共查询到20条相似文献，搜索用时 203 毫秒
1.
三江平原寒地稻田CH_4、N_2O排放特征及排放量估算 总被引：3，自引：1，他引：3
利用静态暗箱-气相色谱法,于2003-2006年对三江平原寒地稻田CH4、N2O通量进行了为期4年的田间原位观测研究.结果表明:三江平原寒地稻田CH4和N2O排放具有明显的季节变化,水稻生长季淹水期是CH4排放的强源,稻田排水后CH4排放显著下降,休闲期CH4排放微弱或呈弱吸收汇,整个生长季CH4排放呈现单峰型态,并随水稻植株生长和叶面积指数而变化;水稻生长季和休闲期N2O排放通量都很小,冬季休闲期有时还出现微弱的吸收现象.生长季一般在施肥和表土落干时都会出现不同强度的排放峰,除了几次比较显著的排放峰值外,其它淹水状态下N2O排放很弱;温度和土壤水分状况是影响稻田CH4和N2O排放的重要因子,稻田积水深度和气体排放无明显的相关性;水稻植株对稻田土壤CH4排放起促进作用而对稻田土壤N2O排放起抑制作用;稻田氮肥用量增加可以降低土壤CH4排放,但却增加了N2O的排放.根据试验数据对三江平原地区寒地稻田CH4和N2O排放总量估算值分别为0.1035 Tg/a和0.0021 Tg/a. 相似文献
2.
太湖地区不同水旱轮作方式下稻季甲烷和氧化亚氮排放研究 总被引：15，自引：0，他引：15
为准确编制我国稻田温室气体排放清单及制定合理减排措施提供基础数据,选择太湖地区典型水稻种植区江苏省苏州市,研究设计了休闲水稻(对照,CK)、紫云英水稻(T1)、黑麦草水稻(T2)、小麦水稻(T3)和油菜水稻(T4)5种水旱轮作方式,采用静态箱气相色谱法,开展了不同水旱轮作方式下水稻生长季田间甲烷(CH4)和氧化亚氮(N2O)排放监测试验。试验结果表明:不同水旱轮作方式下水稻生长季CH4排放通量呈先升高后降低的变化趋势,CH4排放峰值出现在水稻生育前期,移栽至有效分蘖临界叶龄期CH4累积排放量占全生育期排放总量的比例为65%~81%,而N2O仅在水稻烤田期间有明显排放。水旱轮作方式对稻季CH4和N2O排放有极显著(P 0.01)影响,CH4季节总排放量表现为T1(283.2 kg.hm 2)CK(139.5 kg.hm 2)T3(123.4kg.hm 2)T4(114.7 kg.hm 2)T2(100.8 kg.hm 2),N2O季节总排放量顺序为T1 T4 T3 T2 CK,依次为1.06kg.hm 2、0.87 kg.hm 2、0.81 kg.hm 2、0.72 kg.hm 2和0.53 kg.hm 2。T1处理稻季排放CH4和N2O产生的增温潜势最高[7 396 kg(CO2).hm 2],显著(P 0.05)高于其他处理,比CK[3 646 kg(CO2).hm 2]增加103%,T2[2 735kg(CO2).hm 2]较CK减少25%(P 0.05)。紫云英水稻轮作方式增加了太湖地区水稻生长季的温室效应。 相似文献
3.
于2008年采用静态暗箱-气相色谱法对人工手插和机插2种水稻种植方式下CH4和N2O排放进行田间观测,研究稻麦轮作条件下机插水稻CH4和N2O的排放特征及其温室效应。结果表明,水稻生长季CH4排放通量人工手插水稻和机插水稻均呈先升高后降低的变化趋势,N2O仅在水稻搁田期间有明显排放,机插和人工手插水稻CH4平均排放通量分别为4.68、4.39 mg.m-2.h-1,N2O平均排放通量为92.80、111.33μg.m-.2h-1。与人工手插水稻相比,机插水稻增加CH4排放总量14%,减少N2O排放总量11%,使稻季排放CH4和N2O所产生的全球增温潜势（GWP）和＂单位产量的GWP＂分别提高8%和10%。在稻麦轮作条件下采用机插水稻种植方式,水稻生长期间排放的CH4和N2O所形成的温室效应有提高的趋势。 相似文献
4.
