LI Xuebin,LI Yuefei,CHEN Lin,et al.Effects of Different Land Use Types on Soil Active Organic Carbon in Desert Steppe of Ningxia[J].Northern Horticulture,2021,(01):91-99.[doi:10.11937/bfyy.20200709]
宁夏荒漠草原不同土地利用方式对土壤活性有机碳的影响
- Title:
- Effects of Different Land Use Types on Soil Active Organic Carbon in Desert Steppe of Ningxia
- Keywords:
- land use types; soil organic carbon; soil readily oxidizable carbon; dissolved organic carbon
- 文献标志码:
- A
- 摘要:
- 以宁夏荒漠草原不同土地利用方式(耕地、弃耕地、草地和柠条地)的土壤为研究对象,测定了不同土层土壤有机碳和活性有机碳含量,分析了土壤活性有机碳占有机碳的比例,以期探寻不同土地利用方式对土壤活性有机碳的影响。结果表明:不同土地利用方式土壤总有机碳含量范围在1.78~6.17 g?kg-1,具体表现为弃耕地>柠条地>草地>耕地。表层(0~5 cm)土壤有机碳含量显著高于深层(10~60 cm),说明荒漠草原土壤有机碳主要富集在表层;4种土地利用方式土壤易氧化有机碳含量为0.57~1.38 mg?g-1,变化趋势具体表现为柠条地>草地>耕地>弃耕地,且柠条地在每个土层都高于其它3种土地利用方式;土壤可溶性有机碳含量范围为6.8~11.1 mg?kg-1,变化趋势表现为草地>耕地>柠条地>弃耕地。土壤易氧化有机碳含量占有机碳的比例范围为13.7%~43.1%,大小排序为柠条地>耕地>草地>弃耕地;土壤可溶性有机碳含量占有机碳的比例范围为0.11%~0.48%,比例大小为耕地>草地>柠条地>弃耕地,耕地和草地中土壤可溶性有机碳含量占有机碳比例随着土壤深度的增加而减小,这与有机碳在耕地和草地中变化趋势一致。土地利用变化可以显著影响土壤活性有机碳的含量与分布,能够敏感的反映土壤碳库的变化,可以作为评价宁夏荒漠草原土壤质量和肥力的指标之一。
- Abstract:
- The content of soil organic carbon and active organic carbon under different land use patterns (arable land,derelict land,grassland and woodland) in Ningxia desert steppe was determined,and the proportion of soil active organic carbon to organic carbon was analyzed in order to explore the influence of different land use patterns on soil active organic carbon.The proportion of soil active organic carbon in organic carbon and the soil driving factors that affect the soil active organic carbon had been analyzed.The results showed that the total content of soil organic carbon in the four land use types ranges from 1.78 g?kg-1 to 6.17 g?kg-1,which was obviously showed by the trend of derelict land>horqin peashrub land>grassland>arable land.And the content of organic carbon in the surface layer (0-5 cm) was significantly higher than that of the deep soil layer (10-60 cm),which indicated that soil organic carbon was mainly enriched in the surface layer.The content of easily oxidizing organic carbon in the four land use types ways ranges from 0.57 mg?g-1 to 1.38 mg?g-1,and the changing trend was specifically showed by horqin peashrub land>grassland>arable land>derelict land.Besides,content of the horqin peashrub land was higher than the other three types of land in each soil layer.The soil water soluble organic carbon content of these four lands was from 6.8 mg?kg-1 to 11.1 mg?kg-1,which was showed by grassland>arable land>forestland>derelict land.The proportion of easily oxidizing organic carbon in these four lands was from 13.7% to 43.1%,which was showed by horqin peashrub land>arable land>grassland>derelict land.And the proportion of water soluble organic carbon in these four lands was from 0.11% to 0.48%,which was showed by arable land>grassland>horqin peashrub land>derelict land.The proportion of water soluble organic carbon in arable land and grassland declines with the rises of soil depth,which was consistent with the trend of organic carbon in arable land and grassland.Land use change could significantly affect the content and distribution of soil active organic carbon,and could sensitively reflect the change of soil carbon pool.It could be used as one of the indicators to evaluate soil quality and fertility in Ningxia desert steppe.
