地球科学进展 ›› 2002, Vol. 17 ›› Issue (2): 262 -267. doi: 10.11867/j.issn.1001-8166.2002.02.0262

中国典型地区土地利用变化对生态系统的影响机制 上一篇    下一篇

风沙流对植物生长影响的研究
于云江 1,2,史培军 1,贺丽萍 3,刘家琼 2   
  1. 1.北京师范大学环境演变与自然灾害教育部重点实验室,北京师范大学资源科学研究所,北京 100875;2.中国科学院寒区旱区环境与工程研究所沙坡头沙漠试验研究站,甘肃兰州 730000;3.内蒙古伊盟林业处,内蒙古 东胜 017000
  • 收稿日期:2001-12-07 修回日期:2001-12-28 出版日期:2002-12-20
  • 通讯作者: 于云江(1964-).男,内蒙古乌前旗人,博士研究生,主要从事干旱区资源与植物生态生理研究.E-mail:yyj@irs.bnu.edu.cn E-mail:yyj@irs.bnu.edu.cn
  • 基金资助:

    国家重点基础研究发展规划项目“中国北方沙漠化过程及其防治研究”(编号:G2000048701);国家重点基础研究发展规划项目“草地与农牧交错带生态系统重建机理及优化生态—生态范式”(编号:G2000018604);中科院沙坡头沙漠试验站开放基金(200021);教育部骨干青年教师基金资助.

RESEARCH ON THE EFFECTS OF WIND-SAND CURRENT ON THE PLANT GROWTH

YU Yun-jiang 1,2,  SHI Pei-jun 1, HE Li-ping 3, LIU Jia-qiong 2   

  1. 1.Institute of Resource Science, Key laboratory of Environmental Change and Natural Disaster, Ministry of Education of China, Beijing Normal University, Beijing 100875, China;2.Desert Experimental Research Station at Shapotou, Institute of Cold and Arid Regions Environment and Engineering,  CAS,Lanzhou 730000, China; 3.Forestry Department, Yikezhaomen Region, the Inner Mongolia Autonomous,Dong Sheng 017000,China
  • Received:2001-12-07 Revised:2001-12-28 Online:2002-12-20 Published:2002-04-01

在中国乃至全球,风沙活动都十分频繁,它直接影响着风沙地区植物资源的可持续利用与发展,因此,研究风沙流对植物生长的影响十分必要。以往,相关的研究主要是围绕沙漠逆境的综合条件(如降水、温度、湿度、土壤水分、养分等综合因子)进行的,研究内容涉及植物的生理、生化、物质代谢以及生态适应性等。但国内外就风沙流单因子对植物生理生化影响的研究还没有深入展开,为此,作者利用野外风洞条件,就不同风况下的风沙胁迫对某些植物生长特征的影响进行了实验研究;结果表明:风沙流胁迫可使植物的净光合速率(Pn)、气孔导度(Cs)、叶温(Tl)、叶片水势(Wp)降低,使蒸腾速率(Tr)升高;且风速越大,吹风间隔越短,这些参数变幅越大;风沙流比净风的影响更大。风沙流能降低试验植物的水分利用率,进而增加植物的干燥作用;同时可使脯氨酸含量增加。由于风沙流运动和植物的复杂多样性,因此这个研究领域还有许多问题需要探索。

Blown Sand is frequent in China and even the globe, it affects the sustained utilization and development of botanical resource, thus it is essential to study on the effects of the blown sand on plant. In the past time, concerned research mainly comprised plant physiology, substance metabolizing and its adaptability under integrated factor of the desert instead of single wind-sand current factor, thus the author study on the effects of the blown sand on the growth characteristics of some plants in different windy condition by the field wind tunnel. The results showed: Wind and wind-sand current made net photosynthetic ratio(Pn), stomata conductance(Cs),  leaf temperature (Tl),leaf water potential (Lwp) decrease, made transpiration ratio(Tr) rise. The larger the windy velocity was or the shorter the interval of  blown sand was, the larger the changes of the above indexes was, and the effects of wind-sand current on above indexes were more fiercely than pure wind;  wind-sand stress made the plants experimented proline acid cumulate; because of decreasing water use efficiency (Wue), wind-sand current aggravated desiccation on plants; because of diversity and complexity of plant and blown sand movement, there were many further problems to study about effect of blown sand on plant growth.

