:2016-07-20
通讯作者: ymzhang@ms.xjb.ac.cn
作者简介:陶冶(1983-),男,安徽宿州人,讲师,博士。E-mail: xishanyeren@163.com
基金资助:
国家重点基础研究发展计划项目(2014CB954202),国家自然科学基金项目(41471251)和新疆杰出青年人才项目(2013711013)资助

Regional-scale ecological stoichiometric characteristics and spatial distribution patterns of key elements in surface soils in the Junggar desert, Chin

TAO Ye^{1, 2}, LIU Yao-Bin³, WU Gan-Lin¹, ZHANG Yuan-Ming^{2, *}

1.College of Life Sciences, The Province Key Laboratory of the Biodiversity Study and Ecology Conservation in Southwest Anhui, Anqing Normal University, Anqing 246133, China;
2.Key Laboratory of Biogeography and Bioresource in Arid Land, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
3.Bureau of Industry and Information Technology of Guyuan, Guyuan 756000, China

Received:2016-01-06 Revised:2016-03-15 Online:2016-07-20 Published:2016-07-20

摘要/Abstract

摘要：

干旱荒漠生态系统具有降水稀少、土壤贫瘠、生物多样性低的特点,对荒漠土壤生态化学计量特征的研究有助于深入了解荒漠土壤养分供给能力及其对生物多样性和生态系统稳定性的影响。对准噶尔荒漠79个样点浅层(0~10 cm)土壤及环境因子进行调查取样,分析了土壤有机碳(C)、全氮(N)及全磷(P)化学计量特征、空间分布及其影响因素。结果表明,准噶尔荒漠土壤C、N、P平均含量分别为(5.73±0.49),(0.207±0.009)和(0.347±0.004) g/kg,C:N、C:P、N:P分别为(29.92±2.55),(15.97±1.23)和(0.498±0.024)。土壤P稳定性最高(CV=0.098),而C、C:N和C:P的变异性较强(CV=0.687~0.758)。C、P、C:N及C:P在不同生境(沙漠、戈壁和盐碱荒漠)、不同群落(白梭梭、梭梭及小灌木)间均存在差异。与全国及全球平均水平相比,准噶尔荒漠土壤C、N、P含量、C:P及N:P均较低而C:N较高,养分元素缺乏程度表现为N>C>P。土壤养分元素及其化学计量比之间多具有显著的二次函数关系,且化学计量比主要受C和N的制约。在区域尺度上,各化学计量参数表现出明显的空间异质性,其中C、C:N和C:P分布格局相似,并受年降水量、纬度和经度的影响;N与N:P分布格局相似,受经度、海拔和年均温的影响。

Abstract:

Ecological stoichiometry focuses on the element equilibrium and coupling relations, and it has been widely used in study of plant growth, limiting element determination, and ecosystem stability, among others. Desert ecosystems are an important component of terrestrial ecosystems, and are characterized by low precipitation, poor soil development and low floral and faunal biodiversity. Study of the ecological stoichiometry of desert soils enhances understanding of the nutrient supply capability and its effect on biodiversity and ecosystem stability. In this study, surface soil samples (0-10 cm) and environmental factors (including climate and geographical factors) in 79 sites in the Junggar desert were investigated, and then the stoichiometric characteristics of soil organic carbon (C), total nitrogen (N), total phosphorus (P) contents, their distribution patterns and factors influencing them were systematically studied using one-way ANOVA, a Kriging technique and correlation analysis. Soil C, N and P contents were (5.73±0.49), (0.207±0.009) and (0.347±0.004) g/kg respectively; and the soil C∶N, C∶P, and N∶P ratios were (29.92±2.55), (15.97±1.23) and (0.498±0.024) respectively. Soil P showed the highest stability (CV=0.098), whereas C, C∶N and C∶P exhibited relatively strong variability (CV=0.687-0.758). Soil C, P, C∶N and C∶P varied among different habitats (sandy desert, Gobi desert and saline-alkali desert) and different communities (Haloxylon ammodendron, H. persicum and small shrubs). Compared with national and global averages, the soil C, N and P contents, and C∶P and N∶P ratios in the Junggar desert were lower, but the C∶N was higher. The degree of deficiency of soil nutrient elements ranked in order: N>C>P. The soil nutrients and their stoichiometric ratios typically exhibited quadratic relationships with other nutrients, and the stoichiometric ratios were dominated by C and N. At a regional scale, all stoichiometric traits displayed obvious spatial heterogeneity. Soil C, and C∶N and C∶P ratios showed similar distribution patterns and were influenced by mean annual precipitation, latitude and longitude. Soil N and N∶P ratio displayed similar distribution patterns and were influenced by longitude, elevation and mean annual temperature.