通过静态箱-气相色谱法,研究了崇明岛稻麦轮作地水稻生长季及收割后休耕期（2011年6月至2011年11月）温室气体CO2、CH4和N2O的排放、吸收规律及交换量,并运用增温潜势进行了温室效应估算。3种温室气体通量在水稻不同生长阶段有明显差异：稻田除成熟收割期外,其他期均表现为CH4排放源,并在分蘖期达到最大值;N2O除幼苗期表现为汇,其他期均为排放源,并在拔节期达到最大值。温室效应分析得出：水稻田温室气体以CH4和N2O排放为主,二者对全球温室效应的贡献为3.255×103kgCO2·hm-2;由于光合作用,稻田表现为对CO2固定,固定量为2.462×103kgCO·2hm-2;崇明水稻生长季排放温室气体综合GWP值为793kgCO·2hm-2,为温室气体排放源。 相似文献
5.
不同灌溉模式下寒地稻田CH_4和N_2O排放及温室效应研究 总被引：3，自引：0，他引：3
为了研究寒地稻田CH4和N2O排放特征,选取黑龙江省寒地稻田为研究对象,采用静态箱—气相色谱法对控制灌溉、间歇灌溉、浅湿灌溉及淹灌四种水分管理模式等4个处理的CH4和N2O排放通量进行观测。结果表明,不同灌溉模式下的CH4和N2O排放高峰均出现在水稻生长旺季,而休闲期内排放较少。相对于淹灌,浅湿灌溉稻田CH4累积排放量降低了27.2%,控制灌溉处理的降低了34%,间歇灌溉处理的降低了48.2%。长期淹灌稻田N2O排放量比间歇灌溉稻田减少0.41kg/hm2,比控制灌溉稻田增加0.38kg/hm2,比浅湿灌溉稻田增加0.37kg/hm2。总体温室效应分析,节水灌溉模式能有效抑制温室气体的排放并显著地降低CH4和N2O的总温室效应。水稻生育期内,CH4排放量减少时期,N2O排放量有增加趋势,综合考虑CH4和N2O排放的消长关系,才能有效减缓稻田温室气体的排放。 相似文献
6.
由于土壤水分状况的不同,水稻生长季土壤N2O排放量明显不同于旱地作物。基于多元统计模型,通过多点代面的方法进行尺度扩展,并应用蒙特卡洛方法模拟影响因素的变异程度,模拟了中国稻田水稻生长季的N2O排放情况。所模拟的378个点的水稻生长季N2O排放通量为6.0～74.3μgN.m-2.h-1,其均值接近于原始观测结果;378个点位的N2O排放通量空间分布不均,排放量较高的点位于北纬20°到30°之间;378个点中单季稻、稻-旱轮作中的水稻和双季稻的生长季N2O平均排放量分别占年总排放量的53%、34%和59%。多点代面的尺度扩展结果显示2008年中国稻田水稻生长季N2O排放量均值为22.48Gg,其95%的概率区间为20.5～24.8Gg;化肥氮的N2O排放系数为0.27%,与IPCC缺省值0.3%接近。用秩相关关系表征影响因子对中国稻田水稻生长季N2O排放量的不确定性的贡献,结果表明水分管理类型、有机肥类型、土壤属性、氮用量等对结果均有显著影响。 相似文献
7.
控制灌溉稻田的甲烷减排效果 总被引：3，自引：2，他引：1
为探讨节水灌溉水分调控对稻田甲烷（CH4）排放的影响,寻找节水减排的稻田灌溉模式,依据5a田间原位观测资料,分析控制灌溉稻田CH4排放规律及其减排效果。结果表明,控制灌溉稻田稻季CH4排放量为1.07±0.17 g/m2,较淹水灌溉稻田（6.49±0.17 g/m2）降低83.5%,差别极显著。本研究得到的中国东南部稻田稻季和全年CH4排放量均低于已有报道中的中国稻田CH4排放量,其中控制灌溉稻田全年CH4排放量低于世界大部分地区稻田。根据本研究结果估算中国稻田CH4排放总量为2.06 Tg/a,大面积推广控制灌溉后,中国稻田CH4排放量还将进一步下降。控制灌溉模式显著影响水稻全生育期稻田CH4排放通量的变化,削峰效果显著。控制灌溉稻田CH4排放通量在返青期至分蘖中期（移栽后18 d内）逐渐上升至最大值,然后逐渐减小,从水稻分蘖后期（移栽后21 d）开始至生育期结束均维持在较低水平。控制灌溉稻田CH4排放通量峰值为3.69 mg/m2·h,较淹水灌溉稻田降低69.0%。在持续降雨的作用下,控制灌溉和淹水灌溉模式下稻田CH4排放通量均呈现下降趋势。控制灌溉模式的土壤水分调控,使稻田经历一系列的脱水过程,改变了根层土壤的水气状况,减小了稻田CH4排放。控制灌溉模式在水稻全生育期的应用可显著地减少稻田CH4排放。 相似文献
8.
