植茶年限对土壤水稳性团聚体腐殖质组分特征的影响
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摘要
退耕植茶是川西低山丘陵区响应退耕还林工程实施的重要措施之一.为了研究茶园土壤团聚体中腐殖质组分的分布特征,反映植茶对土壤质量的影响,选取不同植茶年限(18、25、33、55 a)的老川茶园为研究对象,以邻近撂荒地为对照(CK),研究植茶对土壤团聚体中富里酸(FA)和胡敏酸(HA)分布的影响.结果表明:(1)不同植茶年限下,土壤富里酸含量(以质量分数计)在2.97~6.26 g/kg之间,胡敏酸含量在1.24~4.89 g/kg之间;随植茶年限的延长,土壤富里酸、胡敏酸含量先增加后降低,均在植茶25 a时达到最大值.(2)随着土壤团聚体粒径的减小,富里酸含量逐渐降低,胡敏酸则表现为≥5 mm粒径团聚体高于其他粒径.(3)土壤胡富比(HA/FA)在0.30~0.88之间,总体表现为≥5 mm和<0.25 mm粒径团聚体腐殖化程度较高,植茶25 a时大团聚体数量的增加有利于有机质含量和品质的提高.(4)逐步回归分析表明,≥5、2~5、0.25~0.5和<0.25 mm粒级团聚体中有机碳组分对水稳性团聚体的形成和稳定的影响较大.研究显示,植茶有利于土壤团聚体中腐殖质各组分的积累和腐殖化程度的增强,可增加土壤有机碳的稳定性;植茶25 a时土壤碳汇效应较强,植茶33 a后土壤固碳能力有所下降,可通过改善茶园施肥管理等措施保持茶园土壤的结构和肥力,以实现茶园土壤的可持续利用.
Changing farmlands to tea plantation is an important measure in response to the Grain for Green Project in the hilly region of western Sichuan Province,China. The distribution characteristics of humus fractions in soil aggregates of tea garden were studied in order to reflect the influence of tea plantation on soil quality,and to provide theoretical basis for the sustainable utilization of tea garden soil. Soil samples were collected from an abandoned land(CK) and four tea plantations with different ages(18,25,33,55 years old),and examined for the distribution of humus fractions(FA,HA) in soil aggregates. The results showed that:(1) The fulvic acid(FA) content varied from 2. 97 g/kg to 6. 26 g/kg,while the humic acid(HA) content varied from 1. 24 g/kg to 4. 89 g/kg. The contents of fulvic acid and humic acid first increased and then decreased with increasing age of tea plantation,and reached to peak point with tea plantation age of 25 years.(2) With decrease in size of the soil aggregates,fulvic acid content decreased gradually,while humic acid content was higher in aggregate size of ≥5 mm than others.(3) The ratio of HA to FA varied from 0. 30 to 0. 88. ≥5 and <0. 25 mm aggregates showed a higher humification degree. The increase of large aggregates was beneficial to the improvement of organic matter content and quality in soils with tea plantation for 25 years.(4) The result of stepwise regression analysis showed that soil organic carbon fractions in ≥5,2-5 and<0. 25 mm aggregates influenced the stability of soil aggregates. The findings suggested that tea plantation was beneficial for accumulation of humus in soil aggregates,for enhancement of humification and to increase the soil organic carbon stability. The soil carbon sink effectwas strongest in the tea plantation for 25 years. After long-term tea planting(33 a),the humus content and soil C sequestration capacity decreased. So the soil structure and fertility of tea garden could be maintained by improving the management of fertilization for sustainable utilization of tea garden soils.
Changing farmlands to tea plantation is an important measure in response to the Grain for Green Project in the hilly region of western Sichuan Province,China. The distribution characteristics of humus fractions in soil aggregates of tea garden were studied in order to reflect the influence of tea plantation on soil quality,and to provide theoretical basis for the sustainable utilization of tea garden soil. Soil samples were collected from an abandoned land(CK) and four tea plantations with different ages(18,25,33,55 years old),and examined for the distribution of humus fractions(FA,HA) in soil aggregates. The results showed that:(1) The fulvic acid(FA) content varied from 2. 97 g/kg to 6. 26 g/kg,while the humic acid(HA) content varied from 1. 24 g/kg to 4. 89 g/kg. The contents of fulvic acid and humic acid first increased and then decreased with increasing age of tea plantation,and reached to peak point with tea plantation age of 25 years.(2) With decrease in size of the soil aggregates,fulvic acid content decreased gradually,while humic acid content was higher in aggregate size of ≥5 mm than others.(3) The ratio of HA to FA varied from 0. 30 to 0. 88. ≥5 and <0. 25 mm aggregates showed a higher humification degree. The increase of large aggregates was beneficial to the improvement of organic matter content and quality in soils with tea plantation for 25 years.(4) The result of stepwise regression analysis showed that soil organic carbon fractions in ≥5,2-5 and<0. 25 mm aggregates influenced the stability of soil aggregates. The findings suggested that tea plantation was beneficial for accumulation of humus in soil aggregates,for enhancement of humification and to increase the soil organic carbon stability. The soil carbon sink effectwas strongest in the tea plantation for 25 years. After long-term tea planting(33 a),the humus content and soil C sequestration capacity decreased. So the soil structure and fertility of tea garden could be maintained by improving the management of fertilization for sustainable utilization of tea garden soils.
