秸秆生物质炭对稻田土壤剖面N2O和N2浓度的影响*     

马芸芸  周伟  何莉莉  赵旭  王林权 《土壤学报》2021,58(6)

氧化亚氮（N2O）和氮气（N2）是淹水稻田土壤剖面反硝化过程的重要气态产物,可通过土水界面向大气排放,也可随水向下淋溶。秸秆生物质炭施入稻田后会改变土壤理化及微生物学性质,影响反硝化过程及N2O和N2产排。本研究依托2010年夏建立的连续秸秆生物质炭还田的稻麦轮作农田试验,通过埋设淋溶管收集土壤剖面溶液,采用气相色谱和膜进样质谱分别定量溶液中N2O和exN2（反硝化产生N2量）,观测了2018和2019年水稻季不同秸秆生物质炭施用量（CK：每季0 t·hm-2;1BC：每季2.25 t·hm-2;5BC：每季11.3 t·hm-2;10BC：每季22.5 t·hm-2）下0~1 m土壤剖面溶液中N2O和exN2浓度的时空变化,评估了长期施用秸秆生物质炭对稻田土壤剖面反硝化作用及其主要气态氮产物exN2随水流失的影响。结果表明,两个稻季CK处理N2O浓度以60 cm处较高,exN2浓度则随土壤深度增加呈降低趋势。秸秆生物质炭处理能降低剖面N2O和exN2浓度,以10BC处理最为明显。其中,N2O浓度降低以60 cm处较大,exN2浓度降低随土壤深度增加而加大。施用秸秆生物质炭对土壤剖面溶液无机氮（NO3-+NH4+）含量无明显影响,但5BC和10BC处理增加了可溶性有机碳（DOC）和溶解氧（DO）浓度以及氧化还原电位（Eh）。CK处理下土壤剖面溶液N2O和exN2浓度变化与DOC、硝态氮（NO3-）及DO有关;秸秆生物质炭处理下则主要受DO和Eh控制。exN2淋溶量（按1 m深度计算）CK处理下为2.3 ~5.5 kg·hm-2,相当于无机氮和有机氮（DON）淋溶量的32%~34%,5BC和10BC处理则降低为1.7 ~3.7 kg·hm-2和1.1~1.9 kg·hm-2,上述结果表明,反硝化产生N2随水淋溶量不容忽视,秸秆生物质炭还田可改善淹水稻田土壤剖面的通气状况,增加DO,提高Eh,进而有效减少深层反硝化及其主要气态产物exN2随水流失的风险。  相似文献   

短期培养下抑制剂烯丙基硫脲对土壤硝化作用及微生物的影响     

沈晓忆  夏围围  次仁拉姆  李乙坤 《土壤学报》2021,58(6):1552-1563

硝化抑制剂烯丙基硫脲（ATU）对土壤硝化作用及温室效应的影响及机理尚不清楚。本研究采集典型旱地土壤,进行21天室内微宇宙培养,探究了氮肥与不同剂量ATU（分别为氮素用量的1%, 5%, 10%, 15%和20%）配施对土壤硝化作用及N2O和CO2排放通量的影响,并通过实时荧光定量PCR和高通量测序16S rRNA基因技术监测硝化微生物群落变化,同时与传统硝化抑制剂双氰胺（DCD）进行了保氮减排效果的对比。结果表明,与未施加氮肥的对照相比（CK）,单施氮肥（N）显著提高了土壤硝化强度并促进了N2O排放。DCD能显著抑制硝态氮和N2O的积累,抑制效率分别为68.6%和93.3%。而低浓度ATU对土壤硝化作用无影响,仅在高浓度具有抑制效应,且抑制效率最高仅为14.7%。所有ATU处理N2O排放量均显著降低,降幅为60.3～68.2%,仍远高于DCD处理。处理间N2O和CO2的综合温室效应强弱顺序为N>ATU+N>DCD+N≈CK,且不同ATU施用量处理之间差异不显著。相关分析发现氨氧化细菌（AOB）,而不是氨氧化古菌（AOA）和全程氨氧化细菌（Comammox）,与土壤硝态氮积累和N2O排放显著正相关,与土壤pH显著负相关。高通量测序结果表明Nitrosovibrio tenuis类型AOB对氮肥诱导的硝化过程起主导作用。除此之外,ATU和DCD还能显著提高Cupriavidus,并降低Patulibacter、Aeromicrobium、Actinomycetospora、Defluviicoccus和Acidipila等微生物属在群落中的相对丰度。该研究为深化土壤碳氮循环理论,合理使用硝化抑制剂以及减缓温室气体排放提供科学依据。  相似文献   

