1. 甘肃省荒漠化与风沙灾害防治国家重点实验室,甘肃,武威,733000
2. 甘肃民勤荒漠草地生态系统国家野外观测研究站, 甘肃 民勤,733300
3. 甘肃省治沙研究所,甘肃,兰州,730070
纸质出版:2019
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郭春秀, 安富博, 刘虎俊, 等. 青土湖人工输水区白刺群落结构及土壤特性研究[J]. 水土保持通报, 2019,39(6):44-51.
Guo Chunxiu, An Fubo, Liu Hujun, et al. Community Structure and Soil Characteristics of Nitraria Tangutorum in Artificial Water Transfer Area of Qingtu Lake[J]. Bulletin of Soiland Water Conservation, 2019, 39(6): 44-51.
郭春秀, 安富博, 刘虎俊, 等. 青土湖人工输水区白刺群落结构及土壤特性研究[J]. 水土保持通报, 2019,39(6):44-51. DOI: 10.13961/j.cnki.stbctb.2019.06.007.
Guo Chunxiu, An Fubo, Liu Hujun, et al. Community Structure and Soil Characteristics of Nitraria Tangutorum in Artificial Water Transfer Area of Qingtu Lake[J]. Bulletin of Soiland Water Conservation, 2019, 39(6): 44-51. DOI: 10.13961/j.cnki.stbctb.2019.06.007.
[目的] 对青土湖人工输水区白刺群落物种组成及土壤特性进行研究,以揭示研究区白刺灌丛生态系统的健康状况,为科学保育研究区灌丛沙堆以及生态恢复和防沙治沙工作提供科学依据。[方法] 通过野外植被调查和对距水面不同距离白刺沙堆的土壤理化特性进行分析研究。[结果] ①所调查群落中共有植物种18种,隶属6科17属,其中一年生草本8种,多年生草本6种,灌木植物4种,群落结构简单,物种相对单一。②距水面不同距离白刺群落0—60 cm土层土壤含水量,随着土层的加深呈现逐渐增加的趋势,随着距水面边缘距离的增加,白刺沙堆的土壤含水量逐渐降低,在200 m后趋于平稳;土壤机械组成主要以细砂粒为主,粗砂粒次之,黏粒含量相对较低;距水面0—100 m土层深度0—40 cm粗砂粒含量降低,黏粉粒含量较大。③青土湖人工输水区属于湖积沙区,土壤养分均属于严重缺乏,各养分含量均较低,且含量不均,土壤均处于偏碱性状态;土壤有机碳、全氮、速效钾含量表聚现象明显;距水面相同距离范围内土壤全磷、全钾、碱解氮和速效磷含量差异不显著(p>0.05),且随土层变化规律不明显。④有机碳含量与土壤全氮、全磷、速效钾、电导率之间呈显著正相关(p<0.05),电导率和全氮、全磷、速效钾之间呈极显著正相关(p<0.01),土壤有效养分含量与对应元素总含量相关性不显著(p>0.05)。[结论] 距青土湖水面不同距离植被群落结构简单,很多种为单属单科;水面形成区影响白刺沙堆土壤水分,增强细砂粒在近水面区域的沉降,土壤养分含量总体偏低,且含量不均,“表聚”现象明显。
[Objective] The species composition and soil characteristics of Nitraria tangutorum community in the artificial water transfer area of Qingtu Lake was studied
in order to reveal the health status of shrub ecosystem in the study area
and to provide scientific basis for scientific protection of shrub sand pile
ecological restoration and desertification control in the study area.[Methods] Based on field vegetation survey
the physical and chemical properties of soil at different distance from water surface were studied.[Results] ① There were 18 species of plants belonged to 6 families and 17 genera in the investigated community
including 8 species of annual herbs
6 species of perennial herbs and 4 species of shrub plants. The community structure was simple. ② The soil moisture content in 0-60 cm soil layer at different distances from the water surface showed a gradual increase trend with the increase of soil depth. As the distances were increased from the edge of the water surface
the soil moisture content of Nitraria tangutorum sand pile decreased gradually and became stable after 200 m. The mechanical composition of soil was mainly fine sand and coarse sand
and clay particle content iwas relatively low. From the water surface 0-100 m
the content of coarse sand was decreased in the 0-40 cm soil layer and the clay power particle content was great. ③ The artificial water transfer area of Qingtu Lake belonged to the area of fluvial sand
which was seriously deficient in the soil nutrients. The contents of all nutrients were low and uneven
and the soil was in a status of alkalinity. The accumulation of soil organic carbon
total nitrogen and rapidly available potassium was obvious. Within the same distance from the water surface
the content of total phosphorus
total potassium
alkali-hydrolyzed nitrogen and available phosphorus showed no siginificant difference(p>0.05)
and the change was not obvious with the increase of soil depth. ④There was a positive correlation between organic carbon content and soil total nitrogen
total phosphorus
available potassium and electrical conductivity(p<0.05)
and there was a significant positive correlation between electrical conductivity and total nitrogen
total phosphorus and available potassium(p<0.01)
while there was no significant correlation between soil available nutrient content and the total content of corresponding elements(p>0.05).[Conclusion] The vegetation community structure with different distance from water surface is simple
and many species belong to single genus and single family. Water surface formation area affects the soil water content of Nitraria tangutorum sand pile
and enhances the settlement of fine sand particles in the area near water surface. Soil nutrient content is generally low and uneven
and the phenomenon of "surface accumulation" is obvious.
