1. 安徽理工大学 地球与环境学院,安徽,淮南,232001
2. 安徽省煤炭勘探工程技术研究中心,安徽,宿州,234000
3. 中国科学技术大学 地球和空间科学学院,安徽,合肥,230026
纸质出版:2016
移动端阅览
周育智, 王芳, 陈孝杨, 等. 生态修复模式对淮南矿区重构土壤CO2通量日变化的影响[J]. 水土保持通报, 2016,36(6):40-46.
ZHOU Yuzhi, WANG Fang, CHEN Xiaoyang, et al. Effects of Ecological Restoration Patterns on Diurnal Variation of CO2 Flux fromRehabilitated Soil of Coal Mining Areas in Huainan City[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 40-46.
周育智, 王芳, 陈孝杨, 等. 生态修复模式对淮南矿区重构土壤CO2通量日变化的影响[J]. 水土保持通报, 2016,36(6):40-46. DOI: 10.13961/j.cnki.stbctb.2016.06.007.
ZHOU Yuzhi, WANG Fang, CHEN Xiaoyang, et al. Effects of Ecological Restoration Patterns on Diurnal Variation of CO2 Flux fromRehabilitated Soil of Coal Mining Areas in Huainan City[J]. Bulletin of Soiland Water Conservation, 2016, 36(6): 40-46. DOI: 10.13961/j.cnki.stbctb.2016.06.007.
[目的
]
探讨淮南矿区不同生态修复模式(植被类型和覆土厚度)对土壤CO
2
通量的影响,以期为该区域以及相似矿区的生态修复提供理论依据及参数。[方法
]
采用静态箱-碱液吸收法对淮南市采煤沉陷生态修复区土壤CO
2
通量进行动态测定,分析土壤CO
2
通量日变化特征,以及土壤呼吸速率对地表温度、地下5 cm土壤温度和土壤含水量的敏感性。[结果
]
不同生态修复模式下土壤CO
2
通量日变化格局均表现为单峰曲线,最高峰出现在14:00,最低值出现在6:00,其均值大小依次为:B区(灌木林) > C区(灌木林) > D区(乔木林) > A区(草地),且B,C与A区差异显著(p
<
0.05),其他区之间差异不显著(p>0.05)。不同覆土厚度下土壤表层CO
2
通量平均值的大小依次为:40-80 cm > 0-20 cm > 20-40 cm > 80-100 cm。其最大值和变幅的大小顺序也遵循平均值大小顺序。4种修复模式下土壤CO
2
通量与地下5 cm土壤温度、地表温度均呈指数方程关系,R
2
值分别在0.34~0.70,0.48~0.83之间,与土壤含水量呈二次方函数关系,R
2
值在0.08~0.44之间。[结论
]
不同植被类型条件下,土壤CO
2
通量大小表现为:灌木林>乔木林>草地;不同覆土厚度条件下,除了覆土40-80 cm的样地外,土壤CO
2
通量随覆土厚度的增加而减少。植被类型对土壤CO
2
通量的影响较覆土厚度显著。
[Objective] To explore the effects of ecological restoration patterns in coal ming areas of Huainan City
including rehabilitation thickness of soil and reestablished vegetation type on soil CO2 flux
and to provide theoretical basis for ecological restoration patterns similar coal mining region.[Methods] Method of close static chamber-alkali absorption was used to measure the diurnal variation of reconstructing soil CO2 flux. Meanwhile
temperatures of soil surface and 5 cm depth and soil water content were measured and their influences on soil CO2 flux were analyzed in different ecological remediation patterns for coal mining district in Huainan City
Anhui Province.[Results] Diurnal variation of soil CO2 flux exhibited an obvious unimodal pattern during the whole observation period
with peak value at 14:00 and minimum flux at 6:00 for all of the ecological restoration models. The flux ranked at different revegetation districts as:B(brushwood) > C(brushwood) > D(arboreal forest) > A(grassland). Soil CO2 flux of B and C districts were significantly higher than that of A(p<0.05); no significant differences among others were observed(p>0.05). Soil CO2 flux with different rehabilitation thickness ranked as:40-80 cm > 0-20 cm > 20-40 cm > 80-100 cm
and their maximum and amplitude also followed this order. Significant relationships were found between soil temperature in 0 and 5 cm depth and soil CO2 flux
which could be described by exponential equation. R2 ranged from 0.34 to 0.70 and from 0.48 to 0.83
respectively. Relationship between soil CO2 flux and soil water content can be described by quadratic equation
with 0.08~0.44 R2 value.[Conclusion] Soil CO2 flux differed under different vegetation types
the highest occurred in brushwood[5.22 μmol/(m2·s)]
followed by arboreal forest[4.56 μmol/(m2·s)]
the lowest was grassland[3.89 μmol/(m2·s)].Except for 40-80 cm thickness
soil CO2 flux decreased with the increase of soil rehabilitation thickness. The influence of vegetation on soil CO2 flux was more significant than the one of soil rehabilitation thickness.
Raich J W, Potter C S. Global patterns of carbon dioxide emissions from soils[J]. Global Biogeochemical Cycles, 1995,9(1):23-36.
王铭.松嫩平原西部盐碱化生态系统土壤呼吸特征及土壤CO
2
无机通量研究[D].中国科学院研究生院,2014.