基于APSIM模型分析不同降水年型下施氮深度对旱地小麦的产量效应     

尹嘉德  侯慧芝  张绪成  马明生  雷康宁  郭宏娟 《水土保持学报》2022,36(1):247-254

氮肥深施有助于提高旱地作物产量,但施氮深度对黄土高原丘陵沟壑区旱地小麦产量在不同降水年型的影响尚不清楚.利用1990-2020年气象观测数据,基于APSIM模型和数学统计方法探讨施氮深度对不同降水年型小麦产量的影响.结果 表明:模型模拟的小麦产量和生物量模拟值与观测值相关性决定系数(R2)＞0.9、模型有效性指数(ME...  相似文献   

氮锌配施对不同玉米品种灌浆期生理特性和籽粒氮锌含量的影响     

张盼盼  邵运辉  刘京宝  乔江方  李川  张美微  黄璐 《核农学报》2022,36(5):1042-1051

提高粮食作物中可食部分的锌生物有效性是解决人体缺锌的重要措施。为研究氮锌肥料施用对玉米籽粒锌营养的影响,本研究以郑单958和谷神玉66为试验材料,在大田条件下研究3个氮水平(90、180 和225 kg N·hm^-2)和2个喷锌处理(0和4.5 kg·hm^-2 ZnSO₄·7H₂O)下玉米籽粒产量和氮锌含量以及灌浆期叶片生理特性的变化。结果表明,吐丝后,与施氮量90 kg·hm^-2处理相比,施氮量180和225 kg·hm^-2处理提高了吐丝后穗位叶SPAD值及硝酸还原酶(NR)、谷氨酰胺合成酶(GS)、碳酸酐酶(CA)、超氧化物歧化酶(SOD)活性和灌浆后期PSⅡ综合性能指数(PI),降低了丙二醛(MDA)含量。施锌能提高吐丝后穗位叶CA、SOD、过氧化物酶(POD)、过氧化氢酶(CAT)活性和灌浆后期SPAD值和PI,降低MDA含量。2个品种相比,谷神玉66灌浆后期穗位叶SPAD值、叶片初始荧光(F_o)和最大荧光(F_m)较高,而灌浆前期穗位叶PI和吐丝后NR、CA、SOD以及POD活性则以郑单958较高。施氮量为90 kg·hm^-2时,玉米籽粒产量平均为8.55 t·hm^-2,随着施氮量增加,玉米籽粒产量显著提高。籽粒中氮含量以施氮量180 kg·hm^-2时最高,为14.85 g·kg^-1。施氮量90和180 kg·hm^-2时,籽粒锌含量平均为27.2 mg·kg^-1,显著高于施氮量225 kg·hm^-2处理。与不施锌相比,喷锌后玉米籽粒产量未有显著变化,籽粒中氮、锌含量分别增加了11.7%和18.0%。郑单958籽粒产量较谷神玉66提高了3.8%,籽粒氮锌含量则分别减少了11.9%和5.3%。综合来看,施氮量为180 kg N·hm^-2时,与喷施ZnSO₄·7H₂O 4.5 kg·hm^-2 配合施用能够增强玉米灌浆期叶片SPAD和荧光特性,提高氮锌代谢关键酶活性,增强氧自由基清除系统酶活性,减弱膜脂过氧化作用的伤害,促进籽粒中氮、锌的吸收和累积。本研究结果可为玉米生产中优化锌生物强化措施提供理论依据。  相似文献   

秸秆还田种类对稻田N₂O排放及硝化反硝化微生物的影响   总被引：1，自引：0，他引：1  

谢婉玉  王永明  纪红梅  黄茜  徐永记  纪洋  冯彦房 《土壤》2022,54(4):769-778

以太湖流域典型单季稻田的原状土柱为研究对象,通过设置温室土柱试验,同步监测3种秸秆(水稻秸秆RS、小麦秸秆WS、玉米秸秆MS)施用下水稻各生长期N₂O排放、水稻产量和土壤理化因子,同时定量化分析多个N₂O排放相关菌群及功能基因的丰度,以阐明N₂O排放对不同种类秸秆施用引发的微生物响应机制,筛选控制单季稻田N₂O减排增效最佳的秸秆种类。结果表明：与对照相比,RS、WS和MS处理下水稻生长期N₂O排放量分别增加162.32%、107.11%和9.48%,其中RS处理显著高于MS处理。水稻生育期内,土壤氨氧化菌(AOA、AOB)和反硝化菌群落(nir S、nos Z)丰度均呈现先上升后下降的变化趋势。与对照相比,拔节期RS处理显著增加AOA、AOB、nirS和nosZ拷贝数,MS和WS处理对上述功能基因丰度均无显著影响。各生育期土壤NH₄⁺-N含量整体高于NO₃^–-N含量,二者均在水稻分蘖期达到峰...  相似文献   

