应用紫外/氯组合工艺去除微污染原水中氨氮的特性研究

针对饮用水中氨氮超标对环境造成的污染问题,采用紫外/氯组合工艺对饮用水中氨氮进行降解研究.结果表明,紫外/氯高级氧化工艺可以有效去除水中氨氮.一方面,自由氯和氨氮之间发生取代反应将氨氮转化为氯胺,254 nm紫外光可有效裂解N—Cl键,一氯胺在254 nm处的摩尔吸光系数为354 L·mol~(-1)·cm~(-1),量子产率为0.68 mol·E~(-1);另一方面,自由氯光解产生的自由基可直接氧化氨氮.随着紫外辐照剂量的增加,氨氮和总溶解性氮(TN)的浓度逐渐减少,当紫外辐照剂量达到1000 mJ·cm~(-2)时,氨氮(起始浓度2 mg·L~(-1))和TN的去除率分别为53%和35%,相比单独氯化条件下分别提高了20%和15%.随着Cl_2/N的增加,氨氮和TN的浓度逐渐减小,当Cl_2/N≥1.6时,紫外/氯组合工艺对氨氮的去除率接近100%,当Cl_2/N1.6时,紫外/氯工艺对TN的去除率相比单独氯化工艺提高了30%左右.此外,氨氮去除率随pH升高而增加,而TN去除率随pH升高而降低.本研究结果可为紫外/氯组合工艺在水厂中的实际应用提供有效的理论和技术支持.     

化学沉淀法去除稀土湿法冶炼废水中钙与高浓度氨氮研究

离子型稀土湿法冶炼过程中会产生大量氨氮废水,由于废水中含有大量Ca2+,而Ca2+是影响磷酸铵镁沉淀法脱氮效率的重要因素.向废水中投入Na2CO3固体生成CaCO3沉淀物,去除废水中的Ca2+,再利用磷酸铵镁(MAP)沉淀法去除废水中的氨氮.实验采用响应面实验设计方法中的中心复合设计法,利用响应面分析法对磷酸铵镁沉淀法反应参数进行优化,得到最优反应条件及最优反应条件下沉淀产物.利用扫描电子显微镜(SEM)及X射线衍射(XRD)对最优反应条件下两种沉淀物进行分析.结果表明,当n(Ca2+)∶n(CO23-)=1∶1.05,搅拌速率为1 500 r.min-1,反应时间为30 min时,Ca2+去除率接近100%;对除钙后废水进行磷酸铵镁法脱氮处理的最优反应条件为:pH=9.03,n(Mg)∶n(N)=1.20,n(P)∶n(N)=1.1,反应时间为30 min,搅拌速率为1 000 r.min-1,氨氮去除率达到95.40%,剩余总磷浓度为5.65 mg.L-1;沉淀物分别为纯净的CaCO3及MgNH4PO4.6H2O.     

不同类型LDHs对垂直流人工湿地无烟煤基质的覆膜改性及其脱氮效果研究

选取垂直流人工湿地无烟煤基质,采用不同类型金属化合物(CaCl2、ZnCl2、MgCl2、FeCl3、AlCl3、CoCl3)两两组合方式,在碱性环境下共沉淀生成9种不同类型的层状双金属氢氧化物LDHs并覆膜于基质表面;构建基质试验柱,分别对未改性及9种LDHs覆膜改性无烟煤基质进行模拟垂直流人工湿地脱氮效果研究.结果表明,9种不同组合方式生成的LDHs均能有效地进行无烟煤基质覆膜改性;Mg2+参与合成的改性基质对TN和氨氮均有很好的去除效果,其中MgCo-LDHs改性基质对TN的平均去除率超过80%,对氨氮的平均去除率达到了85%;Mg2+和Fe3+参与合成的改性基质对氨氮的去除效果优良,其中CaFe-LDHs和MgFe-LDHs改性基质的平均去除率达到了85%以上.     