中图分类号: 

[1]Edwin D Mckee. A Study of Global Sand Seas[M].Yinchuan: Ningxia people’s press, 1993.[Edwin D.Mckee主编.世界沙海的研究[M].赵兴梁译.银川:宁夏人民出版社,1993.]
[2]Shi Peijun,Zhang Hong, Wang Ping,et al. The regional patterns for combating sandification in sandy disaster affected areain china[J]. Journal of Natural Disasters, 2000,9(3):1-7 .[史培军,张宏,王平,等. 我国沙区防沙治沙的区域模式[J]. 自然灾害学报,2000,9(3):1-7.]
[3]Zhu Zhenda. Phenomena of blownsands and their impacts on lands in humid and subhumid zones[J].Journal of Desert Research.1986,6(4):1-10.[朱震达.湿润及半湿润地带的土地风沙化问题[J].中国沙漠,1986,6(4):1-10.]
[4]Bagnold B A. The Physics of Blown Sand and Desert Dunes[M]. Beijing: science press,1987.18-67.[拜格诺 B A风沙和荒漠沙丘物理学[M].钱宁,等译.北京:科学出版社,1959.7-171.]
[5]Wu Zheng. Blown Sand Physiognomy[M].Beijing: Science Press.1987.18-67.[吴正编著.风沙地貌学[M].北京:科学出版社,1987.18-67.]
[6]Wu Zheng,Ling Yuquan. Primary studies on some rule of blown sand movement and controlling sand research on controlling-sand[J].Research on Sand-Control,1965,(7):7-14.[吴正,凌裕泉.风沙运动的若干规律及防止风沙危害问题的初步研究[J].治沙研究,1965,(7): 7-14.]
[7]Kadib A A. A Function for Sand Movement by Wind[M].ASTTA, 1965.
[8]Shi Peijun, Wang Jing’ai.  Statistical analysis of granularity of aeolian sand in Chinese arid and semi-arid desert area[J]. Acta Scientia rum Unive rsitatis Nei Mongol(Natural  Science),1986,(4):12-20.[史培军,王静爱.中国干旱、半干旱沙区风成沙粒度的统计分析[J].内蒙古师大学报(自然科学版),1986,(4):12-20.]
[9] Ling Yuquan. Principle of physics of blown sand on railway sand-controlling for example, baotou-lanzhou railway[A]. In: Research on Fluid Sand at Shapotou Area at the Southeastern Edge of Tengger Desert (2)[C].Yinchuan: Ningxia People’s Publishing House,1988.297-308.[凌裕泉.铁路沙害治理体系的风沙物理学原理——以包兰铁路为例[A].见:腾格里沙漠沙坡头地区流沙治理研究(二)[C].银川:宁夏人民出版社,1988.297-308.]
[10]Liu Kaichang,Zhang Xiuqing,Wang Qingcheng,et al. Effect of plant of density on microclimate in canopy of maize[J].Acta Phytoecological Sinica,2000,24(4):489-493.[刘开昌,张秀清,王庆成,等.密度对玉米群体冠层内小气候的影响[J].植物生态学报,2000,24(4):489-493.]
[11]Dong  Xuejun. Study on water physiology and ecology feature of several fixing-sand[J].  Acta Phytoecologica Sinica, 1994,18(1):84-94.[董学军.几种沙生植物水分生理生态特征的研究[J].植物生态学报,1994,18(1):84-94.]
[12]Liu Xinmin,Pu Jinchun, Liu Jiaqiong,et al. Water relation of some sand fixing plant species and xerophtes in the middle part of the Hexi corridor, Gansu Province[J].Journal of Desert Research,1986,6(4):23-33.[刘新民, 蒲锦春,刘家琼,等.几种固沙植物的水分关系[J].中国沙漠,1986,6(4):23-33.]
[13]Liu Jiaqiong,Pu Jingchun,Liu Xinmin. Comparative studies on water relations and xeromorphic structures of some plant species in the middle part of the desert zone in China[J]. Acta Bot Sin,1987,29:662-673.[刘家琼,蒲锦春,刘新民.我国沙漠中部地区主要不同生态类型植物的水分关系和旱生结构的比较研究[J].植物学报,1987,29(6):662-673.]
[14]Huang Zichen. Study on ecology and physiology of desert plant[A]. In: Research on Fluid Sand at Shapotou Area at the Southeastern Edge of Tengger Desert (2) [C].Yinchuan:Ningxia People’s Publishing House, 1988.27-57.[黄子琛.荒漠植物的生态生理研究[A].见:腾格里沙漠沙坡头地区流沙治理研究(二)[C].银川:宁夏人民出版社, 1988.27-57.]
[15]Luo Shiming,Chen Yuhua. Agricultural Ecology[M].Chang Sha: Hunan Publishing House of Science and Technology, 1987.49-84, 151-152.[骆世明,陈聿华. 农业生态学[M].长沙: 湖南科学技术出版社,1987 .49-84, 151-152]
[16]Wang Zhuhao. Plant and Environment[M].Beijing: Science Press,1986.60-64.[王铸豪主编.植物与环境[M].北京:科学出版社,1986.60-64.]
[17]Freas K E, Kemp K R. Some relationships between environmental reliability and seed dormancy in desert annual plants[J].Journal   of Ecology,1983,71:211-217.
[18]Pamadusa M A, Lovell P H. Interference in population of some dune annuals[J].  Ecology, 1981,62:855-866