开垦年限对黑土氮初级转化速率和净转化速率的影响   总被引：2，自引：0，他引：2  

李平  郎漫 《土壤学报》2020,57(1):165-173

以东北黑土区开垦2 a和开垦30 a的典型旱作土壤为研究对象,采用15N同位素成对标记技术开展室内培养试验,利用数值计算模型(FLUAZ)计算不同开垦年限土壤的氮初级转化速率,以比较不同开垦年限黑土氮初级转化速率和净转化速率的差异,明确开垦年限对黑土氮转化过程的影响。结果表明,与开垦2a土壤相比,开垦30a土壤的有机碳和水溶性有机碳含量显著降低,导致土壤氮初级矿化速率和初级固定速率也显著降低。但开垦30a土壤的初级硝化速率、净硝化速率和净氮矿化速率却显著高于开垦2a土壤。两个开垦年限土壤的初级硝化速率分别为净硝化速率的1.15倍和1.02倍,说明土壤微生物对硝态氮的固定很少。开垦30a土壤的m/i值(氮初级矿化速率与初级固定速率之比)和n/ia值(初级硝化速率与初级铵态氮固定速率之比)均显著大于1,而开垦2 a土壤的m/i值和n/ia值均接近1。表明开垦2 a土壤的氮矿化与固定过程紧密偶联,氮素损失的风险较小,而开垦30 a土壤中氮矿化量超过了固定量,这为硝化作用的进行提供了底物,增加了硝酸盐反硝化和淋溶风险。  相似文献   

Is N‐feedback involved in the regulation of nitrogenase activity in Medicago truncatula?     

Saad Sulieman  Joachim Schulze  Karl H. Mühling  Lam-Son Phan Tran 《植物养料与土壤学杂志》2020,183(1):42-45

To determine whether senescing leaves provoke an active nitrogen (N) remobilization that results in the reduction of nitrogenase activity, 60% of Medicago truncatula lower leaves were either darkened or individually excised for two weeks. Although a considerable amount of N was remobilized, N₂ fixation activity was found to be increased to maintain the N source/sink balance, indicating an absence of the negative N‐feedback regulation of nitrogenase activity in the senescing M. truncatula.  相似文献   

Mineralization of Organic Nitrogen in Soils with Contrasting Fertility Was Regulated Differently by Addition of Biochar and Animal Manures     

Jirong Zhu  Hongmei Yu  Minghua Xiong  Pengfei Zhu  Yuan Liu 《Communications in Soil Science and Plant Analysis》2020,51(9):1227-1237

ABSTRACT

How to restore the soil fertility and productivity in a damaged and then reclaimed area with extremely low fertility is a big concern worldwide. To explore the method of soil restoration in the coal mining subsidence area, the effects of biochar application coupled with organic fertilizer (animal manures) on the process of organic nitrogen (N) mineralization were studied in a 149 days leaching experiment. Biochar were applied (wt/wt) at the rates of 0%, 1%, and 3%. Two organic fertilizers with different C/N ratio (chicken and sheep manures) were applied at the rate of 200 mg N·kg^?1 soil. A vegetable soil with high-fertility was used as the comparison. The results showed that when treated with chicken manure, the reclaimed soil had 11.13% lower mineralization potential and 20.00% lower inorganic nitrogen production from mineralization than the vegetable soil. Compared with the non-biochar treatment, biochar at both application rates decreased N leaching in chicken manure-treated reclaimed soil, i.e., by 21.49% (1% biochar) and 28.31% (3% biochar), respectively, whereas only high rate of biochar application decreased N leaching in chicken manure-treated vegetable soil by 8.10%. However, N leaching in sheep manure-treated reclaimed soil was unaffected by the biochar application. Thus, the effect of the biochar on the organic nitrogen mineralization was affected by both soil and organic fertilizer type.  相似文献   