生物质炭还田对稻田甲烷的减排效果 总被引：8，自引：6，他引：8
为探讨不同生物质炭类型、输入量、还田时间和还田深度等因素作用下的CH4排放特征,采用静态箱-气相色谱法,通过向稻田土壤中施用3种类型的生物质炭（稻秆炭、麦秆炭、竹炭）,开展了水稻一个生长周期的室内观测试验。结果表明,3种类型的生物质炭输入后,对比空白处理,水稻产量显著性增加（P<0.05）,其中竹炭处理每盆实粒质量高达18.12 g,说明施用生物质炭可增加水稻产量;竹炭施用后稻田土壤CH4排放通量（80 mg/m2 h）显著低于稻杆炭和麦杆炭处理（P<0.05）,而稻杆炭和麦杆炭处理无显著性差异（P>0.05）,但都显著高于空白处理（P<0.05）,说明施用生物质炭可有效减少CH4排放。CH4排放通量与生物质炭用量负相关,CH4的排放通量随着生物质炭用量的逐渐增加而降低。同时,水稻移植前施用竹炭CH4排放通量（56.6 mg/m2 h）低于空白（96 mg/m2 h）及水稻成活前后（73.4和76.6 mg/m2 h）,但无显著性差异（P>0.05）,这与土壤氧化还原电位（Eh）变化相一致,说明生物质炭施用时间对稻田土壤CH4排放通量影响不大。此外,不同竹炭还田深度下的土壤CH4排放通量顺序为：中部输入（15 cm处输入）<表层输入（5 cm处输入）<深部输入（25 cm处输入）<空白（不输入生物质炭）,说明生物质炭中部输入更适用微生物生长和CH4气体减排。该研究可为太湖地区苕溪流域稻田增汇和温室气体减排提供参考。 相似文献
9.
10.
稻田CH4和N2O综合排放对控制灌溉的响应 总被引：4，自引：6，他引：4
为了揭示水稻控制灌溉对稻田CH4和N2O综合排放的影响,该文采用静态暗箱-气相色谱法对控制灌溉稻田CH4和N2O排放进行原位观测,分析稻田CH4和N2O综合排放对控制灌溉水分调控的动态响应。结果表明,控制灌溉稻田CH4排放通量多低于常规灌溉稻田,且主要集中在水稻分蘖前期,峰值出现在土壤脱水后第1～2d,排放总量较常规灌溉稻田减少81.2%～82.8%;N2O排放通量多高于常规灌溉稻田,峰值出现在肥后且土壤脱水后3～4d,排放总量较常规灌溉稻田增加了121.8%～144.3%。控制灌溉稻田CH4和N2O的综合全球增温潜势较常规灌溉稻田显著减少(p<0.05),减少幅度为15.0%～34.8%。控制灌溉显著降低了稻田CH4和N2O的综合温室效应。 相似文献
11.
中国常年淹水稻田CH4排放量估算 总被引：4，自引：0，他引：4
A special kind of rice field exists in China that is flooded year-round. These rice fields have substantially large CH4 emissions during the rice-growing season and emit CH4 continuously in the non-rice growing season. CH4 emission factors were used to estimate the CH4 emissions from year-round flooded rice fields during the rice-growing season in China.The CH4 emissions for the year-round flooded rice fields in China for the rice growing season over a total area of 2.66 Mha were estimated to be 2.44 Tg CH4 year^-1. The uncertainties of these estimations are discussed as well. However,the emissions during the non-rice growing season could not be estimated because of limited available data. Nevertheless,methane emissions from rice fields that were flooded year-round could be several times higher than those from the rice fields drained in the non-rice-growing season. Thus, the classification of “continuously flooded rice fields”in the IPCC (International Panel on Climate Change) Guidelines for National Greenhouse Gas Inventories is suggested to be revised and divided into “continuously flooded rice fields during the rice growing season” and “year-round flooded rice fields”. 相似文献
12.