陶冶, 刘耀斌, 吴甘霖, 张元明. 准噶尔荒漠区域尺度浅层土壤化学计量特征及其空间分布格[J]. 草业学报, 2016, 25(7): 13-23.

TAO Ye, LIU Yao-Bin, WU Gan-Lin, ZHANG Yuan-Ming. Regional-scale ecological stoichiometric characteristics and spatial distribution patterns of key elements in surface soils in the Junggar desert, Chin[J]. Acta Prataculturae Sinica, 2016, 25(7): 13-23.

参考文献

[1] Elser J J, Sterner R W, Gorokhova E, et al . Biological stoichiometry from genes to ecosystems. Ecology Letters, 2000, 3: 540-550.
[2] Güsewell S. N: P ratios in terrestrial plants: Variation and functional significance. New Phytologist, 2004, 164(2): 243-266.
[3] He J S, Han X G. Ecological stoichiometry: Searching for unifying principles from individuals to ecosystems. Chinese Journal of Plant Ecology, 2010, 34(1): 2-6.
[4] Wang S Q, Yu G R. Ecological stoichiometry characteristics of ecosystem carbon, nitrogen and phosphorus elements. Acta Ecologica Sinica, 2008, 28(8): 3938-3949.
[5] Zhu Q L, Xing X Y, Zhang H, et al . Soil ecological stoichiometry under different vegetation area on Loess hilly-gully region. Acta Ecologica Sinica, 2013, 33(15): 4674-4682.
[6] Huang C Y. Pedology[M]. Beijing: China Agriculture Press, 2000.
[7] Wang W Q, Tong C, Jia R X. Ecological stoichiometry characteristics of wetland soil carbon, nitrogen and phosphorus in different water-flooded frequency. Journal of Soil and Water Conservation, 2010, 24(3): 238-242.
[8] Li C J, Xu X W, Sun Y Q, et al . Stoichiometric characteristics of C, N, P for three desert plants leaf and soil at different habitats. Arid Land Geography, 2014, 37(5): 976-984.
[9] Zhang Y M, Wang X Q. Study on the Biological Soil Crust of the Junggar Desert[M]. Beijing: Science Press, 2008.
[10] Whitford W G. Ecology of Desert Systems[M]. London, UK: Academic Press, 2002.
[11] Zhang L Y, Chen C D. On the general characteristics of plant diversity of Gurbantunggut sandy desert. Acta Ecologica Sinica, 2002, 22(11): 1923-1932.
[12] Qian Y B, Wu Z N, Zhao R F, et al . Vegetation patterns and species-environment relationships in the Gurbantunggut Desert of China. Journal of Geographical Sciences, 2008, 18(4): 400-414.
[13] China Vegetation Committee, Chinese Academy of Sciences. Vegetation Atlas of China[M]. Beijing: Science Press, 2001.
[14] Bao S D. Soil Chemical Analysis of Agriculture[M]. Beijing: China Agriculture Press, 2000.
[15] Hijmans R J, Cameron S E, Parra J L, et al . Very high resolution interpolated climate surfaces for global land areas. International Journal of Climatology, 2005, 25: 1965-1978.
[16] Zhou L L, Zhu H Z, Zhong H P, et al . Spatial analysis of soil bulk density in Yili, Xinjiang Uygur Autonomous Region, China. Acta Prataculturae Sinica, 2016, 25(1): 64-75.
