[1]刘玉萍,陈 西,王延华,等.滇池流域土壤养分分布及其对水体富营养化的影响[J].南京师范大学学报(自然科学版),2017,40(04):129.[doi:10.3969/j.issn.1001-4616.2017.04.021]
 Liu Yuping,Chen Xi,Wang Yanhua,et al.Soil Nutrients Distribution in the Small Catchment andTheir Effects on the Eutrophication of Dianchi Lake[J].Journal of Nanjing Normal University(Natural Science Edition),2017,40(04):129.[doi:10.3969/j.issn.1001-4616.2017.04.021]
点击复制

滇池流域土壤养分分布及其对水体富营养化的影响()
分享到:

《南京师范大学学报》(自然科学版)[ISSN:1001-4616/CN:32-1239/N]

卷:
第40卷
期数:
2017年04期
页码:
129
栏目:
·地理学·
出版日期:
2017-12-30

文章信息/Info

Title:
Soil Nutrients Distribution in the Small Catchment andTheir Effects on the Eutrophication of Dianchi Lake
文章编号:
1001-4616(2017)04-0129-08
作者:
刘玉萍1陈 西1王延华12杨 浩12张明礼1谢 标1崔 骏1
(1.南京师范大学地理科学学院,江苏 南京 210023)(2.江苏省物质循环与污染控制重点实验室,江苏 南京 210023)
Author(s):
Liu Yuping1Chen Xi1Wang Yanhua12Yang Hao12Zhang Mingli1Xie Biao1Cui Jun1
(1.School of Geography Science,Nanjing Normal University,Nanjing 210023,China)(2.Jiangsu Provincial Key Laboratory of Materials Cycling and Pollution Control,Nanjing 210023,China)
关键词:
滇池小流域土壤养分土地利用方式生态风险
Keywords:
Dianchi lakesmall catchmentnutrientland useecological risk
分类号:
X53
DOI:
10.3969/j.issn.1001-4616.2017.04.021
文献标志码:
A
摘要:
在滇池松华坝小流域(SHB)和上游小流域(SY)选取荒地、林地和草地3种土地利用方式,分别采集0~40 cm土壤样品. 测定样品中总有机碳(TOC)、总氮(TN)和总磷(TP)含量,对比不同土地利用方式下土壤营养盐分布差异,并对流域内土壤营养盐负荷及其对水体富营养化的潜在影响进行评价. 结果表明,①SHB小流域:TOC、TN和TP的含量均为草地最高,分别为16.88、1.77和0.42 mg/g; TOC含量:林地>荒地,TN和TP在林地和荒地中的含量差异不明显; ②SY小流域不同土地利用方式下营养
Abstract:
In this paper,three types of land uses including abandoned land,forestland and grassland in the Songhuaba catchment(SHB)and the Shangyou catchment(SY)of the Dianchi watershed were investigated to determine the effects of land use on soil nutrients. Contents of total nitrogen(TN),total phosphorus(TP)and total organic carbon(TOC)in the soil samples were measured to compare the differences between three types of land uses in two catchments. Nutrients pollution and the risk of eutrophication was in discussion as well. Results are as follows:(1)In the SHB catchment,the highest contents of TOC(16.88 mg/g),TN(1.77 mg/g)and TP(0.42 mg/g)were observed in the grassland. TOC content in the forestland was higher than that in the abandoned land. While the difference of TN and TP contents between the forestland and grassland was not obvious.(2)In the SY catchment,the similar distribution was found. The contents of TOC,TN and TP were highest in the grassland and lowest in the abandoned land. Not obvious difference of TN and TP contents in three types of land uses were observed.(3)Comparing the soil profile,TOC,TN and TP contents in the layer of 0-20 cm soil were much higher than those in the layer of 20-40 cm in both catchments. The TOC,TN and TP contents in the surface soil of the grassland is much higher than those in the abandoned land.(4)The TN standard index of three types of land uses was beyond the safe line,reflecting high eutrophication potential. The key measure will be the control of nitrogen inputs in the small catchment. OI and TP standard indexes in the abandoned land were lower than those in the forestland and grassland. Three standard indexes in the layer of 0-20 cm soil are relatively high,indicating ecological risks.

参考文献/References:

