稻田CH4和N2O的排放及养萍和施肥的影响

用箱法对我国东北稻田ＣＨ４和Ｎ２Ｏ排放进行观测研究表明,东北稻田的ＣＨ４排放通量比南方稻田小,平均日排放通量和生长季节排放总量分别为０．０７和７．４ｇ·ｍ－２．稻田淹水期几乎没有Ｎ２Ｏ的净排放,但在非淹水期内却有大量Ｎ２Ｏ排放（平均通量５９μｇＮ２Ｏ·ｍ－２·ｈ－１）．稻田养萍和施肥明显促进ＣＨ４和Ｎ２Ｏ排放．稻田ＣＨ４和Ｎ２Ｏ排放之间存在消长关系．制定稻田温室气体减排技术措施时应充分注意这一关系．     

长白山北坡不同土壤N2O和CH4排放的初步研究

用箱法技术原位测定了长白山北坡不同土壤（苔原土、生草森林土、棕色针叶林土和暗棕色森林土）６—８月间的Ｎ２Ｏ和ＣＨ４排放．结果表明,这些土壤既是Ｎ２Ｏ的源,又同时是ＣＨ４的汇．Ｎ２Ｏ通量变化于６．１７—１２．３３μｇ·ｍ－２·ｈ－３之间（平均９．３７μｇ·ｍ－２·ｈ－１）,ＣＨ４通量为－８５．６３—－７．５８μｇ·ｍ－２·ｈ－１（平均－４１．４５μｇ·ｍ－３·ｈ－１）,并观察到在Ｎ２Ｏ排放和ＣＨ４吸收之间有着相互消长关系．实验室培养实验表明,最大反硝化作用活性存在于土壤上层（０—６ｃｍ）;不同土壤的反硝化作用活性明显不同．山地暗棕色森林土的ＣＨ４吸收作用也主要发生在土壤的上层（０—１２ｃｍ）．     

东北典型旱作农田N_2O和CH_4排放通量研究

应用封闭式箱法技术测定了玉米、大豆田中Ｎ２Ｏ和ＣＨ４全年的通量变化．指出Ｎ２Ｏ排放有明显的季节变化和明显的日变化．大量的Ｎ２Ｏ排放发生在作物生长季节中．在冰雪溶化期和收割作物后也有一定量的Ｎ２Ｏ从土壤中排放．此外,实验结果也指出,玉米和大豆田作为大气ＣＨ４源或汇的作用不明显．     

玉米植株对大田温室气体N2O排放的影响

利用封闭式箱法对玉米田Ｎ２Ｏ排放通量的观测表明,大田种植玉米后,对Ｎ２Ｏ排放产生了很大影响,玉米土壤系统的Ｎ２Ｏ排放通量大于不种玉米的土壤．此外,植物根系能明显促进土壤中Ｎ２Ｏ的排放,特别是在玉米生长后期尤为明显．从播种开始到年底,施尿素导致Ｎ２Ｏ排放为３．３ｋｇ·ｈｍ－２,玉米植株为０．６９ｋｇ·ｈｍ－２,占总排放量的１７．３％．     

铝对玉米生长和硝酸还原酶活性的影响

测定了生长在Ａｌ２（ＳＯ４）３１００μｍｏｌ／Ｌ氮素营养液中的两个玉米品种（ＳＣ７０４和ＶＡ３５的根系和叶片）的ＮＡＤＨ－硝酸还原酶（ＥＣ１．６．６．１）和ＮＡＤ（Ｐ）Ｈ－硝酸还原酶（ＥＣ１．６．６．２）活性。     

