[1]ZHANG Shuilin,MA Lina,WANG Yan,et al.Characteristics of Soil Carbon, Nitrogen and Phosphorus Stoichiometry and Enzyme Activity Under Different Ecological Restoration Types of Rocky Desertification in Fault Basin[J].Research of Soil and Water Conservation,2023,30(04):69-74.[doi:10.13869/j.cnki.rswc.2023.04.010.]
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Characteristics of Soil Carbon, Nitrogen and Phosphorus Stoichiometry and Enzyme Activity Under Different Ecological Restoration Types of Rocky Desertification in Fault Basin

References:
[1] 曹建华,邓艳,杨慧,等.喀斯特断陷盆地石漠化演变及治理技术与示范[J].生态学报,2016,36(22):7103-7108.
[2] 邹志刚,张浩,曾昭霞,等.云南断陷盆地喀斯特4种典型种植模式的能值分析[J].应用生态学报,2018,29(8):2641-2650.
[3] 丁新辉,刘孝盈,刘广全.基于改进TOPSIS法的南方岩溶区石漠化生态治理模式评价[J].泥沙研究,2021,46(2):54-58,20.
[4] 伏文兵,严友进,李华林,等.岩溶槽谷石漠化综合治理区治理生态效益评价[J].西南大学学报:自然科学版,2021,43(7):146-156.
[5] 许尔琪.基于CiteSpace的喀斯特石漠化国际研究进展[J].中国岩溶,2021,40(4):728-738.
[6] Jiang Z, Lian Y, Qin X, et al. Rocky desertification in Southwest China: impacts, causes, and restoration[J]. Earth-Science Reviews, 2014,132:1-12.
[7] Liu Y, Huang X, Yang H, et al. Environmental effects of land-use/cover change caused by urbanization and policies in Southwest China Karst area: A case study of Guiyang[J]. Habitat International, 2014,44:339-348.
[8] 汪攀.喀斯特石漠化生态系统土壤C,N,P生态化学计量学特征及其环境影响因子研究[D].贵阳:贵州师范大学,2019.
[9] 刘娜,喻理飞,赵庆,等.喀斯特高原石漠化区次生林叶片-枯落物-土壤连续体碳氮磷生态化学计量特征[J].应用与环境生物学报,2020,26(3):681-688.
[10] Fan H, Wu J, Liu W, et al. Linkages of plant and soil C:N:P stoichiometry and their relationships to forest growth in subtropical plantations [J]. Plant and Soil, 2015,392(1):127-138.
[11] 关松荫.土壤酶及其研究法[M].北京:农业出版社,1986.
[12] Badiane N N Y, Chotte J L, Pate E, et al. Use of soil enzyme activities to monitor soil quality in natural and improved fallows in semi-arid tropical regions[J]. Applied Soil Ecology, 2001,18(3):229-238.
[13] 王宇,张华,张贵,等.喀斯特断陷盆地环境地质分区及功能[J].中国岩溶,2017,36(3):283-295.
[14] 鲍士旦.土壤农化分析[M].3版.北京:农业出版社,2000.
[15] Kandeler E, Getber H. Short-term assay of soil urease activity using determination of ammonium[J]. Biology and Fertility of Soils, 1988,6(1):68-72.
[16] 陈玉平,吴佳斌,张曼,等.枯落物处理对森林土壤碳氮转化过程影响研究综述[J].亚热带资源与环境学报,2012,7(2):84-94.
[17] 吴丽芳,王妍,刘云根,等.岩溶石漠化区人工植被类型对土壤团聚体生态化学计量特征的影响[J].东北林业大学学报,2021,49(6):63-69.
[18] 曾锋,邱治军,许秀玉,等.森林凋落物分解研究进展[J].生态环境学报,2010,19(1):239-243.
[19] 陈培云,范弢,何停,等.滇东岩溶高原不同恢复阶段云南松林叶片-枯落物-土壤碳氮磷化学计量特征[J].应用与环境生物学报,2022,28(6):1549-1556.
[20] Tian H, Chen G, Zhang C, et al. Pattern and variation of C:N:P ratios in China's soils: a synthesis of observational data[J]. Biogeochemistry, 2010,98:139-151.
[21] 杨宁,邹冬生,杨满元,等.衡阳紫色土丘陵坡地不同植被恢复阶段土壤微生物群落多样性的变化[J].林业科学,2016,52(8):146-156.
[22] 殷全玉,许希希,孟晓楠,等.不同炭化温度生物质炭对不同质地植烟土壤铵态氮含量的影响[J].南京农业大学学报,2018,41(5):881-887.
[23] 何高迅,王越,彭淑娴,等.滇中退化山地不同植被恢复下土壤碳氮磷储量与生态化学计量特征[J].生态学报,2020,40(13):4425-4435.
[24] 杨万勤,钟章成,陶建平,等.缙云山森林土壤酶活性与植物多样性的关系[J].林业科学,2001,37(4):124-128.
[25] 赵朝辉.湘西南石漠化治理模式对土壤微生物量和酶活性的影响[D].长沙:中南林业科技大学,2012.
[26] 孙文颖,马维伟,李广,等.尕海湿地植被退化过程中土壤蔗糖酶和淀粉酶活性的动态特征[J].草地学报,2019,27(1):88-96.
[27] Park S C, Smith T J, Bisesi M S, et al. Activities of phosphomonoesterase from Lumbricus terrestris[J]. Soil Biology and Biochemistry, 1992,24:873-876.
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