[1] 金相灿. 中国湖泊富营养化[M]. 北京:中国环境科学出版社,1992:8-12.
[2]吴雅丽,许海,杨桂军,等. 太湖水体氮素污染状况研究进展[J]. 湖泊科学,2014,26(1):19-28.
[3]KRONVANG B,GRAESB?LL P,LARSEN S E,et al. Diffuse nutrient losses in Denmark[J]. Water science and technology,1996,33(4/5):81-88.
[4]周慧平,高超. 巢湖流域非点源磷流失关键源区识别[J]. 环境科学,2008,29(10):2 696-2 702.
[5]李秀芬,朱金兆,顾晓君,等. 农业面源污染现状与防治进展[J]. 中国人口·资源与环境,2010,20(4):81-84.
[6]ZUAZO V H D. Soil-erosion and runoff prevention by plant covers:a review[J]. Agronomy for sustainable development,2008,28(1):65-86.
[7]MUNODAWAFA A. Assessing nutrient losses with soil erosion under different tillage systems and their implications on water quality[J]. Physics and chemistry of the Earth parts a/b/c,2007,32(15/18):1 135-1 140.
[8]EKHOLM P,LEHTORANTA J. Does control of soil erosion inhibit aquatic eutrophication?[J]. Journal of environmental management,2012,93(1):140-146.
[9]BAKKER M M,GOVERS G,DOORN A V,et al. The response of soil erosion and sediment export to land-use change in four areas of Europe:the importance of landscape pattern[J]. Geomorphology,2008,98(3/4):213-226.
[10]马广文,王业耀,香宝,等. 长江上游流域土地利用对面源污染影响及其差异[J]. 农业环境科学学报,2012,31(4):791-797.
[11]WANG H J,SHI X Z,YU D S,et al. Factors determining soil nutrient distribution in a small-scaled watershed in the purple soil region of Sichuan Province,China[J]. Soil and tillage research,2009,105(2):300-306.
[12]耿润哲,李明涛,王晓燕,等. 基于SWAT模型的流域土地利用格局变化对面源污染的影响[J]. 农业工程学报,2015,31(16):241-250.
[13]杨文龙,杨树华. 滇池流域非点源污染控制区划研究[J]. 湖泊科学,1998,10(3):55-60.
[14]徐美娜. 滇南小流域沉积有机质源解析及其影响机制[D]. 南京:南京师范大学,2016.
[15]钱君龙,张连弟. 土壤理化分析[M]. 上海:上海科学技术出版社,1978:62-67.
[16]隋桂荣. 太湖表层沉积物中OM、TN、TP的现状与评价[J]. 湖泊科学,1996,8(4):319-324.
[17]LEIVUORI M,NIEMIST? L. Sedimentation of trace metals in the Gulf of Bothnia[J]. Chemosphere,1995,31(8):3 839-3 856.
[18]彭近新,陈慧君. 水质富营养化与防治[M]. 北京:中国环境科学出版社,1988:48-62.
[19]李任伟. 沉积物污染和环境沉积学[J]. 地球科学进展,1998,13(4):398-402.
[20]陈春瑜,和树庄,胡斌,等. 土地利用方式对滇池流域土壤养分时空分布的影响[J]. 应用生态学报,2012,23(10):2 677-2 684.
[21]LENKA N K,DASS A,SUDHISHRI S,et al. Soil carbon sequestration and erosion control potential of hedgerows and grass filter strips in sloping agricultural lands of eastern India[J]. Agriculture ecosystems and environment,2012,158(6):31-40.
[22]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):3 733-3 742.[23]COLLINS H P,ELLIOTT E T,PAUSTIAN K,et al. Soil carbon pools and fluxes in long-term corn belt agroecosystems[J]. Soil biology and biochemistry,2000,32(2):157-168.
[24]傅华,陈亚明,王彦荣,等. 阿拉善主要草地类型土壤有机碳特征及其影响因素[J]. 生态学报,2004,24(3):469-476.
[25]NAVAS A,GASPAR L,QUIJANO L,et al. Patterns of soil organic carbon and nitrogen in relation to soil movement under different land uses in mountain fields(South Central Pyrenees)[J]. Catena,2012,94(94):43-52.
[26]LIANG Q,CHEN H,GONG Y,et al. Effects of 15 years of manure and inorganic fertilizers on soil organic carbon fractions in a wheat-maize system in the North China Plain[J]. Nutrient cycling in agroecosystems,2012,92(1):21-33.
[27]刘艳丽,李成亮,高明秀,等. 不同土地利用方式对黄河三角洲土壤物理特性的影响[J]. 生态学报,2015,35(15):5 183-5 190.
[28]张阳. 黄河下游典型土地利用方式下土壤碳、氮分布与变化机制研究[D]. 开封:河南大学,2015.
[29]HESHMATI M,ARIFIN A,SHAMSHUDDIN J,et al. Predicting N,P,K and organic carbon depletion in soils using MPSIAC model at the Merek catchment,Iran[J]. Geoderma,2012,s 175/176(3):64-77.
[30]宋金明,李学刚,邵君波,等. 南黄海沉积物中氮、磷的生物地球化学行为[J]. 海洋与湖沼,2006,37(4):370-376.
[31]王晓燕,王一峋,王晓峰,等. 密云水库小流域土地利用方式与氮磷流失规律[J]. 环境科学研究,2003,16(1):30-33.
[32]杨艳芳,邵婷,吕梦宇,等. 龙窝湖湿地不同土地利用方式土壤养分和重金属污染特征[J]. 生态学杂志,2014,33(5):1 312-1 318.

相似文献/References:

[1]谢 云,王延华,杨 浩.滇池西白沙小流域沉积物重金属污染及来源研究[J].南京师范大学学报(自然科学版),2017,40(04):120.[doi:10.3969/j.issn.1001-4616.2017.04.020]
 Xie Yun,Wang Yanhua,Yang Hao.Pollution and Sources Study of Heavy Metals in Sediments ofXi Baisha Small Watershed in Dianchi[J].Journal of Nanjing Normal University(Natural Science Edition),2017,40(04):120.[doi:10.3969/j.issn.1001-4616.2017.04.020]

备注/Memo

备注/Memo:
收稿日期:2017-01-13.
基金项目:国家自然科学基金(41673107)、南京师范大学百人计划项目(184080H20181)、南京师范大学青蓝工程(184080H10330).
通讯联系人:王延华,教授,研究方向:流域生态环境演变. E-mail:wangyanhua@njnu.edu.cn
更新日期/Last Update: 2017-12-30