Methane emission from paddy fields in Taiwan 总被引：3，自引：0，他引：3
In order to investigate the effect of environmental conditions on CH4 emission from paddy fields in Taiwan, four locations, two cropping seasons and two irrigation systems were studied. CH4 emission was high at the active tillering and the booting stages in the first cropping season, whereas it was low at the
transplanting and the ripening stages with an intermittent irrigation system. CH4 emission was high at the transplanting stage in the second cropping season, and decreased gradually during rice cultivation.
Daily temperature and light intensity increased gradually during rice growth in the first cropping season (February–June),
while it was reversed in the second cropping season (August–December). The seasonal CH4 emission from paddy fields ranged from 1.73 to 11.70 g m–2, and from 10.54 to 39.50 g m–2 in the first and second cropping seasons, respectively. The seasonal CH4 emission in the second cropping season was higher than that in the first cropping season in all test fields. The seasonal
CH4 emission was 32.65 mg m–2 in the first cropping season of the National Taiwan University paddy field with continuous flooding, and it was 28.85 mg
m–2 in the second cropping season. The annual CH4 emission ranged from 12.3 to 49.3 g m–2 with an intermittent irrigation system, and the value was 61.5 g m–2 with a continuous flooding treatment. The annual CH4 emission from paddy fields was estimated to be 0.034 Tg in 1997 from 364,212 ha of paddy fields with an intermittent irrigation
system, which was less than the 0.241 Tg calculated by the IPCC method with a continuous flooding treatment
Received: 23 February 2000 相似文献
13.
水稻植株特性对稻田甲烷排放的影响及其机制的研究进展 总被引：6，自引：0，他引：6
水稻是我国最主要的口粮作物,稻田是重要温室气体甲烷的主要排放源之一。水稻植株特性既是水稻产量形成的关键因子,也是稻田甲烷排放的主要影响因子。但是,至今关于水稻植株对稻田甲烷排放的调控效应及其机制仍存在许多不一致的认识。为此,本文从形态特征、生理生态特征、植株-环境互作等方面,对现有的相关研究进行了综合论述。水稻地上部形态特征如分蘖数、株高、叶面积等对稻田甲烷排放的影响的研究结果不尽相同,起关键作用的是地下系统。优化光合产物分配在持续淹水的情况下可以减少稻田甲烷排放。提高水稻生物量在低碳土壤增加稻田甲烷排放,但在高碳土壤下降低甲烷排放。本文还明确了相关研究现状和存在的问题。在此基础上,作者认为未来应加强水稻根系形态及其生理特征,以及水稻植株-土壤环境(尤其是水分管理和养分管理)互作对稻田甲烷产生、氧化和排放影响的研究,在方法上应加强微区试验和大田试验的结合,并开展植株和稻田的碳氮互作效应及其机制研究,为高产低碳排放的水稻品种选育和低碳稻作模式创新提供理论参考和技术指导。 相似文献
14.
Yo Toma Shingo Oomori Asuka Maruyama Hideto Ueno Osamu Nagata 《Soil Science and Plant Nutrition》2016,62(1):69-79
Agricultural fields, including rice (Oryza sativa L.) paddy fields, constitute one of the major sources of atmospheric methane (CH4) and nitrous oxide (N2O). Organic matter application, such as straw and organic fertilizer, enhances CH4 emission from paddy fields. In addition, rice straw management after harvest regulates CH4 emissions in the growing season. The interaction of tillage times and organic fertilizer application on CH4 and N2O emissions is largely unknown. Therefore, we studied the effects of fallow-season tillage times and fertilizer types on CH4 and N2O emissions in paddy fields in Ehime, southwestern Japan. From November 2011 to October 2013, four treatments, two (autumn and spring) or one (spring) in the first year, or two (autumn and spring) or three (autumn, winter, and spring) in the second year times of tillage with chemical or organic fertilizer application, were established. Gas fluxes were measured by the closed-chamber method. Increasing the number of tillage times from one to two decreased succeeding CH4 emission and the emission factor for CH4 (EFCH4) in the rice-growing season, suggesting that the substrate for CH4 production was reduced by autumn and spring tillage in the fallow season. Higher EFCH4 [1.8–2.0 kg carbon (C) ha?1 d?1] was observed when more straw was applied (6.9–7.2 Mg ha?1) in the second year. Organic fertilizer application induced higher CH4 emission just after the application as basal and supplemental fertilizers, especially at a lower straw application rate. This indicated that EFCH4 in the organically managed fields should be determined individually. Organic fertilizer application with two tillage times induced N2O efflux during the rice-growing season in the second year, but N2O emissions were not affected by winter tillage. Although paddy fields can act as an N2O sink because of reduced soil conditions when straw application was high, application of organic C and nitrogen as fertilizer can enhance N2O production by the denitrification process during the growing season, especially in the ripening stage when soil anaerobic conditions became moderate. These results suggest that negative emission factors for N2O (EFN2O) can be applied, and EFN2O of organic fertilizer should be considered during the estimation of N2O emission in the paddy field. 相似文献
15.
