陶瓷杯与蒸渗仪测定硝态氮和氨态氮淋溶的比较

干旱区地理 ›› 2015, Vol. 38 ›› Issue (2): 298-304.

陶瓷杯与蒸渗仪测定硝态氮和氨态氮淋溶的比较

王琦¹，张恩和²，师尚礼¹，刘青林²，Keith Cameron³

（1 甘肃农业大学草业学院，甘肃兰州 730070； 2 甘肃农业大学农学院，甘肃兰州 730070；3 Centre for Soil and Environmental Research，Lincoln University，Canterbury，New Zealand）

收稿日期:2014-09-08 修回日期:2014-12-01 出版日期:2015-03-25
作者简介:王琦（1970-），男，甘肃陇西人，博士，副教授，主要从事草坪、作物和牧草节水技术研究. Email：wangqigsau@gmail.com
基金资助:
国家自然基金（41161090）

Comparison of lysimeters and porous ceramic cups for measuring nitrate and ammonium leaching in different soil types

WANG Qi¹，ZHANG En-he²，SHI Shang-li¹，LIU Qing-lin²，Keith CAMERON³

（1 College of Grassland Science，Gansu Agricultural University，Gansu Province，China；2 Agronomy College，Gansu Agricultural University，Gansu Province，China；3 Centre for Soil and Environmental Research，Lincoln University，Canterbury，New Zealand）

Received:2014-09-08 Revised:2014-12-01 Online:2015-03-25

摘要/Abstract

摘要： 土壤硝态氮（NO₃^--N）和氨态氮（NH4+-N）淋溶量测定方法因草本植物和土壤类型不同而异。试验采用陶瓷杯（ceramic suction cups）和蒸渗仪（lysimeters）分别测定草地土壤NO₃^--N和NH4+-N淋溶量。蒸渗仪直径为50 cm和深度为70 cm，土壤类型分别为新西兰Gorge silt loam、Mataura sandy loam和Lismore stony silt loam，重复4次。陶瓷杯水平插入蒸渗仪不锈钢筒，陶瓷杯插孔中心离不锈钢筒底部距离分别为35 cm（上陶瓷杯）和60 cm（下陶瓷杯）。在试验前，喷灌72 h冲洗蒸渗仪土壤溶液，使淋溶液NO₃^--N浓度接近0 mg·L^-1，然后1次性施加250 kg N·hm^-2尿素溶解液，用喷灌系统喷灌蒸渗仪，每周喷灌1次，喷灌系统误差使Gorge、Mataura和Lismore土壤喷灌强度分别为15.0、19.0和18.7 mm·h^-1，1次喷灌持续时间为3 h。在Gorge和Lismore土壤，陶瓷杯和蒸渗仪测定NO₃^--N淋溶量差异显著。在Gorge土壤，上陶瓷杯、下陶瓷杯和蒸渗仪测定NO₃^--N淋溶累计量分别为64、68和54 kg N·hm^-2，测定NH₄⁺-N淋溶累计量分别为0.43、0.49和0.43 kg N·hm^-2；在Mataura土壤，上陶瓷杯、下陶瓷杯和蒸渗仪测定NO₃^--N淋溶累计量分别为57、68和62 kg N·hm^-2，测定NH₄⁺-N淋溶累计量分别为0.51、0.37和0.23 kg N·hm^-2；在Lismore土壤，上陶瓷杯、下陶瓷杯和蒸渗仪测定NO₃^--N淋溶累计量分别为61、103和99 kg N·hm^-2，测定NH₄⁺-N淋溶累计量分别为1.70、2.24和2.04 kg N·hm^-2。在结构发育良好的Gorge和Lismore土壤，陶瓷杯不适合测定NO₃^--N淋溶量，但适合应用于砂土质地和发育不完善Mataura土壤。NH₄⁺-N淋溶累计量占NO₃^--N淋溶累计量的0.37%～2.93%，在测定和计算氮淋溶时，NH₄⁺-N淋溶可以忽略不计。

关键词: 硝态氮, 氨态氮, 淋溶, 测定方法

Abstract: The measurement of nitrate and ammonium leaching varied with plant species and soil types. This study compared 2 methods of measuring nitrate and ammonium leaching （lysimeters versus ceramic suction cups） using 12 soil monolith lysimeters （50 cm diameter and 70 cm deep） containing 4 replicates of 3 contrasting New Zealand soils：Gorge silt loam，Mataura sandy loam （both stone-free soils） and Lismore stony silt loam. The ceramic suction cups were installed at 35 cm （top cups） and 60 cm （bottom cups） depths. Sprinkler irrigation applied on lysimeters to minimize the NO₃^--N content of drainage water close to 0 mg·L-1，before experiments starting. Urea solution was surface applied at 250 kg N·hm^-2，followed by regular weekly irrigation. Due to small variations in irrigation nozzle application rates，the actual 3 hour irrigation totals measured were 45 mm，57 mm and 56 mm for the Gorge，Mataura and Lismore soils，respectively. There were significant differences between the cumulative leaching loss measured in the lysimeter drainage and values estimated from the cups in the Gorge and Lismore soils. The cumulative leaching loss，measured from the top cups，bottom cups and lysimeter drainage，were 64，68 and 54 kg N·hm^-2 of nitrate and 0.43，0.49 and 0.43 kg N·hm^-2 of ammonium，respectively，in the Gorge soil；57，68 and 62 kg N·hm-2 of nitrate and 0.51，0.37 and 0.23 kg N·hm^-2 of ammonium，respectively，in the Mataura soil; and 61，103 and 99 kg N·hm^-2 of nitrate and 1.70，2.24 and 2.04 kg N·hm^-2 of ammonium，respectively，in the Lismore soil. It was concluded that suction cups were inappropriate for the determination of cumulative leaching in the structured Gorge soil and the Lismore soil，but ceramic cups could provide useful data on cumulative leaching in the Mataura sandy loam soil. The cumulative ammonium leaching accounted for 0.37%-2.93% of the cumulative nitrate leaching in different soil types，and ammonium leaching could be neglected in measuring of nitrogen leaching.

