1. 河北师范大学 资源与环境科学学院 河北省环境演变与生态建设省级重点实验室,河北,石家庄,050024
2. 河北省科学院 地理科学研究所,河北,石家庄,050011
3. 保定长城汽车股份有限公司,河北,保定,071000
纸质出版:2016
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胡国云, 郭中领, 王仁德, 等. 河北坝上低山区坡地灌丛沙堆表面土壤理化性质[J]. 水土保持通报, 2016,36(4):315-319.
HU Guoyun, GUO Zhongling, WANG Rende, et al. Soil Physical and Chemical Properties of Nebkhas on Slopes in Bashang Region of Hebei Province[J]. Bulletin of Soiland Water Conservation, 2016, 36(4): 315-319.
胡国云, 郭中领, 王仁德, 等. 河北坝上低山区坡地灌丛沙堆表面土壤理化性质[J]. 水土保持通报, 2016,36(4):315-319. DOI: 10.13961/j.cnki.stbctb.2016.04.054.
HU Guoyun, GUO Zhongling, WANG Rende, et al. Soil Physical and Chemical Properties of Nebkhas on Slopes in Bashang Region of Hebei Province[J]. Bulletin of Soiland Water Conservation, 2016, 36(4): 315-319. DOI: 10.13961/j.cnki.stbctb.2016.04.054.
[目的] 揭示河北省坝上地区低山坡地不同坡向和坡位小叶锦鸡灌丛沙堆土壤理化性质变化规律,为坡地草地生态环境稳定提供理论依据。[方法] 基于对山坡638个灌丛沙堆野外测量和86个室内土样分析的数据,运用地统计学和样品室内分析的方法。[结果](1)从低山坡脚到坡顶,灌丛沙堆pH值、粗砂、中砂和细砂总含量逐渐减少,粉砂、极细砂逐渐增加;有机质、全氮和全磷含量逐渐增加。(2)迎风坡不同坡位上灌丛沙堆表面颗粒中粗砂、中砂、细砂总含量大于背风坡相同坡位,极细砂和粉砂小于背风坡相同坡位。表面的土壤养分(有机质、全氮和全磷)为迎风坡坡脚大于背风坡坡脚,迎风坡坡中和坡顶的灌丛沙堆土壤养分含量小于背风坡坡中和坡顶灌丛沙堆,但是pH值变化与灌丛沙堆养分变化趋势相反。[结论] 受坡位和坡向的影响,灌丛沙堆土壤理化性质空间分布具有一定的差异性。
[Objective] The soil physical and chemical properties of Caragana Nebkhas were analyzed in different slope position and slope direction at the he Bashang area of Hebei Province in order to keep the slope eco-environment stabile . [Methods] Investigation data of 638 nebkhass and assay data of 86 soil samples were analyzed by geo-statistics. [Results] From the top to the foot of the investigated hills
contents of coarse sand
medium sand and fine sand and pH value gradually decreased
whereas
contents of clay
silt
organic matter
total N and total P showed an increased trend. Soil particle composition was different for slope wind exposure
the contents of coarse sand
medium sand and fine sand in the windward slope of nebkhas were greater than the corresponding values in the leeward slope; Comparatively
contents of very fine sand and silt were less than that in the leeward slope. Soil nutrients(organic matter
total N and total P content) in the foot of windward slope were greater than that in the foot of leeward slope; However
in the middle and top of the windward slope were less than the corresponding values of the leeward slope. pH value had a reverse trend. [Conclusion] Soil properties of nabkhas are different in different slope positions and directions resulted from wind-involved pedogenesis.
康玉梅.河北坝上缓坡耕地土壤风蚀特征研究[D].河北 石家庄:河北师范大学,2013.
武胜利,李志忠,惠军,等.和田河流域灌(草)丛沙堆的形态特征与发育过程[J].地理研究,2008,27(2):314-322.
杜建会,严平,俄有浩.甘肃民勤不同演化阶段白刺灌丛沙堆表面理化性质研究[J].中国沙漠,2009,29(2):248-253.
张展赫,来风兵,陈蜀江,等.和田河西侧胡杨沙堆的三维形态特征及空间自相关性[J].水土保持研究,2015,22(3):137-149.
贾晓红,李新荣.腾格里沙漠东南缘不同生境白刺(
Nitraria
)灌丛沙堆的空间分布格局[J].环境科学,2008,29(7):2046-2053.
杨帆,王雪芹,何清,等.绿洲-沙漠过渡带柽柳灌丛沙堆形态特征及空间分布格局[J].干旱区研究,2014,31(3):556-563.
崔楠,吕光辉,刘晓星,等.胡杨、 梭梭群落土壤理化性质及其相互关系[J].干旱区研究,2015,32(3):476-482.
苏永中,赵哈林,张铜会.几种灌木、半灌木对沙地土壤肥力影响机制的研究[J].应用生态学报.2002,13(7):802-806.
陈鸿洋.荒漠区红砂灌丛"肥岛"效应及其固碳特征[D].甘肃 兰州:兰州大学,2014.
郑敬刚,张本昀,何明珠,等.灌丛化对贺兰山西坡草场土壤异质性的影响[J].干旱区研究,2009,26(1):26-30.
Hesp P, Mclachlan A. Morphology, dynamics, ecology and fauna of
Arctotheca populifolia
, and
Gazania
rigens, nabkha dunes[J]. Journal of Arid Environments, 2000, 44(44):155-172.
王乐,李改欣,王仁德,等.半干旱农田灌丛沙堆形态及沉积特征[J].水土保持研究,2014,21(1):76-80.
朱永磊.河北主要土壤肥力质量时空变异及评价研究[D].河北 保定:河北农业大学,2014.
贾晓红,李新荣,王新平.流沙固定过程中土壤性质变异初步研究[J].水土保持学报,2003,17(4):46-50.
贾宝全,张红旗,张志强,等.甘肃省民勤沙区土壤结皮理化性质研究[J].生态学报,2003,23(7):1442-1448.
Dougill A J, Thomas A D. Nebkha dunes in the Molopo Basin, South Africa and Botswana: Formation controls and their validity as indicators of soil degradation[J]. Journal of Arid Environments, 2002, 50(3): 413-428.
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