雄激素对人前列腺细胞中鸟氨酸脱羧酶基因表达的调节作用

 为探讨雄激素对人前列腺中鸟氨酸脱羧酶（ Ｏ Ｄ Ｃ）基因表达的调节作用,以研究雄激素诱导前列腺良性增生的分子机理,分离培养了人胎儿前列腺间质细胞,以 Ｍ Ｔ Ｔ 法测定不同浓度 Ｄ Ｈ Ｔ对细胞的促增殖作用;以最适浓度的 Ｄ Ｈ Ｔ（１ ０００ μｇ／ Ｌ）刺激该细胞,分别于 ０,３,６,１２,２４,３０ ｈ 提取总 Ｒ Ｎ Ａ,用斑点杂交及 Ｎｏｒｔｈｅｒｎ ｂｌｏｔ 法分析测定各组细胞中 Ｏ Ｄ Ｃ ｍ Ｒ Ｎ Ａ 的丰度,并对杂交膜进行薄层扫描定量．结果显示：（１） Ｄ Ｈ Ｔ 对前列腺间质细胞的增殖呈双相调节作用,即在低浓度时随着 Ｄ Ｈ Ｔ 浓度的增加,对该细胞的促增殖作用增强,１ ０００ μｇ／ Ｌ时刺激活性最强,高浓度 Ｄ Ｈ Ｔ 对该细胞的刺激作用降低．（２）斑点杂交显示,在 １ ０００ μｇ／ Ｌ Ｄ Ｈ Ｔ 刺激细胞后 ６ ｈ 时, Ｏ Ｄ Ｃ ｍ Ｒ Ｎ Ａ开始明显升高,２４ ｈ 达高峰（约为 ０ ｈ 的 ４８ 倍）,至 ３０ ｈ 有所降低．（３） Ｎｏｒｔｈｅｒｎ ｂｌｏｔ 结果显示,人胎儿前列腺间质细胞中有两种 Ｏ Ｄ Ｃ ｍ Ｒ Ｎ Ａ,分别为 ２０ ｋｂ 和 ２６ ｋｂ,经扫描定量结果显示：１ ０００μｇ／ Ｌ Ｄ Ｈ Ｔ 对两种 Ｏ Ｄ Ｃ ｍ Ｒ Ｎ Ａ     

Ap—2号溶磷黑曲霉深层发酵工艺的研究

为了实现Ａｐ－２号磷菌肥的工业化生产,对Ａｐ－２号溶磷黑曲霉进行了深层发酵工艺的研究。确定了最佳发酵条件：Ｃ／Ｎ１０：１;菊花糖４％,黄豆饼粉２％,麸皮１％,酵母粉０．５％,ＭｇＳＯ４．７Ｈ２Ｏ０．０５％,Ｋ２ＨＰ０４,０．１％,温度３０℃,ｐＨ６,摇床转数１８０ｒ／ｍｉｎ,发酵９６小时,ｐＨ降至３．１,残糖降至１％以下,柠檬酸、草酸总量达３％以上,菌丝浓度达２．５ｇ／ｍｌ。采用ＥＳ－１５型自控发     

6BA诱导的带正电荷的葡萄叶过氧化物酶

河岸葡萄叶的带正电荷过氧化物酶（ｃａｔｉｏｎｉｃ ｐｅｒｏｘｉｄａｓｅ, ＣＰＯＤ） 可受６ＢＡ 诱导,但盐、Ｈ２Ｏ２ 或Ｆｅ２＋＋ Ｈ２Ｏ２ 均使叶片ＣＰＯＤ 活性明显下降,而高浓度的无机盐明显刺激纯ＣＰＯＤ 活性增加。在以愈创木酚为底物时ＣＰＯＤ 最适ｐＨ 为４ ．６０ ～５ ．７５ ,对Ｈ２Ｏ２ 的表观Ｖｍａｘ 和Ｋｍ 值分别为１１０ Ｕ／ｍｇ 蛋白和１ ．１５ｍ ｍｏｌ／Ｌ。     