[19]Inouye R S. Population biology of desert annual plants, in the ecology of desert communities(Polis G S,ed. ) [M]. Arizona: The University of Arizona,1991.24-54
[20]Griddings L A. Transpiration of silphium Laciniatam[J]. Plant World, 1914,35:937-942.
[21]Pan Ruizhi, Dong Yude. Plant Physiology[M]. Beijing:High Education Press,1984.17-24,132.[潘瑞炽,董愚得编著.植物生理学(上册) [M].北京:高等教育出版社,1984.17-24,132.]
[22]Bjorkman O.Comparative studies on photosynthesis in higher plants[A]. In; Giese A, ed. Comparative Plant Ecophysiology[C]. New York: Academic Press, 1973.231-268.
[23]Schulze E D.Carbon dioxide and water vapour exchange in response to drought in the atmosphere and in the soil[J].Ann Rev Plant Physiol,1986,37:247.
[24]Raiser W M. Effects of  water deficit on photosynthesis capacity[J] .Plant Physiol,1987,71:142.
[25]Wang Suoming , Zhu Xingyun,  Wang Zengrong . Initial research of function of seeping adjustment of puccinellia distans in adapting to salt adversity[J].  Acta Grass Sinica, 1993,2(3):40-46.[王锁民,朱兴运,王增荣.渗透调节在碱茅幼苗适应盐逆境中的作用初探[J].草业学报1993,2(3):40-46.]
[26]Iliha L, Porffling K.Changes in abscisia acid and proline levels in maize varieties of different drought resistance[J].Physiol Plant,1985,55:129-135.
[27]Bates L S, Walddren, R P,Teare I D. Rapid determination of free proline for water stress studies[J].  Plant and Oil,1973,39:205-207.
[28]Handa S, Handa A K, Hasegaw P M, et al. Proline accumulation and the adaptation of cultured plant cell to water stress[J]. Plant Physiol, 1986,80:938-945.
[29]Zhao Xingliang. Research on problem of controlling-sand of vegetable[A] . In: Research on Fluid Sand at Shapotou Area at the Southeastern Edge of Tengger Desert (2)[C]. Yinchuan: Ningxia People’s Publishing House, 1988.[赵兴梁.沙坡头地区植物固沙问题的探讨[A].见:腾格里沙漠沙坡头地区流沙治理研究(二)[C]. 银川:宁夏人民出版社,1988.]
[30]Qiu Guoyu, Shi Qinghui. Moisture Dynamic of sand dune and succesional characteristics of artificial vegetation in the Shapotou area [A]. Annual Report Shapotou Desert Experimental Research Station Lanzhou Research Institute, Academia Sinica[C].Lanzhou: Gansu Publishing House of Science and Technology,1993.120-129.[邱国玉,石庆辉.腾格里沙漠东南缘沙坡头段水分动态和植被演替[A].见:中国科学院沙坡头沙漠试验研究站年报[C].兰州:甘肃科学技术出版社,1993.120-129.]
[31]Wang Gang,Liang Xuegong. The seed bank dynamic of artificial plant community in Shapotou area [J].Acta Botanica Sinica,1995,37(3):231-237. [王刚,梁学功.沙坡头人工固沙区种子库动态[J]. 植物学报, 1995,37(3):231-237.]
[32]Feng Jinzhao,Chen Hesheng. Studies on sand-fixing plants’ utilization for precipitation and its physiology and ecology[J]. Acta  Ecologica Sinica,1994,14(3):231-237.[冯锦朝,陈荷生.沙生植物对降水资源的利用及生理生态研究[J].生态学报,1994,14(3):231-237.]
[33]Zhang Liping, Wang Xinping, Liu Lichao,et al. Study on gas exchange characteristics of main constructive plants [WT6BX]A.ordosica[WT6BZ] and [WT6BX]C.korshinskii[WT6BZ] in shaptou region[J]. Acta Ecologica Sinica, 1998,18,(2):133-137.[张利平,王新平,刘立超,等.沙坡头主要建群植物油蒿和柠条的气体交换特征研究[J].生态学报,1998,18(2):133-137.]
[34]Yu Yunjiang, Xin Yueyong, Liu Jiaqiong, et al.  Effects of wind-sand current on the physiological status of different sand-fixing Plants[J] .Acta Botanica Sinica,1998,40(10):962-968.[于云江,辛越勇,刘家琼,等.风和风沙流对不同固沙植物生理状况的影响[J]. 植物学报,1998,40(10):962-968.]
[35]Zhu Zhenda,Liu Shu,Di Xingming.Development and harness of land desertificationin in China[A] .In: Paper Collection of Chinese Academy Desert Research Institute in Lanzhou[C]. 1986.[朱震达,刘恕,邸醒民.中国土地沙漠化发生发展及其整治[A].见:中国科学院兰州沙漠所集刊[C]. 1986.] 
[36]Shi Peijun,Yan Ping,Gao Shangyu, et al .The duststorm disaster in china and its research progress[J]. Journal of Natural Disasters,2000,9(3):71-77.[史培军,严平,高尚玉,等. 我国沙尘暴灾害及其研究进展与展望[J].自然灾害学报,2000,9(3):71-77.]