唐艳,刘连友,杨志鹏,等.毛乌素沙地南缘灌丛沙丘土壤水分与粒度特征研究[J].水土保持研究,2009,16(2):6-10.
Tengberg A. Nebkha dunes as indicators of wind erosion and land degration in the Sahel zone of Burkina Faso[J]. Journal of Arid Environment, 1995,30(3):265-282.
司建华,冯起,常宗强,等.阿拉善雅布赖风沙区荒漠植物群落结构和物种多样性研究[J].西北植物学报,2011,31(3):602-608.
李保军.植物群落结构的稳定性与复杂性[J].中国草业科学,1988,4(3):16-18.
张凯,冯起,吕永清,等,司建华.石羊河下游民勤湖区土壤特性和空间分异研究[J].土壤,2012,44(5):838-845.
新疆维吾尔自治区土壤普查办公室编.新疆土壤[M].北京:科学出版社,1996,407.
董治宝,李振山.风成沙粒度特征对其风蚀可蚀性的影响[J].水土保持学报,1998,4(4):1-12.
陈广庭.北京平原土壤机械组成和抗风蚀能力的分析[J].干旱区资源与环境,1991,5(1):103-113.
Orlovsky L, Orlovsky N, Durdyev A. Dust storms in Turkmenistan[J]. Journal of Arid Environment, 2005,60(1):83-97.
Singer A, Zobeck T, Poberezsky L, et al. The PM10 and PM2.5 dust generation potential of soils/sediments in the Southern Aral Sea Basin, Uzbekistan[J]. Journal of Arid Environments, 2003,54(4):705-728.
王军,傅伯杰,将小平.土壤水分异质性的研究综述[J].水土保持学报,2002,16(1):1-5.
熊顺贵.基础土壤学[M].北京:中国农业大学出版社,2001.
王洪杰,李宪文,史学正,等.不同土地利用方式下土壤养分的分布及其与土壤颗粒组成关系[J].水土保持学报,2003,17(2):44-50.
Li Xinrong. Influence of variation of soil spatial heterogeneity on vegetation restoration[J]. Science in China(D):Earth Sciences, 2005,48(11):2020-2031.
张继义,王娟,赵哈林.沙地植物恢复过程土壤颗粒组成变化及其空间变异特征[J].水土保持学报,2009,23(3):153-157.
石瑞香,杨小唤,王立新.伊犁新垦区土壤养分特征与土地开垦的方向探讨[J].资源科学,2009,31(12),2016-2023.
潘晓玲,沈观冕,陈鹏.白刺属植物的分类学及系统学研究[J].云南植物研究,1999,21(3):287-295.
张远东,潘晓玲,顾峰雪,等.阜康荒漠植被灌丛种群生态位的研究[J].植物生态学报,2001,25(6):741-745.
张萍,哈斯,岳兴玲,等.白刺灌丛沙堆形态与沉积特征[J].干旱区地理,2008,31(6):926-932.
贾宝全,蔡体久,高志海,等.白刺灌丛沙包生物量的预测模型[J].干旱区资源与环境,2002,16(1):96-99.
熊小刚,韩兴国,白永飞,等.锡林河流域草原小叶锦鸡儿分布增加的趋势、原因和结局[J].草业学报,2003,12(3):57-62.