Key words: nitrate, ammonium, leaching, methods of measurement

中图分类号:

S153.6

王琦，张恩和，师尚礼，刘青林，Keith Cameron. 陶瓷杯与蒸渗仪测定硝态氮和氨态氮淋溶的比较[J]. 干旱区地理, 2015, 38(2): 298-304.

WANG Qi，ZHANG En-he，SHI Shang-li，LIU Qing-lin，Keith CAMERON. Comparison of lysimeters and porous ceramic cups for measuring nitrate and ammonium leaching in different soil types[J]. , 2015, 38(2): 298-304.

参考文献

［1］ YANG J F，Li B Q，LIU S P. A large weighing lysimeter for evapotranspiration and soil-water-groundwater exchange studies ［J］. Hydrological Processes，2000，14：1887-1897.

［2］ CHRISTINE L. Lysimeter stations and soil hydrology measuring sites in Europer-purpose，equipment，research results，future developments［D］. Austria：School of Natural Sciences at the Karl-Franzens-University Graz，2004.

［3］ DI H J，CAERON K C. The use of a nitrification inhibitor. dicyandiamide （DCD），to decrease nitrate leaching and nitrous oxide emissions in a simulated grazed and irrigated grassland［J］.Soil Use and Management，2002，18：395-403.

［4］ DI H J，CAMERON K C. Reducing environmental impacts of agriculture by using a fine particle suspension nitrification inhibitor to decrease nitrate leaching from grazed pastures［J］. Agriculture，Ecosystems and Environment，2005，109：202-212．

［5］ DERBY N E，KNIGHTN R E，MONTGOMERY B R. Construction and performance of large soil core lysimeters［J］. Soil Science Society of America Journal，2002，66：1446-1453.

［6］赵长盛，胡承孝，黄魏，等. 大型蒸渗仪的设计、建造与安装［J］.农业工程学报，2010，26（2）：48-53.

［7］ SHINONAGE T，SCHIMMACK W，GERZAMEK M H. Vertical migration of 60Co，137Cs and 226Ra in agricultural soils as observed in lysimeters under crop rotation［J］. Journal of Environmental Radioactivity，2005，79：93-106．

［8］ CAMERON K C，SMITH N，MCLAY C D A，et al. Lysimeters without edge flow: An improved design and sampling procedure ［J］. Soil Science Society of America Journal，1992，56（5）：1625-1628．

［9］ CARRICK S. The dynamic interplay of mechanisms governing infiltration into structured and layered soil columns［D］. Canterbury，New Zealand：Lincoln University，2009.

［10］王胜佳，王家玉，陈义. 稻田土壤氮素淋失的形态及剖面分布特征［J］. 浙江农业学报，1997，9（2）：57-61.

［11］ CORWIN D L. Evaluation of a simple lysimeter-design medication to minimize sidewall flo［J］. Journal of Contaminant Hydrology，2000，42：35-49.

［12］ CARRICK S，BUCHAN G，ALMOND P，et al. Atypical early- time infiltration into a structured soil near field capacity：The dynamic interplay between sorptivity，hydrophobicity and air encapsulation［J］. Geoderma，2011，160：579-589.

［13］ CARRICK S，ALMOND P，BUCHAN G，et al. In situ characterization of hydraulic conductivities of individual soil profile layers during infiltration over long time periods［J］. European Journal of Soil Science，2010，61：1056-1069.

［14］ WEBSTER C P，SHEPHERD M A，GOULDING K W T，et al．Comparisons of methods for measuring the leaching of mineral nitrogen from arable land ［J］．Journal of Soil Science，1993，44:49-62．

［15］ MCLEOD M，AISLABIE J，RYBUNR J，MCGILL A．Regionalizing potential for microbial bypass flow through New Zealand soils ［J］．Journal of Environmental Quality，2008，37: 1959-1967．

［16］ LORD E I and SHEPHERD M A．Developments in the use of porous ceramic cups for measuring nitrate leaching ［J］．Journal of Soil Science，1993，44:435-449．

［17］ POSS R，NOBLE A D，DUNIN F X，et al．Evaluation of ceramic cup samplers to measure nitrate leaching in the field ［J］．European Journal of Soil Science，1995，46: 667-674．

［18］ GOULDING K W T and WEBSTER C P. Methods for measuring nitrate leaching［J］. Aspects of Applied Biology，1992，30：63-70.

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