细锥香茶菜甲素的结构订正和丙素的化学结构

前已报道［１］从唇形科香茶菜属植物细锥香茶菜（Ｒａｂｄｏｓｉａｃｏｅｔｓａ（Ｂｕｃｈ．Ｈａｎ．ｅｘＤ．Ｄｏｎ）Ｈａｒａ）中分离到３个结晶单体,并测定了其中两个单体——细锥香茶菜甲素（１）和乙素的结构。本文通过１Ｈ－１ＨＣＯＳＹ、１３Ｃ－１ＨＣＯＳＹ和ＮＯＥＳＹ,修订细锥香茶菜甲素（１）的结构为（２）,并经理化常数测定和光谱分析,确定了另一结晶单体——微量新成分细锥香茶菜丙素（３）的结构。（２）Ｒ１＝Ｒ２＝Ｒ４＝Ｈ,Ｒ３＝ＯＡｃ,Ｒ５＝ＯＣＨ３（３）Ｒ１＝Ｒ３＝Ｒ４＝Ｈ,Ｒ２＝ＯＡｃ,Ｒ５＝ＯＣＨ…     

6—BA诱导的带正电荷的葡萄叶过氧化物酶

河岸葡萄叶的带正电荷过氧化物酶可受６－ＢＡ诱导,但盐,Ｈ２Ｏ２或Ｆｅ＾２＋＋Ｈ２Ｏ２均使叶片ＣＯＰＤ活性明显下降,而高浓度的无机盐明显刺激纯ＣＯＰＤ活性增加。在以愈创木酚为底物时ＣＰＯＤ最适ｐＨ为４．６０－５．７５,对Ｈ２Ｏ２的表面Ｖｍａｘ和Ｋｍ值分别为１１０Ｕ／ｍｇ蛋白和１．１５ｍｍｏｌ／Ｌ。     

黑土稻田CH4与N2O排放及减排措施研究

通过对黑土稻田CH₄和N₂O排放的观测,发现水稻生长季CH₄和N₂O排放量低于全国其它地区稻田CH₄和N₂O排放之间存在互为消长关系(r=-0．513,P<0．05),但在同样施肥水平条件下,间歇灌溉与长期淹灌相比,CH₄排放明显减少而N₂O略有增加,其相对综合温室效应被大大减少且水稻产量未受影响。为此,间歇灌溉可作为减少稻田温室气体排放的水分管理措施。另外,通过对CH₄和N₂O排放的相关微生物过程探讨,揭示产甲烷菌数与CH4排放问呈显著性正相关(R²=0．82,P<0．05),硝化菌数和反硝化菌数与N2O排放有重要关系。     

Fate of urea-15N in a soil-wheat system as influenced by urease inhibitor hydroquinone and nitrification inhibitor dicyandiamide

By applying labeled urea into a loamy meadow brown soil, a pot experiment with spring wheat as test crop was carried out. The results showed that at the end of this experiment, the plant recovery, the soil recovery and the total loss of applied urea ¹⁵N was 17.7–23.7%, 43.7–56.3% and 20.0–36.8%, respectively. ¹⁵N recovery by wheat grain in any treatment varied within a range of 9.0–14.7% of the applied ¹⁵N. A combined application of hydroquinone (HQ) and dicyandiamide (DCD) gave the lowest loss and the highest recoveries in both the plant and soil, while applying HQ or DCD alone had less effect on them. During the whole period of wheat growth, HQ+DCD induced an increasing ¹⁵N uptake by plant, and even promoted the translocation of absorbed ¹⁵N from stem to grain. In the presence of inhibitors, organic plus chemically fixed ¹⁵N occupied a large portion of soil ¹⁵N recovery at maturity stage of wheat growth (34.3–50.6%, in contrast to 9.9% in the absence of inhibitors), and DCD and DCD+HQ could remarkably reduce the remaining soil (NO₃ ^-+NO₂ ^-)-¹⁵N. In this pot experiment, the leaching loss of applied ¹⁵N was excluded, and hence, the gaseous loss was considered as the main part of the ¹⁵N loss. Regarding N loss, N₂O flux only occupied a very small part, and its main part was other gaseous N losses. DCD and DCD+HQ retarded N₂O flux from the soil-wheat system after treatment with urea and reduced the total N₂O flux during the whole period of wheat growth. Treatment with both inhibitors had much lower gaseous N losses than that with HQ or DCD alone. Hence, a proper combination application of HQ and DCD is an efficient way to improve urea-N efficiency and crop quality, while decreasing its loss to the environment. This revised version was published online in June 2006 with corrections to the Cover Date.     