Methane emission from flooded rice fields under irrigated conditions 总被引：11，自引：0，他引：11
T. K. Adhya Amarendra K. Rath P. K. Gupta V. R. Rao S. N. Das K. M. Parida D. C. Parashar N. Sethunathan 《Biology and Fertility of Soils》1994,18(3):245-248
In a study on CH4 emission from flooded rice fields under irrigated conditions, fields planted with rice emitted more methane than unplanted fields. The CH4 efflux in planted plots varied with the rice variety and growth stage and ranged from 4 to 26 mg h-1m-2. During the reproductive stage of the rice plants, CH4 emission was high and the oxidation power of rice roots, in terms of -naphthylamine oxidation, was very low. The CH4 emission reached a maximum at midday and declined to minimum levels at midnight, irrespective of the rice variety. The peak CH4 emission at midday was associated with higher solar radiation and higher soil/water temperature. 相似文献
16.
Fifteen upland soils collected from the major arable areas in NOrth China were used to assess the availability of soil sulfur(S) to plants in a pot experiment.Soils were extracted with various reagents and the extractable S was determined using turbidimetric method or inductively coupled plasma atomic emission spectrometry (ICP-AES),respectively.In addition,mineralizable organic S,organic S,N/S ratio,sulfur availability index(SAI) and available sulfur correction value(ASC) in soils were also determined.The S amout extracted by 1.5g L^-1 CaCl2 was nearly equivalent to that by 0.25mol L^-1 KCl(40℃),and both of them were slightly smaller than that by 0.01 molL^-1 Ca(H2PO4)2 solution,as measured by turbidimetric method or ICP-AES.The extractable S measured by turbidimetric method was consistently smaller than that by ICP-AES.All methods tested except that for organic S and N/S ratio produced satisfactoy results in the regression analyses of the relationships between the amounts of S extracted and plant dry matter weight and S uptake in the pot experiment,In general,0.01 mol L^-1 Ca(H2PO4)2-extracted S determined by ICP-AES or turbidimetric method and 0.25mol L^-1 KCl(40℃)-extracted S determined by ICP-AES appeared to be the best indicators for evaluation of soil available S. 相似文献
17.
稻田是大气温室气体甲烷(CH4)和氧化亚氮(N2O)的重要排放源, 稻田温室气体减排一直是生态农业研究的热点。目前, 采用水稻品种选择利用、水分控制管理、肥料运筹管理、耕作制度调整以及种养结合模式等方法来减少稻田温室气体排放有较好实践效应, 但不同稻田栽培环境(露地、网室)基础上的稻鸭共作对麦秸全量还田的稻田温室气体排放特征及相关土壤理化特性关联性的影响尚为少见。本研究采用裂区设计, 在两种栽培环境条件下, 以无鸭子放养的常规稻作和麦秸不还田为对照, 在等养分条件下分析麦秸全量还田与稻鸭共作模式对稻田土壤氧化还原电位、CH4排放量、产CH4潜力及CH4氧化能力、N2O排放量及N2O排放高峰期土壤反硝化酶活性、全球增温潜势、水稻产量的影响, 为稻田可持续生产和温室气体减排提供参考。结果表明, 麦秆还田增加了稻田产CH4潜力、提高了CH4排放量, 降低了稻田土壤反硝化酶活性、土壤氧化还原电位和N2O排放量, 整体上导致全球增温潜势上升96.89%~123.02%; 稻鸭共作模式, 由于鸭子的不间断活动提高了稻田土壤氧化还原电位, 降低了稻田产CH4潜力, 增强了稻田CH4氧化能力, 从而降低稻田CH4排放量, N2O排放量虽有提高, 整体上稻鸭共作模式的全球增温潜势较无鸭常规稻田下降8.72%~14.18%; 网室栽培模式显著提高了稻田土壤氧化还原电位, 降低稻田产CH4潜力、CH4氧化能力和土壤反硝化酶活性, 减少了稻田CH4和N2O排放量, 全球增温潜势降低6.35%~13.14%。本试验条件下, 稻田土壤的CH4氧化能力是产CH4潜力的2.21~3.81倍; 相同环境条件下, 稻鸭共作和麦秸还田均能增加水稻实际产量, 网室栽培的所有处理较相应的露地栽培减少了水稻实际产量1.19%~5.48%。本试验表明, 稻鸭共作和网室栽培可减缓全球增温潜势, 稻鸭共作和麦秸还田能够增加水稻实际产量。 相似文献
18.
