摘要
研究了三峡库区澎溪河落干期消落带不同地点、不同高程段、不同土地利用方式下土壤硝化强度及影响因素。结果表明,研究区域消落带硝化强度范围为0.76~9.76 mg/kg·d,平均值为3.76±0.76mg/kg·d,明显低于国内其他研究区域土壤硝化强度。澎溪河消落带从上游汉丰湖到下游黄石,土壤硝化强度呈现递减的趋势。随着高程的增加,消落带土壤硝化强度逐渐降低,但没有显著差异(P>0.05)。消落带不同土地利用方式中,河滩地土壤硝化强度显著高于耕地土壤硝化强度(P<0.05),是耕地土壤硝化强度的1.82倍。消落带土壤硝化强度与土壤pH值呈显著正相关(P<0.05),与有机质含量及亚硝化菌数量呈极显著正相关(P<0.01),周期性的淹水影响了消落带土壤pH值和有机质含量,从而影响了消落带土壤硝化强度。
The impacts of land locations,utilization patterns and elevations on soil nitrification intensity in Pengxi water-level-fluctuating zone(WLFZ)during the dry period in the Three Gorges Reservoir area were studied.The results indicate that the nitrification intensity of the WLFZ soil ranges from 0.76mg/kg·d to9.76mg/kg·d,while the intensity averages at(3.76±0.76)mg/kg·d,which is significantly lower than those reported in other domestic researches.The soil nitrification intensity decreases from upstream(Hanfeng lake)to downstream(Huangshi city).In addition,the increase of elevation weakly decreases the nitrification intensity(P>0.05).Moreover,the nitrification intensities of flood lands are 1.82 times of those of cultivated soils(P<0.05).The soil nitrification intensity is significantly positively correlated with the soil pH value(P<0.05)as well as the contents of organic matter and the number of nitrosobacteria(P<0.01).Periodic flooding affects the soil pH and organic matter contents,which leads to the variation of soil nitrification intensity.
引文
[1]苏维词,赵纯勇,杨华.三峡库区消落区自然条件及其开发利用评价——以重庆库区为例[J].地理科学,2009,29(2):268-272.SU Weici,ZHAO Chunyong,YANG Hua.Evaluation on natural conditions of water-level-fluctuating zone(WLFZ)in three gorges reservoir[J].Scientia Geographica Sinica,2009,29(2):268-272.(in Chinese)
[2]Veresoglou S D,Chen B,Rillig M C.Arbuscular mycorrhiza and soil nitrogen cycling[J].Soil Biology&Biochemistry,2012,46(1):53-62.
[3]Dalias P,Anderson J M,Bottner P,et al.Temperature responses of net nitrogen mineralization and nitrification in conifer forest soils incubated under standard laboratory conditions[J].Soil Biology&Biochemistry,2002,34(5):691-701.
[4]Jiang X J,Hou X Y,Zhou X,et al.pH regulates key players of nitrification in paddy soils[J].Soil Biology&Biochemistry,2015,81(2):691-701.
[5]牟晓杰,刘兴土,仝川,等.人为干扰对闽江河口湿地土壤硝化反硝化潜力的影响[J].中国环境科学,2013,33(8):1413-1419.MOU Xiaojie,LIU Xingtu,TONG Chuan,et al.Effects of human disturbance on nitrification and denitrification potential in the Min River estuarine wetland[J].China Environmental Science,2013,33(8):1413-419.(in Chinese)
[6]吴承林,田伟君,宫晓敏,等.龙门口水库滨岸带硝化作用研究[J].中国海洋大学学报(自然科学版),2014,44(7):77-81.WU Chenglin,TIAN Weijun,GONG Xiaomin,et al.Studies on Nitrification in the riparian zone of Longmenkou reservoir[J].Periodical of Ocean University of China(Natural Science Edition),2014,44(7):77-81.(in Chinese)
[7]鲍士旦.土壤农化分析[M].北京:中国农业出版社,2005.BAO Shidan.The soil agrochemical analysis[M].Beijing:China Agricul Ture Press,2005.(in Chinese)
[8]林先贵.土壤微生物研究原理与方法[M].北京:高等教育出版社,2010.LIN Xiangui.Principles and methods of soil microbiology research[M].Beijing:Higher Education Press,2010.(in Chinese)
[9]周桦,于万太,徐永刚,等.一种土壤硝化作用潜势测定的方法:201010565600.4[P].2012-05-30.ZHOU Ye,YU Wantai,XU Yonggang,et al.A method for the test of Soil Nitrification Potential:201010565600.4[P].2012-05-30.(in Chinese)
[10]Carter M,Gregorich E,Adl S M,et al.Soil sampling and methods of analysis[J].Journal of Environmental Quality,2007,38(1):15-24.