开放式空气CO2增高对稻田CH4和N2O排放的影响

在FACE(free aircarbondioxideenrichment)平台上 ,采用静态暗箱 气相色谱法观测研究了大气CO2 浓度增加对稻田CH4和N2 O排放的影响 .结果表明 ,在 15 0和 2 5 0kgN·hm-2 两种氮肥水平下大气CO2 浓度增加 2 0 0 μmol·mol-1均明显促进水稻生长 ,水稻生物量积累 .大气CO2 浓度增加对 15 0和 2 5 0kgN·hm-2 两种氮肥水平下稻田CH4排放均无显著影响 ,并简要分析了与现有文献报道结果不一致的原因 .大气CO2 浓度增加也未导致 15 0和 2 5 0kgN·hm-2 两种氮肥水平下稻田N2 O排放的明显变化 ,与大多数研究结果一致 .     

长效氮肥施用对黑土水旱田CH4和N2O排放的影响

通过在黑土玉米地与水稻田施用长效氮肥后发现 ,长效碳酸氢铵 (长碳 )与长效尿素(长尿 )能显著减少黑土玉米地N2 O的排放。与施用普通尿素相比 ,其排放量分别减少了5 9 2 %和 73 3%。长碳和长尿还能促进黑土玉米地对CH4的吸收作用。黑土水稻田施用长尿后 ,N2 O的排放减少了 6 1%。而CH4的排放却略有增加     

与氮转化有关的土壤酶活性对抑制剂施用的响应

利用室内模拟培养试验,研究好气条件下施用尿素后土壤脲酶、脲酸还原酶、亚硝酸还原酶和羟胺还原酶活性对脲酶抑制剂氢醌（HQ）与硝化抑制剂包被碳化钙（ECC）和双氰胺（DCD）组合（HQ ECC、HQ DCD）的响应、结果表明,HQ DCD组合与其它抑制剂处理相比能更有效地降低土壤脲酶活性,增加硝酸还原酶、亚硝酸还原酶、羟胺还原酶活性,不同处理土壤脲酶、亚硝酸还原酶和羟胺还原酶活性与土壤NH4^ 、NO3^-、NH3挥发和N2O排放速率间存在不同形式的显著相关关系：土壤脲酶、亚硝酸还原酶和羟胺还原酶活性之间存在不同形式的显著正相关关系。     

Impact of biochar application on nitrogen nutrition of rice, greenhouse-gas emissions and soil organic carbon dynamics in two paddy soils of China

Aims

Two field microcosm experiments and ¹⁵N labeling techniques were used to investigate the effects of biochar addition on rice N nutrition and GHG emissions in an Inceptisol and an Ultisol.

Methods

Biochar N bioavailability and effect of biochar on fertilizer nitrogen-use efficiency (NUE) were studied by ¹⁵N-enriched wheat biochar (7.8803 atom% ¹⁵N) and fertilizer urea (5.0026 atom% ¹⁵N) (Experiment I). Corn biochar and corn stalks were applied at 12 Mg?ha^?1 to study their effects on GHG emissions (Experiment II).

Results

Biochar had no significant impact on rice production and less than 2 % of the biochar N was available to plants in the first season. Biochar addition increased soil C and N contents and decreased urea NUE. Seasonal cumulative CH₄ emissions with biochar were similar to the controls, but significantly lower than the local practice of straw amendment. N₂O emissions with biochar were similar to the control in the acidic Ultisol, but significantly higher in the slightly alkaline Inceptisol. Carbon-balance calculations found no major losses of biochar-C.

Conclusion

Low bio-availability of biochar N did not make a significantly impact on rice production or N nutrition during the first year. Replacement of straw amendments with biochar could decrease CH₄ emissions and increase SOC stocks.     