Carbon and nitrogen stocks and their mineralization potentials are higher under organic than conventional farming practices in Japanese Andosols     

Valensi Kautsar  Keitaro Tawaraya  Susumu Yamada  Kazunobu Toriyama  Kazuhiko Kobayashi 《Soil Science and Plant Nutrition》2020,66(1):144-151

ABSTRACT

This study aimed at understanding whether and how long-term organic rice farming affects soil carbon (C) and nitrogen (N) stocks and their mineralization potentials in submerged rice paddies in Tochigi, Japan. An incubation experiment was carried out to assess the impacts of internal nutrient cycling after organic farming (OF) for 4–5 years (4OF), 8–9 years (8OF), and 12 years (12OF), compared with a conventional rice field (CF). Soil samples were collected at 0–15 cm and 15–20 cm in flooded rice fields after harvest in October 2013. pH and bulk density at 0–15 cm were significantly lower in 12OF fields than in CF fields (by 0.22 unit pH and 17.5%, respectively). Compared with CF, 12OF fields showed significant differences in soil organic carbon (SOC) and total nitrogen (TN), but 4OF and 8OF fields did not. In 8OF fields, the C decomposition (Co) and N mineralization (No) potentials were significantly higher (by 34.0% and 35.6%, respectively, at 0–15 cm, and by 67.1% and 24.5% at 15–20 cm) than in CF fields. Similarly, in 8OF fields at 0–15 cm, the Co:SOC and No:TN ratios were 19.8% and 23.2% higher, respectively, than in CF fields. Co, No, Co:SOC, and No:TN in 12OF fields were higher than those in CF fields, demonstrating the effects of prolonged organic rice farming. Additionally, in 12OF fields, C and N stocks were significantly higher (by 15.5% and 17.2%, respectively, at 0–15 cm, and by 4.8% and 12.1% at 15–20 cm) than in CF fields. Our findings suggest that long-term organic rice farming increases soil C and N stocks as well as C and N mineralization in Japanese Andosols.  相似文献   

Stable carbon isotope ratios of water-extractable organic carbon affected by application of rice straw and rice straw compost during a long-term rice experiment in Yamagata,Japan     

Toan Nguyen-Sy  Samuel Munyaka Kimani  Hiroyuki Shiono  Reo Sugawara  Keitaro Tawaraya 《Soil Science and Plant Nutrition》2020,66(1):125-132

ABSTRACT

Hot-water- and water-extractable organic matter were obtained from soil samples collected from a rice paddy 31 years after the start of a long-term rice experiment in Yamagata, Japan. Specifically, hot-water-extractable organic carbon and nitrogen (HWEOC and HWEON) were obtained by extraction at 80°C for 16 h, and water-extractable organic carbon and nitrogen (WEOC and WEON) were obtained by extraction at room temperature. The soil samples were collected from surface (0–15 cm) and subsurface (15–25 cm) layers of five plots that had been treated with inorganic fertilizers alone or with inorganic fertilizers plus organic matter, as follows: PK, NPK, NPK plus rice straw (RS), NPK plus rice straw compost (CM1), and NPK plus a high dose of rice straw compost (CM3). The soil/water ratio was 1:10 for both extraction temperatures. We found that the organic carbon and total nitrogen contents of the bulk soils were highly correlated with the extractable organic carbon and nitrogen contents regardless of extraction temperature, and the extractable organic carbon and nitrogen contents were higher in the plots that were treated with inorganic fertilizers plus organic matter than in the PK and NPK plots. The HWEOC and WEOC δ¹³C values ranged from ?28.2% to ?26.4% and were similar to the values for the applied rice straw and rice straw compost. There were no correlations between the HWEOC or WEOC δ¹³C values and the amounts of HWEOC or WEOC. The δ¹³C values of the bulk soils ranged from ?25.7% to ?23.2% and were lower for the RS and CM plots than for the PK and NPK plots. These results indicate that HWEOC and WEOC originated mainly from rice plants and the applied organic matter rather than from the indigenous soil organic matter. The significant positive correlations between the amounts of HWEOC and HWEON and the amount of available nitrogen (P < 0.001) imply that extractable organic matter can be used as an index for soil fertility in this long-term experiment. We concluded that the applied organic matter decomposed more rapidly than the indigenous soil organic matter and affected WEOC δ¹³C values and amounts.  相似文献