参考文献/References:
[1]王淑平,周广胜,高素华,等.中国东北样带土壤活性有机碳的分布及其对气候变化的响应[J].植物生态学报,2003(6):780-785.[2]CARTER M R,STEWART B A.Structure and organic matter storage in agricultural soils[M].Boca Raton:CRC Press,2020.[3]BLAIR G J,LEFROY R,LISLE L.Soil carbon fractions based on their degree of oxidation,and the development of a carbon management index for agricultural systems[J].Australian Journal of Agricultural Research,1995,46(7):393-406.[4]YING W,HONGHUA R,HUANG L L,et al.Soil labile organic carbon with different land uses in reclaimed land area from Taihu Lake[J].Soil Science,2010,175(12):624-630.[5]张仕吉,项文化.土地利用方式对土壤活性有机碳影响的研究进展[J].中南林业科技大学学报,2012,32(5):134-143.[6]刘晶,田耀武,张巧明.豫西黄土丘陵区不同土地利用方式土壤团聚体有机碳含量及其矿化特征[J].水土保持学报,2016,30(3):255-261.[7]祁心,江长胜,郝庆菊,等.缙云山不同土地利用方式对土壤活性有机碳、氮组分的影响[J].环境科学,2015,36(10):3816-3824.[8]陶宝先,张保华,董杰,等.不同土地利用方式对寿光市农业土壤有机碳分子结构和稳定性的影响[J].生态环境学报,2017,26(10):1801-1806.[9]郭岳,张仲胜,宋晓林.三江平原不同土地利用方式下土壤可溶性有机碳的分布特征[J].湿地科学与管理,2017,13(4):43-47.[10]邬建红,潘剑君,葛序娟,等.不同农业利用方式土壤有机碳矿化及其与有机碳组分的关系[J].水土保持学报,2015,29(6):178-183.[11]孙沙沙,段建军,王小利,等.喀斯特小流域不同土地利用方式下土壤有机碳的组分特征[J].山地农业生物学报,2018,37(3):49-55.[12]李欣雨,夏建国,鄢广奎,等.名山河流域不同土壤类型和土地利用方式下有机碳的分布特征[J].水土保持学报,2017,31(3):224-230,238.[13]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(1-2):55-68.[14]张煜,张琳,吴文良,等.内蒙农牧交错带地区土地利用方式和施肥对土壤碳库的影响[J].土壤学报,2016,53(4):930-941.[15]房飞,唐海萍,李滨勇.不同土地利用方式对土壤有机碳及其组分影响研究[J].生态环境学报,2013,22(11):1774-1779.[16]邱璇,赵建宁,李文亚,等.不同利用方式对小针茅荒漠草原土壤活性有机碳的影响[J].草业学报,2016,25(9):1-9.[17]蒲宁宁.放牧强度对昭苏草甸草原土壤有机碳组分及其碳、氮特征的影响[D].乌鲁木齐:新疆农业大学,2013.[18]杨合龙,孙宗玖,范燕敏,等.短期放牧对昭苏草甸草原土壤活性有机碳组分的影响[J].草业科学,2013,30(12):1926-1932.[19]吴建国,张小全,徐德应.六盘山林区几种土地利用方式下土壤活性有机碳的比较[J].植物生态学报,2004,28(5):657-664.[20]马鄂超.第二讲 土壤养分测定(一)[J].新疆农垦科技,2005(6):51-53.[21]朱勇,王振翀,能昌信,等.土壤电导率测量方法的研究与仿真[J].计算机仿真,2012,29(8):413-416.[22]沈宏,曹志洪,徐志红.施肥对土壤不同碳形态及碳库管理指数的影响[J].土壤学报,2000(2):166-173.[23]LIANG B C,MACKENZIE A F,SCHNITZER M,et al Management-induced change in labile soil organic matter under continuous corn in Eastern Canadian soils[J].Biology and Fertility of Soils,1997,26(2):88-94.[24]邰继承,靳振江,崔立强,等.不同土地利用下湖北江汉平原湿地起源土壤有机碳组分的变化[J].水土保持学报,2011,25(6):124-128.