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荒漠区药用植物黑果枸杞研究现状综述 被引量:15
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作者 王方琳 王祺 +7 位作者 李爱德 尉秋实 柴成武 胡小柯 王昱淇 汪媛艳 杨晓寒 靳承东 《中国水土保持》 2019年第5期57-60,共4页
黑果枸杞是我国西北干旱地区特有的兼具耐盐碱和抗旱特性的野生灌木,可正常生长于大多植物无法生长的高盐渍化环境中,并发挥其生态效益;此外,黑果枸杞同时具备药用、食用功效,已被应用于饮料、保健品、药品等诸多行业,具有广阔的市场前... 黑果枸杞是我国西北干旱地区特有的兼具耐盐碱和抗旱特性的野生灌木,可正常生长于大多植物无法生长的高盐渍化环境中,并发挥其生态效益;此外,黑果枸杞同时具备药用、食用功效,已被应用于饮料、保健品、药品等诸多行业,具有广阔的市场前景。丰富的营养价值、良好的经济价值及潜在的药用价值,使黑果枸杞野生资源受到大规模掠夺性开采,天然分布区环境日益恶劣,植被严重退化甚至死亡,其他伴生植物的生长也受到很大的威胁,野生居群的规模及分布区域呈迅速减小的趋势,其资源远远不能满足市场的需求。对荒漠区黑果枸杞现阶段研究成果进行了综合分析。 展开更多
关键词 黑果枸杞 研究现状 荒漠区
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灌溉对退化唐古特白刺植被生长的影响
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作者 李雪娇 李爱德 +2 位作者 柳小平 徐先英 刘克彪 《防护林科技》 2023年第4期7-10,共4页
结合天然白刺(Nitraria tangutorum)灌丛接种培育锁阳药材,通过滴灌、渗灌、喷灌方式对白刺灌丛进行不同方式和不同灌溉量的试验,结果表明:随着灌溉量的增加,白刺林地土壤含水率提高显著,灌溉对提高白刺植被生长恢复效果明显。无灌溉白... 结合天然白刺(Nitraria tangutorum)灌丛接种培育锁阳药材,通过滴灌、渗灌、喷灌方式对白刺灌丛进行不同方式和不同灌溉量的试验,结果表明:随着灌溉量的增加,白刺林地土壤含水率提高显著,灌溉对提高白刺植被生长恢复效果明显。无灌溉白刺灌丛当年生枝条平均生长量为4 cm,灌丛内当年生枝叶生物量平均为0.109 kg;滴灌灌溉白刺灌丛当年生枝条平均生长量为14 cm,灌丛内当年生枝叶生物量平均为0.382 kg;喷灌灌溉白刺灌丛当年生枝条平均生长量为16 cm,灌丛内当年生枝叶生物量平均为0.845 kg;渗灌方法可使灌溉水分充分下渗到植物根系层土壤中,灌溉完成后地表0~<20 cm厚度范围内土壤水分含量在3%以下,与地表滴灌和喷灌相比较,较大地减少了地表水分蒸发损失。3种灌溉方式都能明显提高0~<60 cm深度范围内的土壤水分含量,灌水入渗深度渗灌>滴灌>喷灌。灌溉后土壤表层土壤含水率差异较大,滴灌和喷灌方式的0~<20 cm深度的土壤含水率较大,渗灌方式0~<20 cm深度的土壤含水率较小。因此,渗灌方式灌溉白刺灌丛地表蒸发较小,灌溉水的利用率较高。 展开更多
关键词 唐古特白刺 灌溉 植被恢复
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Canonical Correlation Factors Causing the Formation of Accumulated Sand-belts along the Oasis Fringe in Hexi Corridor
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作者 Chang Zhaofeng Wang Qiangqiang +7 位作者 Zhang Jianhui Tang Jinnian Zhu Shujuan Fan Baoli Zhang Dabiao liu Shizeng Zhang Guozhong li aide 《Animal Husbandry and Feed Science》 CAS 2014年第5期279-284,共6页
Accumulated sand-belts refer to those formed along the oasis fringe,especially at the upwind location,due to the accumulation of sand blocked by farmland windbreak. In the 60 years since the foundation of new China,a ... Accumulated sand-belts refer to those formed along the oasis fringe,especially at the upwind location,due to the accumulation of sand blocked by farmland windbreak. In the 60 years since the foundation of new China,a lot of trees have been planted for desertification combating in northwest and north China,thus,accumulated sand-belts were formed at the upwind location. The formation and the ecological effects of the accumulated sand-belts along the oasis fringe is a new scientific concern. To study the formation causes of these belts in Hexi corridor,21 samples were selected,and the height / width of the belts,as well as the vegetation,soil,soil moisture and climatic factors were investigated. This paper analyzed the correlation between the height / width of the belts and the vegetation,soil,soil moisture and climatic factors using the methods of variance analysis,correlation analysis and canonical correlation analysis. The results indicate that: the accumulated sand-belts take a trend of being high and wide in the east whereas low and narrow in the west,and most of the parts tend to be stable; the species on the belts are dominated by Tamarix austromongolica,the vegetation cover and the pure vegetation cover of different dominant species on the leeward slope