Bi-PbO2电极电化学氧化去除模拟废水中氨氮的研究

本实验采用钛网作为基体,利用电沉积方法制备了纯PbO2电极和Bi-PbO2电极,通过SEM、XRD、XPS对电极的表面形态进行了表征,利用循环伏安法对Bi-PbO2电极电化学特性进行了研究.同时,以氨氮模拟废水作为研究对象,考察了Bi-PbO2电极的电催化活性,探讨了氨氮电化学氧化降解机理.结果表明,Bi-PbO2电极的形态表征、电催化活性明显高于纯PbO2电极,氨氮的去除效率随电流密度的增加而提高,碱性条件下氨氮的去除效果明显好于酸性条件,适量浓度的Cl-的引入在碱性条件下提高了氨氮的去除效果.当氨氮初始浓度为50 mg·L-1、电流密度为40 mA·cm-2、pH=12、Cl-浓度为600 mg·L-1时,电解120 min后,氨氮100%去除.氨氮的降解机理为:体系中无添加氯离子,酸性条件下氨氮主要是通过间接氧化去除,碱性条件下通过直接电氧化和间接氧化共同完成;体系中添加氯离子,氨氮的去除主要是通过溶液中生成的有效氯间接氧化去除.     

海水异养硝化-好氧反硝化芽孢杆菌SLWX2的筛选及脱氮特性

从分离自刺参养殖环境的7株候选菌株中筛选出1株具有较强异养硝化和好氧反硝化能力的菌株SLWX_2,通过形态学特征、生理生化特性和16S rRNA基因测序分析鉴定其为花津滩芽孢杆菌(Bacillus hwajinpoensis).该菌株脱氮特性研究结果表明,SLWX_224 h对氨氮、亚硝酸氮和硝酸氮的去除率分别达到100%、99.5%和85.6%;当3种无机氮源同时存在时,菌株优先利用氨氮,再利用NO_2~--N和NO_3~--N,72 h 3种无机氮的质量浓度均降至0.013 mg·L~(-1)以下,表明该菌株能同时进行异养硝化和好氧反硝化完成脱氮;在氨氮负荷500 mg·L~(-1)、亚硝酸氮负荷100 mg·L·~(-1)和硝酸氮负荷200 mg·L~(-1)范围内,该菌的脱氮能力不受明显抑制,对3种形态的氮均有良好去除效果,96 h最多可去除180 mg NH_4~+-N、30 mg NO_2~--N和120 mg NO_3~--N,并且在硝化过程中没有亚硝酸氮积累.该菌株在海水养殖和高盐高氮工业废水的脱氮处理方面具有更大潜力.     

NanoChem分子筛对高氨氮废水去除效果的研究

采用新型的离子吸附交换材料NanoChem分子筛,研究对高浓度氨氮的模拟废水和实际垃圾渗滤液的去除效果.结果显示,氨氮吸附符合Langmuir吸附等温线,其中单位NanoChem分子筛吸附氨氮饱和浓度以N计算为364 mg.g-1,对高浓度氨氮的吸附能力比天然沸石或者微孔分子筛强3～30倍.在间歇实验中考察了操作参数对氨氮去除的影响,NanoChem分子筛20 h后基本达到离子交换平衡;氨氮去除量随着初始浓度的增加而增加,而去除率则随着初始浓度的增加而减少;同时溶液初始pH值不但影响氨氮去除率还影响离子交换特性;再生前后氨氮去除效果变化不大,重复性强.动态连续流研究发现NanoChem分子筛能用于实际高浓度氨氮废水的去除,去除率可达到100%.     

Research on the degradation mechanism of pyridine in drinking water by dielectric barrier discharge

Pyridine, an important chemical raw material, is widely used in industry, for example in textiles,leather, printing, dyeing, etc. In this research, a dielectric barrier discharge(DBD) system was developed to remove pyridine, as a representative type of nitrogen heterocyclic compound in drinking water. First, the influence of the active species inhibitors tertiary butanol alcohol(TBA),HCO_3~-, and CO_3~(2-)on the degradation rate of pyridine was investigated to verify the existence of active species produced by the strong ionization discharge in the system. The intermediate and final products generated in the degradation process of pyridine were confirmed and analyzed through a series of analytical techniques, including liquid chromatography–mass spectrometry(LC–MS), high performance liquid chromatography(HPLC), ion chromatography(IC), total organic carbon(TOC) analysis, ultraviolet(UV) spectroscopy, etc. The results showed that the degradation of pyridine was mainly due to the strong oxidizing power of ozone and hydroxyl radical produced by the DBD system. Several intermediate products including 3-hydroxyl pyridine, fumaric acid, 2, 3-dihydroxypyridine, and oxalic acid were detected. Nitrogen was removed from the pyridine molecule to form nitrate. Through analysis of the degradation mechanism of pyridine, the oxidation pathway was deduced. The study provided a theoretical and experimental basis for the application of DBD strong ionization discharge in treatment of nitrogen heterocyclic compounds in drinking water.     