Maier C A, Albaugh T J, Lee Allen H, et al. Respiratory carbon use and carbon storage in mid-rotation loblolly pine(Pinus taeda L.)plantations:The effect of site resources on the stand carbon balance[J]. Global Change Biology, 2004,10(8):1335-1350.
Schlesinger W H, Andrews J A. Soil respiration and the global carbon cycle[J]. Biogeochemistry, 2000,48(1):7-20.
Luo Yiqi, Zhou Xuhui.土壤呼吸与环境[M].姜丽芬,曲来叶,周玉梅,等译.北京:高等教育出版社,2007.
Raich J W, Schlesinger W H. The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate[J]. Tellus Series B:Chemical and Physical Meteorology, 1992,44(2):81-99.
Yan Wende, Xu Wangming, Chen Xiaoyong, et al. Soil CO
2
flux in different types of forests under a subtropical microclimatic Environment[J]. Pedosphere, 2014,24(2):243-250.
陈盖,许明祥,张亚锋,等.黄土丘陵区不同有机碳背景下侵蚀坡面土壤呼吸特征[J].环境科学,2015,36(9):3383-3392.
梁福源,宋林华,王静.土壤CO
2
浓度昼夜变化及其对土壤CO
2
排放量的影响[J].地理科学进展,2003,22(2):170-176.
欧强,王江涛,周剑虹,等.滨海湿地不同水位梯度下的土壤CO
2
通量比较[J].应用与环境生物学报,2014,20(6):992-998.
常宗强,冯起,司建华,等.祁连山不同植被类型土壤碳贮量和碳通量[J].生态学杂志,2008,27(5):681-688.
陈孝杨,王芳,严家平,等.覆土厚度对矿区复垦土壤呼吸昼夜变化的影响[J].中国矿业大学学报,2016,45(1):163-169.
张杰琼,方凤满,余健,等.淮南大通矿区复垦土壤微生物量碳氮的分布特征[J].水土保持通报,2014,34(3):267-270.
董霁红,王莹.煤矿塌陷区废碴充填复垦土壤理化性质研究[J].矿业研究与开发,2008,28(1):68-70,88.
田晔,刘小燕,张明旭.微生物促进煤矸石复垦利用研究现状与展望[J].硅酸盐通报,2015,34(9):2529-2533.
丁访军,聂洋,高艳平,等.黔中喀斯特地区5种林型冬季土壤呼吸研究[J].水土保持通报,2010,30(1):11-16.
林莉萨,韩士杰,王跃思.长白山阔叶红松林土壤CO
2
释放通量[J].东北林业大学学报,2005,33(1):11-13.
杨文佳,李永夫,姜培坤,等.亚热带毛竹人工林土壤呼吸组分动态变化及其影响因素[J].应用生态学报,2015,26(10):2937-2945.
刘意立.我国亚热带季风气候区湿地土壤CO
2
,CH
4
排放规律研究[D].浙江杭州:浙江大学,2014.
沈征涛,王宝军,施斌,等.温湿度对土壤CO
2
释放影响的试验研究[J].南京大学学报:自然科学版,2012,48(6):761-767.
李涛,李芹,王树明,等.云南河口不同林龄人工橡胶林土壤CO
2
浓度的变化规律及其影响因素[J].热带作物学报,2015,36(1):9-15.
戚家忠,胡振琪,赵艳玲.铲运机复垦重构土壤容重值的时空变异特性[J].中国矿业大学学报,2005,34(4):467-471.
曹银贵,白中科,张耿杰,等.山西平朔露天矿区复垦农用地表层土壤质量差异对比[J].农业环境科学学报,2013,32(12):2422-2428.
张学礼,胡振琪,初士立.矿山复垦土壤压实问题分析[J].能源环境保护,2004,18(3):1-4.
Rosenzweig S T, Carson M A, Baer S G, et al. Changes in soil properties, microbial biomass, and fluxes of C and N in soil following post-agricultural grassland restoration[J]. Applied Soil Ecology, 2016,100:186-194.
刘晚苟,李良贤,谢海容,等.土壤容重对野生香根草幼苗根系形态及其生物量的影响[J].草业学报,2015,24(4):214-220.
何娜,王立海,孟春.压实对落叶松人工林夏季土壤呼吸日变化的影响[J].应用生态学报,2010,21(12):3070-3076.
吴雅琼,刘国华,傅伯杰,等.中国森林生态系统土壤CO
2
释放分布规律及其影响因素[J].生态学报,2007,27(5):2126-2135.
刘斌,鲁绍伟,高东,等.物理性环境因素对淮北地区杨树人工林土壤呼吸的影响[J].西部林业科学,2014,43(6):148-153.
吴蒙,马姜明,梁士楚,等.桂林市尧山桉树及马尾松林春、夏两季土壤碳通量特征[J].水土保持通报,2015,35(1):303-310.
杨金艳,王传宽.土壤水热条件对东北森林土壤表面CO
2
通量的影响[J].植物生态学报,2006,30(2):286-294.
李小宇,李勇,于寒青,等.退耕还林坡地土壤CO
2
排放的空间变化:地形的控制作用[J].植物营养与肥料学报,2015,21(5):1217-1224.
刘硕,李玉娥,孙晓涵,等.温度和土壤含水量对温带森林土壤温室气体排放的影响[J].生态环境学报,2013,22(7):1093-1098.
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