秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响

师澜峰; 米彩红; 郭成久; 王瑄; 周丽丽; 许秀泉; 刘菁华

doi:10.13870/j.cnki.stbcxb.2018.06.040

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秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响

更新时间：2025-03-12

- 秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响
- Effect of Straw Biochar on Vertical Migration of Inorganic Nitrogen and Phosphate in Surface Layer of Black Soil During Freezing and Thawing Period
- 水土保持学报 2018年32卷第6期页码：278-285
- 作者机构：
  
  沈阳农业大学水利学院,沈阳,110866
- 作者简介：
  
  [ "师澜峰(1993-)男,硕士研究生,主要从事水土流失与农业面源污染防治研究。E-mail:1051493339@qq.com" ]
- 基金信息：
  
  国家自然科学基金项目（41471225）辽宁省博士科研启动基金项目（201601105）
- DOI：10.13870/j.cnki.stbcxb.2018.06.040
  中图分类号： S158;S155.2
- 纸质出版：2018
- 稿件说明：
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师澜峰, 米彩红, 郭成久, 等. 秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响[J]. 水土保持学报, 2018,32(6):278-285.

SHI Lanfeng, MI Caihong, GUO Chengjiu, et al. Effect of Straw Biochar on Vertical Migration of Inorganic Nitrogen and Phosphate in Surface Layer of Black Soil During Freezing and Thawing Period[J]. 2018, 32(6): 278-285.
师澜峰, 米彩红, 郭成久, 等. 秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响[J]. 水土保持学报, 2018,32(6):278-285. DOI： 10.13870/j.cnki.stbcxb.2018.06.040.

SHI Lanfeng, MI Caihong, GUO Chengjiu, et al. Effect of Straw Biochar on Vertical Migration of Inorganic Nitrogen and Phosphate in Surface Layer of Black Soil During Freezing and Thawing Period[J]. 2018, 32(6): 278-285. DOI： 10.13870/j.cnki.stbcxb.2018.06.040.

摘要

为研究秸秆生物炭输入对冻融期黑土表层无机氮磷垂直迁移的影响，采用室内模拟冻融循环试验，设置冻融与不冻融、冻融循环次数和生物炭施加量3个影响因素，分析冻融作用下不同秸秆生物炭输入量土壤表层无机氮磷垂直迁移特征。结果表明：（1）冻融与不冻融、冻融循环次数及生物炭施加量对黑土表层NO3-—N、NH4+—N和PO43-—P垂直迁移液总体积、迁移液总浓度及迁移总量均有极显著影响。（2）淋溶时间随冻融作用增强而缩短，随生物炭施加量增加而延长。所有处理迁移液总体积均随生物炭输入量的增加呈降低趋势。未冻融组迁移液总体积随培养期增加呈现缓慢下降趋势，冻融组处理迁移液总体积在第5次冻融循环试验出现急剧增加，而后趋于平稳。（3）分析冻融作用下秸秆生物炭施入对无机氮磷垂直迁移累积影响，同一控制时间内生物炭对冻融组无机氮磷垂直迁移量的抑制作用大于不冻融组，且随生物炭施入量增加对无机氮磷垂直迁移的抑制作用增强。由于土壤物理性质的改变，冻融组NO3-—N、NH4+—N和PO43-—P累积迁移量均在第5次冻融循环左右发生急剧变化。综上可知，生物炭在冻融期可以有效的固持养分，研究结果可为寒冷地区解冻期面源污染防治提供一定的理论支持。

Abstract

In order to explore the effect of straw biochar on vertical migration of inorganic nitrogen and phosphorus in surface layer of black soil during freezing-thawing period.This research adopts the indoor simulation of freezing-thawing cycle experiment

set the freezing-thawing and not-freezing-thawing

freezing-thawing cycles

biochar apply three influence factors

to analyze the vertical migration characteristics of soil surface inorganic nitrogen and phosphorus under freezing-thawing with different straw biochar apply. (1) Results show black soil surface freezing-thawing and not-freezing-thawing

freezing-thawing cycles and biochar apply have significant effect on NO3--N

NH4+-N and PO43--P inorganic nitrogen and phosphorus migration liquid total volume

total concentration and total amount of migration through freezing-thawing and not-freezing-thawing

freezing-thawing cycles and biochar apply.(2) The leaching time was shortened with the increase of freeze-thaw action and prolonged with the increase of biochar application.All treatments of inorganic nitrogen and phosphorus migration liquid volume show a decrease trend with the increase of biochar input. The total volume of migration liquid in not-freezing-thawing group show a slowly decrease trend as the incubation period increase. The total volume of the migration liquid volume in the freezing-thawing group increases sharply in the 5th freezing-thawing cycle test

and then became stable. (3) The effect of biochar on the vertical migration and accumulation of inorganic nitrogen and phosphorus under freeze-thaw action was analyzed. During the same control period

the inhibition of biochar on the vertical migration of inorganic nitrogen and phosphorus in the freeze-thaw group was greater than that in the non-freeze-thaw group.Because of changes in the physical properties of the soil

the accumulated migration of the freezing-thawing group NO3--N

NH4+-N and PO43--P changed dramatically around the fifth freezing-thawing cycle.To sum up

biochar can effectively retain nutrients during freezing-thawing period

and the research results can provide some theoretical support for the prevention and control of rural surface pollution during thawing period in cold regions.