底物含氮量对厨余堆肥氮素转化及其损失的影响研究

采用静态好氧工艺研究了含氮量分别为32.4 g·kg-1、45.3 g·kg-1和58.2g·kg-1的厨余垃圾(N0、N1、N2)与木屑混合堆制时,堆肥过程中不同形态氮的转化及其氮损失规律.结果表明,堆肥中堆体全氮含量呈先升后降趋势,部分有机氮转化为铵氮导致堆体pH升高,在通风和高温的联合作用下,NH3挥发出堆体造成一定的氮损失.随着底物含氮量的增加,NH3挥发速率和氮损失率均呈上升趋势.堆肥结束时N0、N1、N2的堆体全氮含量分别下降了16.4%、26.3%和21.7%,NH3累计挥发量分别为7.0 g·kg-1、9.8 g·kg-1和29.4 g·kg-1,堆肥氮损失率分别为35.0%、49.9%和53.0%.NH3挥发主要集中在高温阶段的中后期,是厨余堆肥氮损失的主要原因.     

Comparison between UV and VUV photolysis for the pre- and post-treatment of coking wastewater

In this study, ultraviolet (UV) and vacuum ultraviolet (VUV) photolysis were investigated for the pre-treatment and post-treatment of coking wastewater. First, 6-fold diluted raw coking wastewater was irradiated by UV and VUV. It was found that 15.9%-35.4% total organic carbon (TOC) was removed after 24 hr irradiation. The irradiated effluent could be degraded by the acclimated activated sludge. Even though the VUV photolysis removed more chemical oxygen demand (COD) than UV, the UV-irradiated effluent demonstrated better biodegradability. After 4 hr UV irradiation, the biological oxygen demand BOD₅/COD ratio of irradiated coking wastewater increased from 0.163 to 0.224, and its toxicity decreased to the greatest extent. Second, the biologically treated coking wastewater was irradiated by UV and VUV. Both of them were able to remove 37%-47% TOC within 8 hr irradiation. Compared to UV, VUV photolysis could significantly improve the transparency of the bio-treated effluent. VUV also reduced 7% more ammonia nitrogen (NH₄⁺-N), 17% more nitrite nitrogen (NO₂^--N), and 18% more total nitrogen (TN) than UV, producing 35% less nitrite nitrogen (NO₃^--N) as a result. In conclusion, UV irradiation was better in improving the biodegradability of coking wastewater, while VUV was more effective at photolyzing the residual organic compounds and inorganic N-species in the bio-treated effluent.     

Efficient dechlorination of chlorinated solvent pollutants under UV irradiation by using the synthesized TiO2 nano-sheets in aqueous phase

Titanium dioxide(TiO2), which is the widely used photo-catalyst, has been synthesized by simple hydrothermal solution containing tetrabutyl titanate and hydrofluoric acid. The synthesized product has been applied to photo-degradation in aqueous phase of chlorinated solvents, namely tetrachloroethene(PCE), trichloroethene(TCE) and 1,1,1-trichloroethane(TCA). The photo-degradation results revealed that the degradation of these harmful chemicals was better in UV/synthesized TiO2 system compared to UV/commercial P25 system and UV only system. The photo-catalytic efficiency of the synthesized TiO2 was 1.4, 1.8 and 3.0 folds higher compared to the commercial P25 for TCA, TCE and PCE degradation, respectively. Moreover, using nitrobenzene(NB) as a probe of hydroxyl radical(.OH), the degradation rate was better over UV/synthesized TiO2, suggesting the high concentration of.OH generated in UV/synthesized TiO2system. In addition,.OH concentration was confirmed by the strong peak displayed in EPR analysis over UV/synthesized TiO2system. The characterization result using XRD and TEM showed that the synthesized TiO2 was in anatase form and consisted of well-defined sheet-shaped structures having a rectangular outline with a thickness of 4 nm, side length of 50 nm and width of 33 nm and a surface 90.3 m2/g. XPS analysis revealed that ≡Ti-F bond was formed on the surface of the synthesized TiO2. The above results on both photocatalytic activity and the surface analysis demonstrated the good applicability of the synthesized TiO2 nano-sheets for the remediation of chlorinated solvent contaminated groundwater.     

