[1]孔维波,石芸,姚毓菲,等.水蚀风蚀交错带退耕草坡地土壤酶活性和碳氮矿化特征[J].水土保持研究,2019,26(02):1-8,16.
 KONG Weibo,SHI Yun,YAO Yufei,et al.Characteristics of Enzyme Activity, Carbon and Nitrogen Mineralization of Soil in the Abandoned Sloping Cropland in Wind-Water Erosion Crisscross Region[J].Research of Soil and Water Conservation,2019,26(02):1-8,16.
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水蚀风蚀交错带退耕草坡地土壤酶活性和碳氮矿化特征

参考文献/References:

[1] 付晓莉.水蚀风蚀交错区土壤水、碳、氮、磷分布及有关过程对植被类型的响应[D].陕西杨凌:中国科学院教育部水土保持与生态环境研究中心,2010.
[2] 张燕江,邱莉萍,张兴昌,等.黄土高原农牧交错带退耕坡地苜蓿-铁杆蒿群落养分分布特征[J].干旱地区农业研究,2015,33(5):211-216.
[3] 赵哈林,赵学勇,张铜会,等.北方农牧交错带的地理界定及其生态问题[J].地球科学进展,2002,17(5):739-747.
[4] Chen Y P, Wang K B, Lin Y S, et al. Balancing green and grain trade[J]. Nature Geoscience, 2015,8(10):739-741.
[5] 王辽宏,邱莉萍,高海龙,等.农牧交错带本氏针茅坡地土壤-植物系统磷素分布特征[J].植物营养与肥料学报,2013,19(5):1192-1199.
[6] 张平仓.水蚀风蚀交错带水风两相侵蚀时空特征研究:以神木六道沟小流域为例[J].土壤侵蚀与水土保持学报,1999,5(3):93-96.
[7] 张婷,陈云明,武春华.黄土丘陵区铁杆蒿群落和长芒草群落地上生物量及土壤养分效应[J].中国水土保持科学,2011,9(5):91-97.
[8] 刘建,邱莉萍,程积民,等.黄土高原水蚀风蚀交错区5种典型草地群落土壤酶活性的研究[J].草地学报,2017,25(1):32-37.
[9] 沈芳芳,袁颖红,樊后保,等.氮沉降对杉木人工林土壤有机碳矿化和土壤酶活性的影响[J].生态学报,2012,32(2):517-527.
[10] Pajares P, Gallardo G F, Masciandaro M, et al. Enzyme activity as an indicator of soil quality changes in degraded cultivated Acrisols in the Mexican Trans-volcanic Belt[J]. Land Degradation & Development, 2011,22(3):373-381.
[11] 曹慧,孙辉,杨浩,等.土壤酶活性及其对土壤质量的指示研究进展[J].应用与环境生物学报,2003,9(1):105-109.
[12] Zhao N, Li X G. Effects of aspect-vegetation complex on soil nitrogen mineralization and microbial activity on the Tibetan Plateau[J]. Catena, 2017,155:1-9.
[13] Nunes D A D, Gama-Rodrigues E F, Barreto P A B, et al. Carbon and nitrogen mineralization in soil of leguminous trees in a degraded pasture in northern Rio de Janeiro, Brazil[J]. Journal of Forestry Research, 2016,27(1):91-99.
[14] 胡伟,邵明安,王全九.黄土高原退耕坡地土壤水分空间变异的尺度性研究[J].农业工程学报,2005,21(8):11-16.
[15] 陈立明,满秀玲.小兴安岭谷地云冷杉林土壤酶活性的异质性[J].森林工程,2010,26(1):1-6.
[16] 贺金红,廖允成,胡兵辉,等.黄土高原坡耕地退耕还林(草)的生态经济效应研究[J].农业现代化研究,2006,27(2):110-114.
[17] 鲍士旦.土壤农化分析[M].北京:中国农业出版社,1986.
[18] 关松荫.土壤酶及其研究方法[M].北京:农业出版社,1986.
[19] 王玉红,马天娥,魏艳春,等.黄土高原半干旱草地封育后土壤碳氮矿化特征[J].生态学报,2017,37(2):378-386.
[20] Li H, Reynolds J F. On definition and quantification of heterogeneity[J]. Oikos, 1995,73(2):280-284.
[21] Maag M, Vinther F P. Nitrous oxide emission by nitrification and denitrification in different soil types and at different soil moisture contents and temperatures[J]. Applied Soil Ecology, 1996,4(1):5-14.
[22] 曲国辉,郭继勋.松嫩平原不同演替阶段植物群落和土壤特性的关系[J].草业学报,2003,12(1):18-22.
[23] 景福军,张德罡,尚占环,等.黄土高原弃耕地不同地形下植物群落演替初期的群落结构及多样性研究[J].甘肃农业大学学报,2005,40(2):233-238.
[24] Liu X R, Dong Y S, Ren J Q, et al. Drivers of soil net nitrogen mineralization in the temperate grasslands in Inner Mongolia, China[J]. Nutrient Cycling in Agroecosystems, 2010,87(1):59-69.
[25] 程积民,井赵斌,金晶炜,等.黄土高原半干旱区退化草地恢复与利用过程研究[J].中国科学:生命科学,2014,44(3):267-279.
[26] 成毅,安韶山,马云飞.宁南山区不同坡位土壤微生物生物量和酶活性的分布特征[J].水土保持研究,2010,17(5):148-153.
[27] 邱莉萍,张兴昌,程积民.坡向坡位和撂荒地对云雾山草地土壤酶活性的影响[J].草业学报,2007,16(1):87-93.