靳虎甲,马全林,张有佳,等.石羊河下游白刺灌丛演替发育过程的土壤呼吸及其影响因素分析[J].中国沙漠,2012,32(1):140-147.
孙涛,韩富贵,安富博,等.民勤绿洲过渡带白刺沙堆土壤呼吸空间异质特性[J].草业科学,2017,34(4):673-684.
石万里,刘淑娟,刘世增,等.人工输水对石羊河下游青土湖区生态环境的影响分析[J].生态学报,2017,37(18):5951-5960.
李银科,刘世增,刘虎俊,等.石羊河流域中下游沙漠-河岸过渡带土壤特征研究[J].水土保持研究,2012,19(6):29-35.
刘淑娟,袁宏波,刘世增,等.石羊河尾闾水面形成区土壤颗粒的分形特征[J].水土保持通报,2013,33(6):285-289.
刘淑娟,袁宏波,刘世增,等.石羊河尾闾(青土湖)水面形成后土壤养分的空间特征[J].土壤,2015,47(6):1068-1075.
韩福贵,孙涛,郭树江,等.干旱荒漠区不同演替阶段白刺灌丛沙堆土壤呼吸特征及其影响因素分析[J].西北林学院学报,2017,32(5):1-7.
中国科学院土壤研究所.土壤理化分析[M].上海:上海科学技术出版社, l978.
席军强,杨自辉,郭树江,等.不同类型白刺沙丘土壤理化性状与微生物相关性研究[J].草业学报,2015,24(6):64-74.
党荣理,潘晓玲.西北干旱荒漠区种子植物科的区系分析[J].西北植物学报,2002,22(1):24-32.
宋永昌.植被生态学[M].上海:华东师范大学出版社,2001.
郝文芳,杜峰,陈小燕,等.黄土丘陵区天然群落的植物组成、植物多样性及其与环境因子的关系[J].草地学报2012,20(4):609-615.
郭泉水,江洪,王兵,等.中国主要森林群落植物生活型谱的数量分类及空间分布格局的研究[J].生态学报,1999,19(4):573-577.
杨自辉,俄有浩,方峨天,等.民勤绿洲边缘物种多样性对水资源变化的响应[J].中国沙漠,2007,27(2):278-282.
李雪华,李晓兰,蒋德明,等.干旱半干旱荒漠地区一年生植物研究综述[J].生态学杂志,2006,25(7):851-856.
徐宝国,贺访印,刘勤先.民勤荒漠白刺群落的分布与结构特征研究[J].甘肃林业科技2013,38(2):1-6.
黄昌勇.土壤学[M].北京:中国农业出版社,2000.
王家强,韩路,柳维扬,等.塔里木河中游荒漠绿洲过渡带土壤水分与植被空间格局变化关系研究[J].西北林学院学报,2018,33(1):1-10.
孙祥,于卓.白刺根系的研究[J].中国沙漠,1992,12(4):50-54.
贾晓红,李新荣,陈应武.腾格里沙漠东南缘白刺灌丛地土壤性状的特征[J].干旱区地理,2007,30(4):557-564.
马成忠,邓继峰,丁国栋,等.不同初植密度樟子松人工林对毛乌素沙地南缘土壤粒度特征的影响[J].水土保持学报,2017,31(1):230-235.
刘淑娟,袁宏波,李发明,等.青土湖水面形成区土壤颗粒组成与化学特性变化[J].草业科学.2015(12):1953-1959.
施祺,王建民,陈发虎.石羊河古终端湖泊沉积物粒度特征与沉积环境初探[J].兰州大学学报:自然科学版,1999,35(1):194-198.
刘强,游海涛,刘嘉麒.湖泊沉积物年纹层的研究方法及其意义[J].第四纪研究,2004,24(6):684-694.
Su Yan, Qiu Quan, He Qian, et al. On spatial variability and distribution of soil nutients in different Nitraria tangutorum bobr, populations in Tsaidam basin[J]. Agriculture Science & Technology,2015,16(2):285-291.
樊瑞霞.白刺灌丛堆土壤-植被空间变化特征及相关关系研究[D].宁夏银川:宁夏大学,2016.
比拉力·依明,王勇辉,海米提·依米提.博尔塔拉河下游河岸带土壤养分特征及其相关性分析[J].干旱区研究,2014,31(2):216-221.
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