Comparison between UV and VUV photolysis for the pre- and post-treatment of coking wastewater

In this study, ultraviolet (UV) and vacuum ultraviolet (VUV) photolysis were investigated for the pre-treatment and post-treatment of coking wastewater. First, 6-fold diluted raw coking wastewater was irradiated by UV and VUV. It was found that 15.9%–35.4% total organic carbon (TOC) was removed after 24 hr irradiation. The irradiated effluent could be degraded by the acclimated activated sludge. Even though the VUV photolysis removed more chemical oxygen demand (COD) than UV, the UV-irradiated effluent demonstrated better biodegradability. After 4 hr UV irradiation, the biological oxygen demand BOD₅/COD ratio of irradiated coking wastewater increased from 0.163 to 0.224, and its toxicity decreased to the greatest extent. Second, the biologically treated coking wastewater was irradiated by UV and VUV. Both of them were able to remove 37%–47% TOC within 8 hr irradiation. Compared to UV, VUV photolysis could significantly improve the transparency of the bio-treated effluent. VUV also reduced 7% more ammonia nitrogen (NH₄⁺–N), 17% more nitrite nitrogen (NO₂⁻–N), and 18% more total nitrogen (TN) than UV, producing 35% less nitrite nitrogen (NO₃⁻–N) as a result. In conclusion, UV irradiation was better in improving the biodegradability of coking wastewater, while VUV was more effective at photolyzing the residual organic compounds and inorganic N-species in the bio-treated effluent.     

不同水环境下苦草腐解对水质的影响

为探究沉水植物在不同水环境下的腐解对水质的影响,在实验室条件下分别模拟不同生物量沉水植物苦草在高纯水、上覆水及底泥悬浮液环境下的腐解过程及其对水体水质的影响,并分别讨论了N、P等含量在底泥和上覆水环境下的差异性.结果表明:① 随着时间的推移,苦草腐解均会导致上覆水及底泥悬浮液中pH先降后升,ρ（DO）急剧降低.在上覆水环境中,pH自7.8降至7.2,再增至8.7;与试验初期相比,ρ（DO）在第10天降低了56%.在底泥悬浮液中,pH自7.8降至7.3,再增至8.3;在第10天ρ（DO）降低了近60%.② 在上覆水及底泥悬浮液中,苦草腐解以释放有机氮为主,NH₃-N次之;ρ（TP）在试验前期呈先升后降趋势,但在试验中期底泥悬浮液环境中ρ（TP）则呈动态平衡,约为1 mg/L.③ 不同生物量（0.1、0.2、0.4 g/L）的苦草腐解后水环境中的营养盐含量有所不同,其中ρ（COD_Cr）、ρ（TP）与生物量呈正相关,在试验前期ρ（TN）、ρ（NO₂--N）随着峰值的增大而增大.研究显示,苦草腐解对两种水环境的物化性质有着相似的影响,而对其主要营养盐氮、磷形态的变化有着显著性的差异.      

江汉平原中部浅层地下水中氨氮的有机质来源探究

江汉平原地下水氨氮浓度普遍超标，但是氮污染来源尚不明晰，尤其是对潜在的有机来源氮的认识还很不充分。本研究对江汉平原中部浅层地下水和沉积物中的溶解性有机质（Dissolved organic matter，DOM）荧光组分与氨氮关系进行了调查研究，并对沉积物的氮形态进行分析，探讨了沉积物中有机质向氨氮的潜在转化过程。研究表明研究区内浅层地下水中广泛分布溶解性有机碳与NH₄⁺，并且两者浓度呈现正相关关系（R²=0.42，p<0.01），该区域地下水呈现强还原环境有利于DOC与NH₄⁺的赋存。DOM荧光光谱谱图的平行因子分析（Parallel factor analysis，PARAFAC）结果表明：地下水与沉积物中DOM均含有类氨基酸与类富里酸组分。有机质组分荧光强度与氨氮浓度相关性结果表明：沉积物DOM中类富里酸和类氨基酸组分与氨氮均呈现强正相关性（R²=0.92~0.96，p<0.01）；地下水中DOM类富里酸组分与氨氮呈现较强的正相关性（R²=0.62~0.66，p<0.01），而类氨基酸组分与氨氮的正相关性不明显。地下水中相较沉积物中，DOM的类富里酸和类氨基酸组分与氨氮相关性减弱，这种变化可能指示了类富里酸稳定赋存在含水层，而类氨基酸更容易分解消耗。沉积物中凯氏氮占总氮的87.04%~93.51%，表明沉积物中的氮主要为可以转变为NH₄⁺的有机氮形态，因而满足了地下水中的NH₄⁺由沉积物有机氮转化产生的必备条件。江汉平原沉积物中有机氮的分解是浅层地下水氨氮的重要来源。     