引文
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[3]SOLLINS P,GREGG J W.Soil organic matter accumulation in relation to changing soil volume,mass,and structure:concepts and calculations[J].Geoderma,2017,301:60-71.
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[6]YILMAZ E,SONMEZ M.The role of organic/bio-fertilizer amendment on aggregate stability and organic carbon content in different aggregate scales[J].Soil and Tillage Research,2017,168:118-124.
[7]潘根兴,周萍,李恋卿,等.固碳土壤学的核心科学问题与研究进展[J].土壤学报,2007,44(2):327-337.PAN Genxing,ZHOU Ping,LI Lianqing,et al.Core issues and research progresses of soil science of C sequestration[J].Acta Pedologica Sinica,2007,44(2):327-337.
[8]朱秋莲,程曼,安韶山,等.宁南山区植被恢复对土壤团聚体特征及腐殖质分布的影响[J].水土保持学报,2013,27(4):247-251.ZHU Qiulian,CHENG Man,AN Shaoshan,et al.Effects of revegetation on characteristics of soil aggregates and humus in soil aggregate in loess hilly region of southern Ningxia[J].Journal of Soil and Water Conservation,2013,27(4):247-251.
[9]董雪,王春燕,黄丽,等.侵蚀红壤腐殖酸组分特点及其对水稳性团聚体的影响[J].土壤学报,2014,51(1):114-125.DONG Xue,WANG Chunyan,HUANG Li,et al.Characteristics of humus fraction in erosion ultisols and their effects on water-stable aggregates[J].Acta Pedologica Sinica,2014,51(1):114-125.
[10]WIESMEIER M,SPORLEIN P,GEUSS U,et al.Soil organic carbon stocks in southeast Germany(Bavaria)as affected by land use,soil type and sampling depth[J].Global Change Biology,2012,18(7):2233-2245.
[11]JAMALA G Y,OKE D O.Soil organic carbon fractions as affected by land use in the southern Guinea Savanna ecosystem of Adamawa State,Nigeria[J].Journal of Soil Science and Environmental Management,2013,4(6):116-122.
[12]张曼夏,季猛,李伟,等.土地利用方式对土壤团聚体稳定性及其结合有机碳的影响[J].应用与环境生物学报,2013,19(4):598-604.ZHANG Manxia,JI Meng,LI Wei,et al.Effect of land use patterns on soil aggregate stability and aggregate-associated organic carbon[J].Chinese Journal of Applied and Environmental Biology,2013,19(4):598-604.
[13]安韶山,张玄,张扬,等.黄土丘陵区植被恢复中不同粒级土壤团聚体有机碳分布特征[J].水土保持学报,2007,21(6):109-113.AN Shaoshan,ZHANG Xuan,ZHANG Yang,et al.Distribution of organic carbon in different soil aggregates size during revegetation in hilly-gully region of Loess Plateau[J].Journal of Soil and Water Conservation,2007,21(6):109-113.
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[15]WEI Xiaorong,LI Xuezhang,JIA Xiaoxu,et al.Accumulation of soil organic carbon in aggregates after afforestation on abandoned farmland[J].Biology and Fertility of Soils,2013,49(6):637-646.
[16]马帅,赵世伟,李婷,等.子午岭林区不同植被恢复阶段土壤有机碳变化研究[J].水土保持通报,2011,31(3):94-98.MA Shuai,ZHAO Shiwei,LI Ting,et al.Changes of soil organic carbon in various stages of vegetation restoration in Ziwuling Mountain[J].Bulletin of Soil and Water Conservation,2011,31(3):94-98.
[17]LI Wei,ZHENG Zicheng,LI Tingxuan,et al.Effect of tea plantation age on the distribution of soil organic carbon fractions within waterstable aggregates in the hilly region of Western Sichuan,China[J].Catena,2015,133:198-205.
[18]WANG Shengqiang,LI Tingxuan,ZHENG Zicheng.Effect of tea plantation age on the distribution of soil organic carbon and nutrient within micro-aggregates in the hilly region of western Sichuan,China[J].Ecological Engineering,2016,90:113-119.
[19]WANG Shengqiang,LI Tingxuan,ZHENG Zicheng.Distribution of microbial biomass and activity within soil aggregates as affected by tea plantation age[J].Catena,2017,153:1-8.
[20]郑子成,刘敏英,李廷轩.不同植茶年限土壤团聚体有机碳的分布特征[J].中国农业科学,2013,46(9):1827-1836.ZHENG Zicheng,LIU Minying,LI Tingxuan.Distribution characteristics of organic carbon fractions in soil aggregates under tea plantation of different ages[J].China Agriculture Science,2013,46(9):1827-1836.
[21]POEPLAU C,KATTERER T,LEBLANS N I,et al.Sensitivity of soil carbon fractions and their specific stabilisation mechanisms to extreme soil warming in a subarctic grassland[J].Global Change Biology,2017,23(3):1316-1327.
[22]MUNOZ-ROMERO V,LOPEZ-BELLIDO R J,FERNANDEZGARCIA P,et al.Effects of tillage,crop rotation and N application rate on labile and recalcitrant soil carbon in a Mediterranean Vertisol[J].Soil and Tillage Research,2017,169:118-123.
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