[11]张树兰,杨学云,吕殿青,等.几种土壤剖面的硝化作用及其动力学特征[J].土壤学报,2000,37(3):372-379.ZHANG Shulang,YANG Xueyun,LV Dianqing,et al.Nitrification and dynamics in profiles of differently managed Soil Types[J].Acta Pedologica Sinica,2000,37(3):372-379.(in Chinese)
[12]王玉萍,王立立,李取生,等.珠江河口湿地沉积物硝化作用强度及影响因素研究[J].生态科学,2012,31(3):330-334.WANG Yuping,WANG Lili,Li Qusheng,et al.Study on nitrification and impact factors in Pearl River estuarine wetlands[J].Ecological Science,2012,31(3):330-334.(in Chinese)
[13]吕艳华,白洁,姜艳,等.黄河三角洲湿地硝化作用强度及影响因素研究[J].海洋湖沼通报,2008(2):61-66.LV Yanhua,BAI Jie,JIANG Yan,et al.Studies of nieifying activityy and impact factors of wetland in Yellow River Delta[J].Transactions of Oceanology and Limnology,2008(2):61-66.(in Chinese)
[14]郭劲松,黄轩民,张彬,等.三峡库区消落带土壤有机质和全氮含量分布特征[J].湖泊科学,2012,24(2):213-219.GUO Jinsong,HUANG Xuanmin,ZHANG Bin,et al.Distribution characteristics of organic matter and total nitrogen in the soils of water-levelfluctuating zone of Three Gorges Reservoir area[J].Journal of Lake Sciences,2012,24(2):213-219.(in Chinese)
[15]Zaman M,Saggar S,Blennerhassett J D,et al.Effect of urease and nitrification inhibitors on N transformation,gaseous emissions of ammonia and nitrous oxide,pasture yield and N uptake in grazed pasture system[J].Soil Biology and Biochemistry,2009,41(6):1270-1280.
[16]Lars R,Dan B K,Maj B J.Conecntrations and fiuxes of dissolved organic carbon and nitrogen in a Picea abies chronosequence on former arable land in Sweden[J].Forest Ecology and Management,2010,259(3):275-285.
[17]常超,谢宗强,熊高明,等.三峡水库蓄水对消落带土壤理化性质的影[J].自然资源学报,2011,26(7):1236-1244.CHANG Chao,XIE Zongqiang,XIONG Gaoming,et al.The effect of flooding on soil physical and chemical properties of riparian zone in the Three Gorges Reservoir[J].Jouranal of Natural Resources,2011,26(7):1236-1244.(in Chinese)
[18]杨洪昇,田昆,姚茜,等.筑坝蓄水对高原湿地拉市海土壤有机质和全氮分布格局的影响[J].生态学杂志,2015,34(1):162-167.YANG Hongshen,TIAN Kun,YAO Xi,et al.The impacts of dam impoundment on the distribution patterns of soil organic matter and total nitrogen in Lashihai plateau wetland[J].Chinese Journal of Ecology,2015,34(1):162-167.(in Chinese)
[19]Borken W,Ahrens B,Schulz C,et al.Site-to-site variability and temporal trends of DOC concentrations and fluxes in temperate forest soils[J].Global Change Biology,2011,17(7):2428-2443.
[20]曹磊,宋金明,李学刚,等.黄河三角洲典型潮汐湿地碳、氮、磷生物地球化学特征[J].海洋科学,2015,39(1):84-92.CAO Lei,SONG Jinming,LI Xuegang,et al.Biogeochemical characteristics of soil C,N,P in the tidal wetlands of the Yellow River Delta[J].Marine Science,2015,39(1):84-92.(in Chinese)
[21]Alex T C,Kenneth K T,Gao Suduan,et al.Temperature,water content and wet-dry cycle effects on DOC production andcarbon mineralization in agricultural peat soils[J].Soil Biology and Biochemistry,2006,38(3):477-488.
[22]Staik S,Eskelinen A,Mnnisto M K.Regulation of microbial community composition andactivity by soil nutrient availability,soil pH,and herbivory in the timdra[J].Ecosystems,2012,15(1):18-33.
[23]Park S,Bae W,Chung J,et al.Empirical model of the pH dependence of the maximum specific nitrification rate[J].Process Biochemistry,2007,42(12):1671-1676.
[24]Wde B,Kowalchuk G A.Nitrification in acid soils:micro-organisms and mechanisms[J].Soil Biology&Biochemistry,2001,33(7/8):853-866.
[25]Nguyen B T,Marschner P.Effect of drying and rewetting on phosphorus transformations in red brown soils with different soil organic matter content[J].Soil Biology&Biochemistry,2005,37(8):1573-1576.
[26]Shiwei Li S W,Xianjun Jiang X J,Xiaolan Wang X L,et al.Tillage effects on soil nitrification and the dynamic changes in nitrifying microorganisms in a subtropical rice-based ecosystem:A long-term field study[J].Soil&Tillage Research,2015,150(2):132-138.