太湖丘陵地区农田氮素迁移的时空分布特征

在太湖丘陵地区选择4种有代表性的土地利用类型进行野外原位试验,研究自然降雨条件下氮素随地表径流迁移的时空分布特征.试验结果表明,随地表径流迁移的农田氮素以氨氮为主,其“次降雨径流平均浓度”中位值占总氮的44.5%,亚硝态氮浓度最小,仅占1.8%.地表径流中的氮素浓度存在显著的季节性差异,其分布主要受降水量、气温等气象条件以及农事活动的影响.总氮、氨氮、硝态氮和亚硝态氮的“多场降雨径流平均浓度”的时间变异性依次减小.菜地径流中总氮、氨氮和硝态氮以及竹林亚硝态氮的SMC值最高,不同土地利用下氮素浓度的空间分布主要与施肥条件以及植被覆盖度有关.各氮素形态SMC值的空间变异性小于其时间变异性.旱地和菜地的氮素迁移通量大于板栗林和竹林,径流量是导致迁移通量存在显著差异的主导因素.     

海洋厌氧氨氧化菌处理含海水污水的基质抑制及其动力学特性

采用ASBR反应器通过改变单一基质浓度分别研究了NH_4~+-N和NO_2~--N对海洋厌氧氨氧化菌脱氮效能的影响及其动力学特性.结果表明,保持进水NO_2~--N为105.6 mg·L~(-1),当进水NH_4~+-N浓度提高至1 200 mg·L~(-1)时,海洋厌氧氨氧化反应器仍保持较好的脱氮能力,未受到明显的抑制作用,NO_2~--N的去除率稳定在80.70%左右;当进水NO_2~--N浓度提高至265.6mg·L~(-1)时,反应器开始受到明显的抑制作用,NH_4~+-N的去除率下降至63.01%左右,随着进水NO_2~--N浓度继续提高至305.6mg·L~(-1)时,NH_4~+-N的去除率进一步下降至43.93%左右.利用Haldane模型和Aiba模型拟合NH_4~+-N和NO_2~--N抑制作用的动力学特性,得到了NRRmax、KS、Ki这3个动力学参数及出水基质浓度与总氮容积负荷(TNRR)之间的关系,根据进一步分析可知,Haldane模型更适合描述NH_4~+-N抑制作用下的动力学特性,Aiba模型更适合描述NO_2~--N抑制作用下的动力学特性,并得到NH_4~+-N和NO_2~--N的出水抑制浓度分别为3 893.625 mg·L~(-1)和287.208 mg·L~(-1),为海洋厌氧氨氧化菌处理含海水污水提供了理论依据.     

不同类型LDHs覆膜改性人工湿地生物陶粒基质脱氮效果研究

在碱性条件下采用水热-共沉淀法,对二价金属化合物CaCl2、MgCl2、ZnCl2与三价金属化合物FeCl3、AlCl3、CoCl3按两两组合方式生成9种不同类型的LDHs,并分别对人工湿地常用的生物陶粒基质进行覆膜改性;构建模拟基质试验柱,对改性前后的生物陶粒基质进行城市污水的脱氮净化效果研究.结果表明,相对于原始生物陶粒基质,大多数改性基质对CODCr、总氮和氨氮的去除效果均有不同程度的提高,经所有基质处理后的出水中硝态氮浓度均呈上升趋势;Zn2+参与合成的LDHs改性基质对总氮、氨氮有较好的处理效果,其中ZnFe-LDHs和ZnCoLDHs对TN的去除率接近60%,对氨氮的去除率超过92%,这两种改性基质对污水中的氨氮转化为硝态氮具有促进作用.     

Synergistic photocatalytic degradation of pyridine using precious metal supported TiO2 with KBrO3

A series of precious metals catalysts （M/TiO/, M = Ru, Rh, Pd, Ag, Ir, Pt or Au） were prepared by a light deposition method and the synergistic photocatalytic degradations of pyridine （20 mg/L） under UV irradiation （365 nm） using M/TiO2 with electron capture agent KBrO3 have been investigated. The results show that KBrO3 has a greatly synergistic role on M/TiO2 and the photocatalytic activity of M/TiO2 is closely related to its work function. Ag could greatly enhance the activity of TiO2 due to the binding characteristics of pyridine on Ag. Under the conditions of 0.5 wt.% Ag loading, Ag/TiO2 concentration of 0.1 g/L, KlrO3 concentration of 10 mmol/L and reaction liquid pH value at 9, the pyridine can be degraded by 64% within 3 hr, doubled than TiO2 photocatalytic system. The degradation kinetics of pyridine follows first-order kinetics and k = 5.53 × 10-3 min^-1.     

