[1]YOU Zheng,YAO Xu,JING Hang,et al.Coordinated Variation Between Root Distributions and Soil Aggregate Characteristics at Different Successional Stages[J].Research of Soil and Water Conservation,2016,23(06):20-25,31.
Copy
Coordinated Variation Between Root Distributions and Soil Aggregate Characteristics at Different Successional Stages
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
23
Number of periods:
2016 06
Page number:
20-25,31
Column:
Public date:
2016-12-28
- Title:
- Coordinated Variation Between Root Distributions and Soil Aggregate Characteristics at Different Successional Stages
- Keywords:
- vegetation succession; root characteristic; soil aggregate
- CLC:
- Q948
- DOI:
- -
- Abstract:
- In order to understand the change of root distribution and the relationship with soil aggregate structure in different plant communities of succession stage, the characteristics of roots and soil aggregates of Artemisia capillaries, Artemisia gmelinii, Bothriochloa ischaemun community, which are typical species at abandoned stage in loess hilly region were studied by using the method of substituting spatial difference for time change. The results show that in the herbaceous community fine roots are the main part of whole roots and most of roots distribute in the upper soil layer; the root length density (RLD), root surface area (RSA), root biomass and specific root length (SRL) decreased with the increase of the size diameters (< 0.5, 0.5~1.0, 1.0~1.5, 1.5~2, > 2.0 mm). The stability of soil aggregates, RLD and RSA increased with succession durations. The stability of soil aggregates is significantly correlated with fine RLD, fine RSA and fine root biomass in the upper soil layer, which indicates that fine roots play an important role in vegetation succession and soil structure.
- References:
-
[1] 周梦华,程积民,万惠娥,等.云雾山本氏针茅群落根系分布特征[J].草地学报,2008,16(3):267-271.
[2] 郝艳茹,彭少麟.根系及其主要影响因子在森林演替过程中的变化[J].生态环境,2005,14(5):762-767.
[3] 燕辉,苏印泉,朱昱燕,等.秦岭北坡杨树人工林细根分布与土壤特性的关系[J].南京林业大学学报:自然科学版,2009,33(2):85-89.
[4] 程云环,韩有志,王庆成,等.落叶松人工林细根动态与土壤资源有效性关系研究[J].植物生态学报,2005,29(3):303-310.
[5] 韦兰英,上官周平.黄土高原不同演替阶段草地植被细根垂直分布特征与土壤环境的关系[J].生态学报,2006,26(11):3740-3748.
[6] 王长庭,王根绪,刘伟,等.植被根系及其土壤理化特征在高寒小嵩草草甸退化演替过程中的变化[J].生态环境学报,2012,21(3):409-416.
[7] 王清奎,汪思龙.土壤团聚体形成与稳定机制及影响因素[J].土壤通报,2005,36(3):415-421.
[8] 赵勇钢,赵世伟,华娟,等.半干旱典型草原区封育草地土壤结构特征研究[J].草地学报,2009,17(1):106-112.
[9] 周虎,吕贻忠,杨志臣,等.保护性耕作对华北平原土壤团聚体特征的影响[J].中国农业科学,2007,40(9):1973-1979.
[10] 李娜,韩晓增,尤孟阳,等.土壤团聚体与微生物相互作用研究[J].生态环境学报,2013,22(9):1625-1632.
[11] 宋日,刘利,马丽艳,等.作物根系分泌物对土壤团聚体大小及其稳定性的影响[J].南京农业大学学报,2009,32(3):93-97.
[12] 刘定辉,李勇.植物根系提高土壤抗侵蚀性机理研究[J].水土保持学报,2003,17(3):34-37.
[13] 李婕,杨学云,孙本华,等.不同土壤管理措施下土团聚体的大小分布及其稳定性[J].植物营养与肥料学报,2014,20(2):346-354.
[14] 李勇,武淑霞,夏侯国.紫色土区刺槐林根系对土壤结构的稳定作用[J].土壤侵蚀与水土保持学报,1998,4(2):2-8.
[15] Elliott E T. Aggregate structure and carbon, nitrogen, and phosphorus in native and cultivated soils[J]. Soil Science Society of America Journal, 1986,50(3):627-633.
[16] 杨培岭,罗远培,石元春.用粒径的重量分布表征的土壤分形特征[J].科学通报,1993,38(20):1896-1899.
[17] 曾全超,李娅芸,刘雷,等.黄土高原草地植被土壤团聚体特征与可蚀性分析[J].草地学报,2014,22(4):743-749.
[18] Schlossberg M J, Karnok K J, Landry G. Estimation of viable root-length density of Heat-tolerant Crenshaw’ and L93’ Creeping Bentgrass by an Accumulative Degree-day Model[J]. Journal of the American Society for Horticultural Science, 2002,127(2):224-229.
[19] 李鹏,李占斌,澹台湛.黄土高原退耕草地植被根系动态分布特征[J].应用生态学报,2005,16(5):849-853.
[20] Craine J M. Competition for Nutrients and Optimal Root Allocation[J]. Plant and Soil, 2006,285(1/2):171-185.
[21] 吴彦,刘庆,乔永康,等.亚高山针叶林不同恢复阶段群落物种多样性变化及其对土壤理化性质的影响[J].植物生态学报,2001,25(6):648-655.
[22] 董慧霞,李贤伟,张健,等.退耕地三倍体毛白杨林地细根生物量及其与土壤水稳性团聚体的关系[J].林业科学,2007,43(5):24-29.
- Similar References:
Memo
-
Last Update:
1900-01-01