The effect of controlled drainage on methane (CH4) and nitrous oxide (N2O) emissions from a paddy field under controlled irrigation (CI) was investigated by controlling the sub-surface drainage percolation rate with a lysimeter. CI technology is one of the major water-saving irrigation methods for rice growing in China. Water percolation rates were adjusted to three values (2, 5, and 8 mm d?1) in the study. On the one hand, the CH4 emission flux and total CH4 emission from paddy fields under CI decreased with the increase of percolation rates. Total CH4 emissions during the growth stage of rice were 1.83, 1.16, and 1.05 g m?2 in the 2, 5, and 8 mm d?1 plots, respectively. On the other hand, the N2O emission flux and total N2O emissions from paddy fields under CI increased with the increase of percolation rates. Total N2O emissions during the growth stage of rice were 0.304, 0.367, and 0.480 g m?2 in the 2, 5, and 8 mm d?1 plots, respectively. The seasonal carbon dioxide (CO2) equivalent of CH4 and N2O emissions from paddy fields under CI was lowest in the 2 mm d?1 plot (1364 kg CO2 ha?1). This value was 1.4% and 19.4% lower compared with that in the 5 and 8 mm d?1 plots, respectively. The joint application of CI and controlled drainage may be an effective mitigation strategy for reducing the carbon dioxide equivalents of CH4 and N2O emissions from paddy fields. 相似文献
19.
20.
Biochar application can reduce global warming via carbon (C) sequestration in soils. However, there are few studies investigating its effects on greenhouse gases in rice (Oryza sativa L.) paddy fields throughout the year. In this study, a year-round field experiment was performed in rice paddy fields to investigate the effects of biochar application on methane (CH4) and nitrous oxide (N2O) emissions and C budget. The study was conducted on three rice paddy fields in Ehime prefecture, Japan, for 2 years. Control (Co) and biochar (B) treatments, in which 2-cm size bamboo biochar (2 Mg ha?1) was applied, were set up in the first year. CH4 and N2O emissions and heterotrophic respiration (Rh) were measured using a closed-chamber method. In the fallow season, the mean N2O emission during the experimental period was significantly lower in B (67 g N ha?1) than Co (147 g N ha?1). However, the mean CH4 emission was slightly higher in B (2.3 kg C ha?1) than Co (1.2 kg C ha?1) in fallow season. The water-filled pore space increased more during the fallow season in B than Co. In B, soil was reduced more than in Co due to increasing soil moisture, which decreased N2O and increased CH4 emissions in the fallow season. In the rice-growing season, the mean N2O emission tended to be lower in B (?104 g N ha?1) than Co (?13 g N ha?1), while mean CH4 emission was similar between B (183 kg C ha?1) and Co (173 kg C ha?1). Due to the C release from applied biochar and soil organic C in the first year, Rh in B was higher than that in Co. The net greenhouse gas emission for 2 years considering biochar C, plant residue C, CH4 and N2O emissions, and Rh was lower in B (5.53 Mg CO2eq ha?1) than Co (11.1 Mg CO2eq ha?1). Biochar application worked for C accumulation, increasing plant residue C input, and mitigating N2O emission by improving soil environmental conditions. This suggests that bamboo biochar application in paddy fields could aid in mitigating global warming. 相似文献