Effects of Biochar Additions on Moisture Content and Depletion of Loessial Soil

Ma Lingyun; Zhang Fengbao; Yang Jiayan; Li Yuanyuan; Yang Mingyi

doi:10.13961/j.cnki.stbctb.20230524.002

您当前的位置：

首页 >

文章列表页 >

Effects of Biochar Additions on Moisture Content and Depletion of Loessial Soil

- Effects of Biochar Additions on Moisture Content and Depletion of Loessial Soil
- Bulletin of Soiland Water Conservation Vol. 43, Issue 3, Pages: 25-33(2023)
- 作者机构：
  
  1. 西北农林科技大学水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌,712100
  2. 中国科学院水利部水土保持研究所, 陕西杨凌,712100
  3. 郑州大学农学院,河南,郑州,450001
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.20230524.002
  CLC： S152.7;S157.9
- Published：2023
- 稿件说明：
移动端阅览
Ma Lingyun, Zhang Fengbao, Yang Jiayan, et al. Effects of Biochar Additions on Moisture Content and Depletion of Loessial Soil[J]. Bulletin of Soiland Water Conservation, 2023, 43(3): 25-33.
DOI：

Ma Lingyun, Zhang Fengbao, Yang Jiayan, et al. Effects of Biochar Additions on Moisture Content and Depletion of Loessial Soil[J]. Bulletin of Soiland Water Conservation, 2023, 43(3): 25-33. DOI： 10.13961/j.cnki.stbctb.20230524.002.

摘要

[目的] 明确雨季生物炭添加对黄绵土储水、保水能力的影响，为科学利用生物炭改良黄土高原地区土壤以及确定合理的生物炭施用量提供基本理论支持。[方法] 采用多层一体式土壤水分温度测量系统(JDTS-01)对黄土高原地区土壤水分进行野外定点观测，并使用烘干法对监测数据进行校正，研究黄绵土0—40 cm土层水分动态变化与补给、消退情况。基于双变量相关分析探讨了不同生物炭添加量下土壤水分补给和消退变化的影响因素及其相对重要性。[结果] ①整体上生物炭添加能在一定程度上增加土壤水分含量，低生物炭添加量增加了深层土壤水分，而高生物炭添加量增加了表层土壤水分，2.5%左右的生物炭添加量可能是影响土壤水分入渗和蒸发的拐点。②添加生物炭后，0—20 cm土层水分补给量增大，20—40 cm土层水分补给量减小。降雨带来的水分补给能够很大程度上滞留在土壤耕层，添加生物炭量较大时土壤水分补给效果更好；0—20 cm土层中添加生物炭处理的水分消退更快，而不添加生物炭的土壤水分入渗土层更深。③生物炭添加可以促进黄绵土土壤水分补给，减弱土壤水分消退，有利于降雨后土壤储水。[结论] 生物炭添加能够改善黄土高原地区土壤水分入渗特性，减小土壤水分深层入渗量和增加耕层土壤储水量，在添加量大于4%时效果更显著。

Abstract

[Objective] The influence of biochar additions on water storage and water retention capacity of loessial soil during the rainy season was clarified in order to provide basic theoretical support for the scientific use of biochar and to improve soil on the Loess Plateau and determine the reasonable amount of biochar application.[Method] A multi-layer integrated soil moisture-temperature measurement system (JDTS-01) was used to make fixed point observations of soil moisture in a Loess Plateau field. The measured data were corrected by the field correction method. The dynamic change

recharge

and regression of water in the 0-40 cm soil layer were studied. Bivariate correlation analysis was conducted to determine the influencing factors and the relative importance of soil water recharge and regression under different levels of biochar addition.[Results] ① Low biochar content increased deep soil moisture

while high biochar content increased surface soil moisture. On the whole

biochar additions increased soil moisture content. A biochar content of 2.5% may be the inflection point affecting soil water infiltration and evaporation. ② After the addition of biochar

the water content in 0-20 cm soil layer increased

and the water content in 20-40 cm soil layer decreased. The water addition occurring due to rainfall could largely remain in the soil surface layer

and this effect on surface soil water content was greater when the biochar addition was larger. Water in the 0-20 cm soil layer with biochar dissipated faster

while the water in the soil without biochar penetrated deeper into the soil layer. ③ The addition of biochar can promote soil water recharge and weaken soil water regression

thereby increasing loessial soil water storage after rainfall.[Conclusion] Biochar additions can improve loessial soil water infiltration characteristics

reduce deep infiltration of soil water

and increase soil water storage in the topsoil on the Loess Plateau. These effects of biochar additions were more significant when the addition levels were greater than 4%.

关键词

Keywords

references

邵明安,贾小旭,王云强,等.黄土高原土壤干层研究进展与展望[J].地球科学进展,2016,31(1):14-22.

Lehmann J, Joseph S. Biochar for Environmental Management:Science, Technology and Implementation[M]. Routledge, 2015.

Chan K Y, Van Zwieten L, Meszaros I, et al. Agronomic values of greenwaste biochar as a soil amendment[J]. Soil Research,2007,45(8):629.