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references

陈哲,杨世琦,张晴雯,等.冻融对土壤氮素损失及有效性的影响[J].生态学报,2016,36(4):1083-1094.

叶照金,廖敏,黄宇,等.不同施肥管理模式对集雨区苗木地径流氮素流失的影响[J].水土保持学报,2016,30(6):30-37.

范昊明,张瑞芳,周丽丽,等.气候变化对东北黑土冻融作用与冻融侵蚀发生的影响分析[J].干旱区资源与环境,2009,23(6):48-53.

周丽丽,李婧楠,米彩红,等.秸秆生物炭输入对冻融期棕壤磷有效性的影响[J].土壤学报,2017,54(1):171-179.

龙天渝,刘祥章,刘佳.紫色土坡耕地硝态氮随壤中流迁移的时空分布模拟[J].农业环境科学学报,2015,34(10):1973-1978.

华文杏,范昊明,许秀泉,等.东北坡耕地春季融雪侵蚀观测研究[J].水土保持学报,2017,31(2):92-96.

车明轩,宫渊波, Muhammad N K,等.不同雨强、坡度对秸秆覆盖保持水土效果的影响[J].水土保持学报,2016,30(2):131-135,142.

张千丰,王光华.生物炭理化性质及对土壤改良效果的研究进展[J].土壤与作物,2012,1(4):219-226.

William H, Philip R, James W. Effects of three different biochars on aggregate stability, organic carbon mobility and micronutrient bioavailability[J]. Journal of Environmental Management,2016,181:770-778.

邵婧宇.利用CT扫描分析冻融作用对表层黑土和棕壤结构的影响[D].沈阳:沈阳农业大学,2017.

李德明,郭成久,宁睿.初始含水量对黑土坡面养分流失的影响[J].水土保持学报,2014,28(5):17-20.

刘玉学,吕豪豪,石岩,等.生物质炭对土壤养分淋溶的影响及潜在机理研究进展[J].应用生态学报,2015,26(1):304-310.

陈温福,张伟明,孟军.农用生物炭研究进展与前景[J].中国农业科学,2013,46(16):3324-3333.

Kameyama K, Miyamoto T, Shiono T, et al. Influence of sugarcane bagasse-derived biochar application on nitrate leaching in calcaric dark red soil[J]. Journal of Environmental Quality,2012,41(4):1131-1137.

郑博艺,范昊明.东北黑土区垄作农田寒季表土水分垂直变化特征[J].水土保持研究,2016,23(2):28-33.

马世伟.东北低山丘陵区季节性积雪特性研究[D].沈阳:沈阳农业大学,2017.

中华人民共和国国家质量监督检验检疫总局,中国国家标准化管理委员会.气体吸附BET法测定固态物质比表面积:GB/T 19587-2004[S].北京:中国标准出版社,2005.

周丽丽,马世伟,米彩红,等.冻融条件下土壤水分和速效磷垂直迁移规律[J].水土保持研究,2017,24(3):70-74.

刘佳,范昊明,周丽丽,等.冻融循环对黑土容重和孔隙度影响的试验研究[J].水土保持学报,2009,23(6):186-189.

李婧楠.冻融条件下不同秸秆还田方式对土壤有效磷影响研究[D].沈阳:沈阳农业大学,2017.

吴媛媛,杨明义,张风宝,等.添加生物炭对黄绵土耕层土壤可蚀性的影响[J].土壤学报,2016,53(1):81-92.

何绪生,耿增超,佘雕,等.生物炭生产与农用的意义及国内外动态[J].农业工程学报,2011,27(2):1-7.

靖彦,陈效民,李秋霞,等.生物质炭对红壤中硝态氮和铵态氮的影响[J].水土保持学报,2013,27(6):265-269.

Jackson-Blake L, Helliwell R C, Britton A J,et al. Controls on soil solution nitrogen along an altitudinal gradient in the Scottish uplands[J]. Science of the Total Environment,2012,431:100-108.

范志平,李胜男,李法云,等.冻融交替对河岸缓冲带土壤无机氮和土壤微生物量氮的影响[J].气象与环境学报,2013,29(4):106-111.

刘绪军,景国臣,杨亚娟,等.冻融交替作用对表层黑土结构的影响[J].中国水土保持科学,2015,13(1):42-46.

刘玮晶. 生物质炭对土壤中氮素养分滞留效应的影响[D].南京:南京农业大学,2012.

范昊明,靳丽,周丽丽,等.冻融循环作用对黑土有效磷含量变化的影响[J].水土保持通报,2015,35(3):18-22.

Edwards L M. The effect of alternate freezing and thawing on aggregate stability and aggregate size distribution of some Prince Edward Island soils[J]. European Journal of Soil Science,1991,42(2):193-204.

David L, Pierce F, Wang B Q, et al. Biochar impact on nutrient leaching from a Midwestern agricultural soil[J]. Geoderma,2010,158(3/4):436-422.

李卓瑞,韦高玲.不同生物炭添加量对土壤中氮磷淋溶损失的影响[J].生态环境学报,2016,25(2):333-338.

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