of the accumulated sand-belts vary significantly. The canonical correlation analysis shows that: the height and width of accumulated sand-belt is the interaction of precipitation,distance to the sand source,leeward vegetation cover and annual average wind speed. Moreover,the height of accumulated sand-belts are negatively correlated to the soil moisture at the depth of 30- 50 cm,air humidity and leeward vegetation cover,and the width of the belts is also negatively correlated with the distance to the sand source. The ecological effects of the accumulated sand-belts are both positive( stopping sands from moving into farmland,protective role as an obstacle)and negative( when the belts decay and activate one day,they will become the new sand sources). At present,there are no signs showing the negative effects of the belts. The ecological effects of the accumulated sand-belts are: firstly the protective role as an obstacle,and secondly to intercept and reduce the sands moving into farmlands. 展开更多
关键词 Height of accumulated sand-belt Width of accumulated sand-belt Climatic and environmental factors Canonical correlation factors Ecological effects Hexi of Gansu
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Characteristics of the lower layer of sandstorms in the Minqin desert-oasis zone 被引量:9
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作者 ZHAO Ming ZHAN KeJie +7 位作者 YANG ZiHui FANG ErTian QIU GuoYu WANG QiangQiang ZHANG YinChang GUO ShuJiang li aide ZHANG JingChun 《Science China Earth Sciences》 SCIE EI CAS 2011年第5期703-710,共8页
By measuring the sand-dust flux,vertical deposition,and the wind velocity throughout 19 sandstorms in the Minqin region,we quantitatively analyzed the horizontal distribution and vertical variation in sandstorm charac... By measuring the sand-dust flux,vertical deposition,and the wind velocity throughout 19 sandstorms in the Minqin region,we quantitatively analyzed the horizontal distribution and vertical variation in sandstorm characteristics under different land cover conditions.The effect of different land cover on mitigating sandstorms was also investigated.The results indicated that,in the surface layer ranging from 0-50 m,the intensity of sand-dust horizontal flux and concentration of sand-dust decreased with the increase of the height in the desert and the edge of oasis,whereas the two physical quantities increased slightly with the increase of the height in the oasis.The two physical quantities obey power function well under all three cover conditions.Moreover,in the desert and at the edge of oasis,the sand-dust vertical deposition decreased with the increase of the height.But a partial unimodal distribution at the oasis site and the maximum deposition occurred at the height of 9 m,which corresponds to the middle height of farmland protection forest.The annual flux that passed through a section of 1 m in width and 50 m in height was 9169 kg in the desert,5318 kg at the edge of oasis,and 2345 kg in the oasis.And the annual fluxes at the edge of oasis and in the oasis are 42% and 74% less,respectively,than that in the desert.This implies that the wind break forest significantly reduced the intensity of sandstorms. 展开更多
关键词 Minqin the lower layer sand-dust horizontal flux vertical deposition
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