[28] Aon M A, Colaneri A C. Temporal and spatial evolution of enzymatic activities and physico-chemical properties in an agricultural soil[J]. Applied Soil Ecology, 2001,18(3):255-270.
[29] Grayston S J, Prescott C E. Microbial communities in forest floors under four tree species in coastal British Columbia[J]. Soil Biology & Biochemistry, 2005,37(6):1157-1167.
[30] Grønli K E, Frostegård A, Bakken L R, et al. Nutrient and carbon additions to the microbial soil community and its impact on tree seedlings in a boreal spruce forest[J]. Plant and Soil, 2005,278(1):275-291.
[31] 秦燕.贺兰山西坡不同草地类型土壤酶活性特征[D].兰州:兰州大学,2007.
[32] 安韶山,黄懿梅,刘梦云,等.宁南宽谷丘陵区植被恢复中土壤酶活性的响应及其评价[J].水土保持研究,2005,12(3):31-34.
[33] 杨佳佳.延河流域植被类型对土壤酶活性和土壤碳氮形态的影响[D].陕西杨凌:西北农林科技大学,2014.
[34] Elfstrand S, Hedlund K, Martensson A. Soil enzyme activities, microbial community composition and function after 47 years of continuous green manuring[J]. Applied Soil Ecology, 2007,35(3):610-621.
[35] Pinay G, Barbera P, Carreras P A, et al. Impact of atmospheric CO2 and plant life forms on soil microbial activities[J]. Soil Biology & Biochemistry, 2007,39(1):33-42.
[36] 李顺姬,邱莉萍,张兴昌.黄土高原土壤有机碳矿化及其与土壤理化性质的关系[J].生态学报,2010,30(5):1217-1226.
[37] Saggar S, Yeates G W, Shepherd T G. Cultivation effects on soil biological properties, microfauna and organic matter dynamics in Eutric Gleysol and Gleyic Luvisol soils in New Zealand[J]. Soil & Tillage Research, 2001,58(1):55-68.
[38] Eze S, Palmer S M, Chapman P J. Soil organic carbon stock and fractional distribution in upland grasslands[J]. Geoderma, 2018, 314:175-183.
[39] 黄耀,刘世梁,沈其荣,等.环境因子对农业土壤有机碳分解的影响[J].应用生态学报,2002,13(6):709-714.
[40] Wei X, Reich P B, Hobbie S E, et al. Disentangling species and functional group richness effects on soil N cycling in a grassland ecosystem[J]. Global Change Biology, 2017,23(11):4717-4727.
[41] Wei X, Shao M, Fu X, et al. The effects of land use on soil N mineralization during the growing season on the northern Loess Plateau of China[J]. Geoderma, 2011,160(3):590-598.
[42] Tischer A, Blagodatskaya E, Hamer U. Microbial community structure and resource availability drive the catalytic efficiency of soil enzymes under land-use change conditions[J]. Soil Biology & Biochemistry, 2015,89:226-237.
[43] Zhao H, Zhang X, Xu S, et al. Effect of freezing on soil nitrogen mineralization under different plant communities in a semi-arid area during a non-growing season[J]. Applied Soil Ecology, 2010,45(3):187-192.
[44] 朱新萍,贾宏涛,郑春霞,等.高产棉田土壤碱性磷酸酶及脲酶空间变异特征分析[J].干旱区研究,2012,29(4):586-591.
[45] 朱剑兴,王秋凤,何念鹏,等.内蒙古不同类型草地土壤氮矿化及其温度敏感性[J].生态学报,2013,33(19):6320-6327.
[46] Wei X, Huang M, Shao M, et al. Shrubs increase soil resources heterogeneity along semiarid grass slopes in the Loess Plateau[J]. Journal of Arid Environments, 2013,88(1):175-183.

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备注/Memo

收稿日期:2018-03-21;改回日期:2018-06-06。
基金项目:国家自然科学基金(41622105,41571130082,41571296);中国科学院前沿科学重点研究计划(QYZDB-SSW-DQC039)
作者简介:孔维波(1994-),男,河南信阳人,硕士研究生,研究方向为土壤生态。E-mail:kwb0207@163.com
通讯作者:魏孝荣(1978-),男,陕西武功人,研究员,博士生导师,主要从事生物地球化学循环研究。E-mail:xrwei78@163.com

更新日期/Last Update: 1900-01-01