[17] Tian H Q, Chen G S, Zhang C, et al . Pattern and variation of ratios in China's soils: a synthesis of observational data. Biogeochemistry, 2010, 98(1/3): 139-151.
[18] Wang S Q, Zhou C H, Li K R, et al . Analysis on spatial distribution characteristics of soil organic carbon reservoir in China. Acta Geographica Sinica, 2000, 55(5): 533-544.
[19] Zeng Q C, Li X, Dong Y H, et al . Ecological stoichiometry characteristics and physical-chemical properties of soils at different latitudes on the Loess Plateau. Journal of Natural Resources, 2015, 30(5): 870-879.
[20] Yang Y, Liu B R, Yang X G, et al . Soil stoichiometry characteristics of artificial Caragana korshinskii shrubs with different density in desert steppe. Bulletin of Soil and Water Conservation, 2014, 34(5): 67-73.
[21] Qing Y, Sun F D, Li Y, et al . Analysis of soil carbon, nitrogen and phosphorus in degraded alpine wetland, Zoige, southwest China. Acta Prataculturae Sinica, 2015, 24(3): 38-47.
[22] Cleveland C C, Liptzin D. stoichiometry in soil: Is there a Redfield for the microbial biomass. Biogeochemistry, 2007, 85: 235-252.
[23] Ding F, Lian P Y, Zeng D H. Characteristics of plant leaf nitrogen and phosphorus stoichiometry in relation to soil nitrogen and phosphorus concentrations in Songnen Plain meadow. Chinese Journal of Ecology, 2011, 30(1): 77-81.
[24] Pan J, Song N P, Wu X D, et al . Effects of different planting-years of artificial Caragana intermedia shrubs on soil organic carbon, nitrogen and phosphorus stoichiometry characteristics in desert steppe. Journal of Zhejiang University (Agriculture Life Sciences), 2015, 41(2): 160-168.
[25] Wang J L, Zhong Z M, Wang Z H, et al . Soil C/N distribution characteristics of alpine steppe ecosystem in Qinghai-Tibetan Plateau. Acta Prataculturae Sinica, 2014, 23(2): 9-19.
[26] Tao Y, Zhang Y M. Leaf and soil stoichiometry of four herbs in the Gurbantunggut Desert, China. Chinese Journal of Applied Ecology, 2015, 26(3): 659-665.
[27] Liu Z Y, Yang N. Soil ecological stoichiometry properties of different re-vegetation stages on sloping-land of purple soil. Chinese Agricultural Science Bulletin, 2015, 31(18): 163-167.
[28] Yang J, Xie Y Z, Wu X D, et al . Stoichiometry characteristics of plant and soil in alfalfa grassland with different growing years. Acta Prataculturae Sinica, 2014, 23(2): 340-345.
[29] Fan J W, Zhang L X, Zhang W Y, et al . Plant root N and P levels and their relationship to geographical and climate factors in a Chinese grassland transect. Acta Prataculturae Sinica, 2014, 23(5): 69-76.
[30] Wang C L, Guo Q S, Tan D Y, et al . Haloxylon ammodendron community patterns in different habitats along southeastern edge of Zhunger Basin. Chinese Journal of Applied Ecology, 2005, 16(7): 1224-1229.