[1] 李耀辉, 孟宪红, 张宏升, 李忆平, 王闪闪, 沙莎, 莫绍青. 青藏高原—沙漠的陆—气耦合及对干旱影响的进展及其关键科学问题[J]. 地球科学进展, 2021, 36(3): 265-275.
[2] 董治宝, 李超, 吕萍, 胡光印. 侵蚀型沙丘:来自火星的启示[J]. 地球科学进展, 2021, 36(2): 125-138.
[3] 车雪华, 罗万银, 邵梅, 王中原. 青海共和盆地不同发育阶段风蚀坑表面气流场与形态反馈研究[J]. 地球科学进展, 2021, 36(1): 95-109.
[4] 董治宝,吕萍,李超,胡光印. 火星风条痕特征及其形成机制[J]. 地球科学进展, 2020, 35(9): 902-911.
[5] 董治宝,吕萍,李超. 火星风沙地貌研究方法[J]. 地球科学进展, 2020, 35(8): 771-788.
[6] 董治宝,吕萍,李超,胡光印. 火星独特风沙地貌之横向沙脊[J]. 地球科学进展, 2020, 35(7): 661-677.
[7] 董治宝,吕萍,李超,胡光印. 火星大沙波纹特征及其形成机制[J]. 地球科学进展, 2020, 35(10): 1006-1015.
[8] 张克存, 屈建军, 鱼燕萍, 韩庆杰, 王涛, 安志山, 胡菲. 中国铁路风沙防治的研究进展[J]. 地球科学进展, 2019, 34(6): 573-583.
[9] 屈建军,凌裕泉,刘宝军,陈广庭,王涛,董治宝. 我国风沙防治工程研究现状及发展趋势[J]. 地球科学进展, 2019, 34(3): 225-231.
[10] 董治宝,吕萍. 深空探测时代的风沙地貌学[J]. 地球科学进展, 2019, 34(10): 1001-1014.
[11] 柳本立,牛百成,屈建军. 多组复合指纹示踪法及其应用[J]. 地球科学进展, 2019, 34(10): 1092-1098.
[12] 董玉祥,张青年,黄德全. 海岸风蚀地貌研究进展与展望[J]. 地球科学进展, 2019, 34(1): 1-10.
[13] 张克存, 安志山, 蔡迪文, 郭紫晨, 王军战. 沙漠—绿洲过渡带近地表风沙过程研究进展[J]. 地球科学进展, 2015, 30(9): 1018-1027.
[14] 王训明, 周娜, 郎丽丽, 花婷, 焦琳琳, 马文勇. 风沙活动对陆地生态系统影响研究进展[J]. 地球科学进展, 2015, 30(6): 627-635.
[15] 张正偲, 董治宝. 风沙地貌形态动力学研究进展[J]. 地球科学进展, 2014, 29(6): 734-747.
阅读次数
全文


摘要