3种人工湿地基质材料对氨氮的吸附特性

对陶粒、石英砂和砾石这3种人工湿地基质材料进行了氨氮（NH₄⁺-N）吸附特性研究.通过扫描电镜和BET比表面积分析仪对材料进行表征分析,发现陶粒表面相比石英砂和砾石更为粗糙,内部孔隙也较发达,陶粒（18.97 m²·g^-1）比表面积高于石英砂和砾石.在纯氨氮溶液和模拟污水厂出水一级B标准的混合溶液中,3种基质对NH₄⁺-N的吸附能力均表现为：陶粒>砾石>石英砂.陶粒对NH₄⁺-N的饱和吸附容量在混合溶液中最大（63.55 mg·g^-1）.陶粒对NH₄⁺-N的吸附过程符合伪二级动力学模型（在纯氨氮溶液中R²为0.99、在混合溶液中R²为0.98）.在纯氨氮溶液中运用Freundlich和Langmuir模型对等温吸附试验结果进行拟合,发现Freundlich模型（R²=0.93）描述陶粒的吸附特性比Langmuir模型更为精确（R²为0.93）,表明陶粒对NH₄⁺-N的吸附为多层吸附.综上所述,陶粒的吸附容量较强,在混合溶液中吸附容量较纯氨氮溶液增大了31%,适用于作为人工湿地基质填料.     

高氨氮废水短程硝化过程中N2O释放试验研究

试验采用序批式反应器(SBR)处理高氨氮废水,逐步提高废水氨氮(NH+4-N)浓度到800 mg·L-1,通过控制曝气量实现了短程硝化.SBR周期试验表明,在低溶解氧和高游离氨等共同作用下,氨氧化菌(AOB)活性较低,导致AOB以亚硝酸盐氮(NO_2~--N)作为电子受体进行好氧反硝化,氧化亚氮(N_2O)释放因子为9.8%.静态试验控制初始NH_4~+-N为100 mg·L-1且改变曝气量(0.22~0.88 L·min~(-1))条件下,溶解氧浓度的增加能够提高硝化菌活性,N2O释放因子为0.51%~0.85%.当初始NH_4~+-N浓度为100 mg·L~(-1)且曝气量控制在0.66 L·min-1时,初始NO-2-N浓度为0~100 mg·L~(-1)对硝化菌活性影响较小,N2O释放因子为0.50%~0.71%.当溶解氧和游离氨浓度控制在适宜范围内,可维持AOB较高活性,抑制AOB发生好氧反硝化作用,降低N2O释放率.     

外加可溶性碳、氮对不同热量带土壤氨挥发的影响

在室内条件下采用静态吸收法,研究了外加可溶性碳、氮对不同热量带经长期施肥的3种农田土壤:黑土、潮褐土和红壤氨挥发的影响.结果表明,施用氮肥显著促进了土壤氨挥发,在单施氮肥和可溶性碳配施氮条件下,不同热量带土壤氨挥发量从高到低分别为潮褐土(14.3、 7.37 mg·kg~(-1)),黑土(1.52、 1.11 mg·kg~(-1)),红壤(0.998、 0.402 mg·kg~(-1)).添加可溶性碳显著减少土壤因施氮肥产生的氨挥发量,其中黑土减少27.0%,潮褐土减少48.5%,红壤减少60.0%.在黑土、潮褐土长期不同施肥土壤中,单施氮肥后氨挥发量均表现为无肥土壤 > 化肥土壤 > 化肥+有机肥土壤,与可溶性碳配施氮后氨挥发量变化规律相反;在红壤长期不同施肥土壤中,单施氮肥和可溶性碳配施氮后氨挥发量均表现为无肥土壤 > 化肥土壤 > 化肥+有机肥土壤.研究结果还表明,外加可溶性碳、氮后,潮褐土铵态氮含量的减少幅度和硝态氮含量的增加幅度均显著高于黑土和红壤,说明潮褐土中氮素损失潜能大.