[31] Wang X Q, Jiang J, Lei J Q, et al . The distribution of ephemeral vegetation on the longitudinal dune surface and its stabilization significance in the Gurbantunggut Desert. Acta Geographica Sinica, 2003, 58(4): 598-605.
[32] Neufeldt H, Da Silva J, Ayarza M A, et al . Land-use effects on phosphorus fractions in Cerrado Oxisols. Biology and Fertility of Soils, 2000, 31(1): 30-37.
[33] Chen F H, Huang W, Jin L Y, et al . Spatiotemporal precipitation variations in the arid Central Asia in the context of global warming. Science China: Earth Science, 2011, 41(11): 1647-1657.
[34] Zhang S J, Wang T M, Wang T, et al . Spatial-temporal variation of the precipitation in Xinjiang and its abrupt change in recent 50 years. Journal of Desert Research, 2010, 30(3): 668-674.
[3] 贺金生, 韩兴国. 生态化学计量学:探索从个体到生态系统的统一化理论. 植物生态学报, 2010, 34(1): 2-6.
[4] 王绍强, 于贵瑞. 生态系统碳氮磷元素的生态化学计量学特征. 生态学报, 2008, 28(8): 3938-3949.
[5] 朱秋莲, 邢肖毅, 张宏, 等. 黄土丘陵沟壑区不同植被区土壤生态化学计量特征. 生态学报, 2013, 33(15): 4674-4682.
[6] 黄昌勇. 土壤学[M]. 北京: 中国农业出版社, 2000.
[7] 王维奇, 仝川, 贾瑞霞. 不同淹水频率下湿地土壤碳氮磷生态化学计量学特征. 水土保持学报, 2010, 24(3): 238-242.
[8] 李从娟, 徐新文, 孙永强, 等. 不同生境下三种荒漠植物叶片及土壤C、N、P的化学计量特征. 干旱区地理, 2014, 37(5): 976-984.
[9] 张元明, 王雪芹. 准噶尔荒漠生物结皮研究[M]. 北京: 科学出版社, 2008.
[11] 张立运, 陈昌笃. 论古尔班通古特沙漠植物多样性的一般特点. 生态学报, 2002, 22(11): 1923-1932.
[13] 中国科学院中国植被图编辑委员会. 100万中国植被图集[M]. 北京: 科学出版社, 2001.
[14] 鲍士旦. 土壤农化分析[M]. 北京: 中国农业出版社, 2000.
[16] 周李磊, 朱华忠, 钟华平, 等. 新疆伊犁地区草地土壤容重空间格局分析. 草业学报, 2016, 25(1): 64-75.
[18] 王绍强, 周成虎, 李克让, 等. 中国土壤有机碳库及空间分布特征分析. 地理学报, 2000, 55(5): 533-544.
[19] 曾全超, 李鑫, 董扬红, 等. 陕北黄土高原土壤性质及其生态化学计量的纬度变化特征. 自然资源学报, 2015, 30(5): 870-879.
[20] 杨阳, 刘秉儒, 杨新国, 等. 荒漠草原中不同密度人工柠条灌丛土壤化学计量特征. 水土保持通报, 2014, 34(5): 67-73.
[21] 青烨, 孙飞达, 李勇, 等. 若尔盖高寒退化湿地土壤碳氮磷比及相关性分析. 草业学报, 2015, 24(3): 38-47.
[23] 丁凡, 廉培勇, 曾德慧. 松嫩平原草甸三种植物叶片N、P化学计量特征及其与土壤N、P浓度的关系. 生态学杂志, 2011, 30(1): 77-81.
[24] 潘军, 宋乃平, 吴旭东, 等. 荒漠草原不同种植年限人工柠条林土壤碳氮磷化学计量特征. 浙江大学学报(农业与生命科学版), 2015, 41(2): 160-168.
[25] 王建林, 钟志明, 王忠红, 等. 青藏高原高寒草原生态系统土壤碳磷比的分布特征. 草业学报, 2014, 23(2): 9-19.
[26] 陶冶, 张元明. 古尔班通古特沙漠4种草本植物叶片与土壤的化学计量特征. 应用生态学报, 2015, 26(3): 659-665.
[27] 刘作云, 杨宁. 紫色土丘陵坡地不同恢复阶段土壤生态化学计量特征. 中国农学通报, 2015, 31(18): 163-167.
[28] 杨菁, 谢应忠, 吴旭东, 等. 不同种植年限人工苜蓿草地植物和土壤化学计量特征. 草业学报, 2014, 23(2): 340-345.
[29] 樊江文, 张良侠, 张文彦, 等. 中国草地样带植物根系N、P元素特征及其与地理气候因子的关系. 草业学报, 2014, 23(5): 69-76.
[30] 王春玲, 郭泉水, 谭德远, 等. 准噶尔盆地东南缘不同生境条件下梭梭群落结构特征研究. 应用生态学报, 2005, 16(7): 1224-1229.
[31] 王雪芹, 蒋进, 雷加强, 等. 古尔班通古特沙漠短命植物分布及其沙面稳定意义. 地理学报, 2003, 58(4): 598-605.
[33] 陈发虎, 黄伟, 靳立亚, 等. 全球变暖背景下中亚干旱区降水变化特征及其空间差异. 中国科学: 地球科学, 2011, 41(11): 1647-1657.
[34] 张生军, 王天明, 王涛, 等. 新疆近50a来降水量时空变化及其突变分析. 中国沙漠, 2010, 30(3): 668-674.

准噶尔荒漠区域尺度浅层土壤化学计量特征及其空间分布格

Regional-scale ecological stoichiometric characteristics and spatial distribution patterns of key elements in surface soils in the Junggar desert, Chin

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