Karami N, Clemente R, Moreno-Jiménez E, et al. Efficiency of green waste compost and biochar soil amendments for reducing lead and copper mobility and uptake to ryegrass[J]. Journal of Hazardous Materials, 2011,191(1/2/3):41-48.

Blanco-Canqui H. Biochar and soil physical properties[J]. Soil Science Society of America Journal,2017,81(4):687-711.

Yi Susan, Chang N Y, Imhoff P T. Predicting water retention of biochar-amended soil from independent measurements of biochar and soil properties[J]. Advances in Water Resources,2020,142:103638.

王艳阳,魏永霞,孙继鹏,等.不同生物炭施加量的土壤水分入渗及其分布特性[J].农业工程学报,2016,32(8):113-119.

王麒翔,范晓辉,王孟本.近50年黄土高原地区降水时空变化特征[J].生态学报,2011,31(19):5512-5523.

伍永秋,刘宝元,Erikvanden E,等.黄土高原土壤水分的自动监测:TDR系统及其应用[J].水土保持学报,2001,15(2):108-111.

吴奇凡.黄土高原陆地水储量变化归因分析及区域尺度地下水补给[D].陕西杨凌:西北农林科技大学,2019.

杨磊,张涵丹,陈利顶.黄土宽梁缓坡丘陵区次降雨对土壤水分补给效率与阈值研究[J].中国科学:地球科学,2018,48(4):457-466.

王柏,孙艳玲,于艳梅.玉米滴灌水肥一体化条件下土壤水分迁移规律试验研究[J].水利科学与寒区工程,2019,2(6):21-26.

雷志栋,胡和平,杨诗秀.土壤水研究进展与评述[J].水科学进展,1999,10(3):311-318.

赵西宁,吴发启.土壤水分入渗的研究进展和评述[J].西北林学院学报,2004,19(1):42-45.

De Almeida W S, Panachuki E, de Oliveira P T S, et al. Effect of soil tillage and vegetal cover on soil water infiltration[J]. Soil and Tillage Research, 2018,175:130-138.

潘云,吕殿青.土壤容重对土壤水分入渗特性影响研究[J].灌溉排水学报,2009,28(2):59-61.

高海英,何绪生,耿增超,等.生物炭及炭基氮肥对土壤持水性能影响的研究[J].中国农学通报,2011,27(24):207-213.

李帅霖,王霞,王朔,等.生物炭施用方式及用量对土壤水分入渗与蒸发的影响[J].农业工程学报,2016,32(14):135-144.

房彬,李心清,赵斌,等.生物炭对旱作农田土壤理化性质及作物产量的影响[J].生态环境学报,2014,23(8):1292-1297.

李卓,吴普特,冯浩,等.容重对土壤水分入渗能力影响模拟试验[J].农业工程学报,2009,25(6):40-45.

Zhou H, Fang H, Zhang Q, et al. Biochar enhances soil hydraulic function but not soil aggregation in a sandy loam[J]. European Journal of Soil Science,2019,70(2):291-300.

李元元.生物炭添加对黄绵土坡面土壤侵蚀的影响及机制研究[D].陕西杨凌:西北农林科技大学,2021.

Kookana R S, Sarmah A K, Van Zwieten L, et al. Biochar application to soil[M]//Advances in Agronomy.Amsterdam:Elsevier,2011:103-143.

朱志龙.土壤水分消退规律分析[J].水文,1994,14(4):36-39.

季志恒,樊福来.土壤水消退的时空变化规律分析[J].水文,2003,23(1):23-27.

Laird D A, Brown R C, Amonette J E, et al. Review of the pyrolysis platform for coproducing bio-oil and biochar[J]. Biofuels,Bioproducts and Biorefining,2009,3(5):547-562.

陈新均,王学全,卢琦,等.季节性河道土壤水分及其渗漏特征初探[J].干旱区研究,2020,37(1):97-104.

Views

593

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Effects of organic material addition on organic carbon fractions in black loessial and loessial soils

Regional characteristics of soil moisture and nutrients under artificial forests in typical loess regions

Influence of microtopography on spatiotemporal distribution of soil moisture during snowmelt period and short-term prediction

Effects of vegetation restoration duration on runoff and sediment yield in slopes of waste dumps in alpine mining areas

Research progress on microbial-biochar interaction mechanisms in saline-alkali soil improvement

Related Author

Zhao Huanhuan

Xu Chenyang

Li Jiangwen

Wang Dandan

Hu Feinan

Ma Chi

Mo Baoru

Ma Quanlin

Related Institution

College of Natural Resources and Environment， Northwest A&F University， Yangling

College of Soil and Water Conservation Science and Engineering，Northwest A&F University， Yangling

State Key Laboratory of Soil and;Water Conservation and Desertification Control， Institute of Soil and Water Conservation， Chinese Academy of;Sciences and Ministry of Water Resources， Yangling

Key Laboratory of Plant Nutrition and;Agri-Environment in Northwest China， Ministry of Agriculture and Rural Affairs， Yangling

Gansu Academy of Forestry

⁰