[25]SOLOMON D,LEHMANN J,KINYANGI J,et al.Long-term impacts of anthropogenic perturbations on dynamics and speciation of organic carbon in tropical forest and subtropical grassland ecosystems[J].Global Change Biology,2010,13(2):511-530.[26]陈高起,傅瓦利,沈艳,等.岩溶区不同土地利用方式对土壤有机碳及其组分的影响[J].水土保持学报,2015,29(3):123-129.[27]ROBLES M D,BURKE I C.Soil organic matter recovery on conservation reserve program fields in southeastern wyoming[J].Soil Science Society of America Journal,1998,62(3):725-730.[28]刘淑霞,王鸿斌,赵兰坡,等.不同施肥方式下黑土有机碳的变化规律研究[J].河南农业科学,2008(2):48-51,56.[29]董云中,王永亮,张建杰,等.晋西北黄土高原丘陵区不同土地利用方式下土壤碳氮储量[J].应用生态学报,2014,25(4):955-960.[30]李鉴霖,江长胜,郝庆菊.缙云山不同土地利用方式土壤有机碳组分特征[J].生态学报,2015,35(11):3733-3742.[31]邱莉萍,张兴昌,程积民.土地利用方式对土壤有机质及其碳库管理指数的影响[J].中国环境科学,2009,29(1):84-89.[32]BIEDERBECK V O,JANZEN H H,et al.Labile soil organic matter as influenced by cropping practices in an arid environment[J].Soil Biology & Biochemistry,1994,26(12):1647-1656.[33]BIQING L,JOHANNES L,DAWIT S,et al.Stability of biomass-derived black carbon in soils[J].Geochimica Et Cosmochimica Acta,2008,72(24):6069-6078.[34]朱志建,姜培坤,徐秋芳.不同森林植被下土壤微生物量碳和易氧化态碳的比较[J].林业科学研究,2006,19(4):523-526.[35]李太魁,朱波,王小国,等.土地利用方式对土壤活性有机碳含量影响的初步研究[J].土壤通报,2013,44(1):46-51.[36]MIRSKY S B,LANYON L E,NEEDELMAN B A.Evaluating soil management using particulate and chemically labile soil organic matter fractions[J].Soil Science Society of America Journal,2008,72(1):180-185.[37]SIX J,CONANT R T,PAUL E A,et al.Stabilization mechanisms of soil organic matter:Implications for C-saturation of soils[J].Plant & Soil,2002,241(2):155-176.[38]QUIDEAU S A,CHADWICK O A,BENESI A,et al.direct link between forest vegetation type and soil organic matter composition[J].Geoderma,2001,104(1):41-60.[39]STEENWERTH K L,JACKSON L E,FRANCISCO J,et al.Soil microbial community composition and land use history in cultivated and grassland ecosystems of coastal California[J].Soil Biology & Biochemistry,2003,34(11):1599-1611.[40]薛菁芳,高艳梅,汪景宽,等.土壤微生物量碳氮作为土壤肥力指标的探讨[J].土壤通报,2007(2):247-250.[41]张金波,宋长春,杨文燕.土地利用方式对土壤水溶性有机碳的影响[J].中国环境科学,2005,25(3):343-347.
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备注/Memo
第一作者简介:李学斌(1972-),男,博士,研究员,现主要从事草地和森林碳循环等研究工作。E-mail:lixuebin@nxu.edu.cn.基金项目:国家自然科学基金资助项目(31960359);宁夏自然科学基金资助项目(2020AAC03105);第三批宁夏青年科技人才托举工程资助项目(TJGC20180682018)。收稿日期:2020-02-29