Nitric oxide emissions from rice-wheat rotation fields in eastern China: effect of fertilization, soil water content, and crop residue

A better understanding of nitric oxide (NO) emission from a typical rice-wheat agroecosystem in eastern China is important for calculating the regional inventory and to propose effective NO mitigation options. Nitric oxide flux measurements by static chamber method were made from treatments of conventional nitrogen-fertilizer (NPK plus urea) application, no-nitrogen application, and nitrogen-fertilizer with incorporation of wheat straw residue for an entire rotation period (June 2002 to June 2003). During the wheat growing season two further treatments of fertilizer without crops planted and bare soil without nitrogen (N) fertilization were applied. Total annual NO emissions for the conventional fertilizer, no N fertilizer and fertilizer plus straw application were 0.44?±?0.01, 0.22?±?0.01, and 0.57?±?0.02 kg N ha^?1y^?1, respectively. On average 27% of this emission occurred during the rice season due to flooding/drainage cycle. The N fertilizer-induced emission factor for the conventional fertilizer treatment was 0.05% of the total N applied. Incorporation of wheat straw in the rice season showed no significant effect on NO flux due to the high C/N ratio of the straw incorporated. During the wheat growing season, NO emissions for all treatments had similar variation pattern controlled by soil moisture dynamics. Total NO emissions in the wheat season for fertilized bare soil (no wheat planted) were 0.389?±?0.01 and 0.21?±?0.01 kg N ha^?1 y^?1, respectively. The results indicate the importance of N fertilizer and soil moisture to nitrogen loss through the formation of NO.     

Effects of Biochar Addition on CO2 and N2O Emissions following Fertilizer Application to a Cultivated Grassland Soil

Carbon (C) sequestration potential of biochar should be considered together with emission of greenhouse gases when applied to soils. In this study, we investigated CO₂ and N₂O emissions following the application of rice husk biochars to cultivated grassland soils and related gas emissions tos oil C and nitrogen (N) dynamics. Treatments included biochar addition (CHAR, NO CHAR) and amendment (COMPOST, UREA, NO FERT). The biochar application rate was 0.3% by weight. The temporal pattern of CO₂ emissions differed according to biochar addition and amendments. CO₂ emissions from the COMPOST soils were significantly higher than those from the UREA and NO FERT soils and less CO₂ emission was observed when biochar and compost were applied together during the summer. Overall N₂O emission was significantly influenced by the interaction between biochar and amendments. In UREA soil, biochar addition increased N₂O emission by 49% compared to the control, while in the COMPOST and NO FERT soils, biochar did not have an effect on N₂O emission. Two possible mechanisms were proposed to explain the higher N₂O emissions upon biochar addition to UREA soil than other soils. Labile C in the biochar may have stimulated microbial N mineralization in the C-limited soil used in our study, resulting in an increase in N₂O emission. Biochar may also have provided the soil with the ability to retain mineral N, leading to increased N₂O emission. The overall results imply that biochar addition can increase C sequestration when applied together with compost, and might stimulate N₂O emission when applied to soil amended with urea.     

UV-B辐射增强对小麦秸秆化学成分及其施用后土壤N2O排放的影响

在室外试验的基础上,研究了地表UV-B辐射增强条件下小麦秸秆成分的变化,及在室内不同培养条件下施用UV-B辐射处理后小麦秸秆对土壤N₂O排放的影响.室外试验结果表明：地表UV-B辐射增强减少了小麦地上部分生物量,显著增加了小麦秸秆木质素和全氮含量,增幅分别达94.2%和12.3%,降低了其C/N.室内培养试验结果表明：与常规小麦秸秆相比,UV-B辐射处理后的小麦秸秆显著提高了旱地和淹水条件下N₂O的排放量;施用秸秆同时伴施硝态氮条件下,经过UV-B辐射处理的小麦秸秆显著促进了旱地条件下N₂O的排放,其排放量为常规秸秆处理的3.2倍,但在淹水条件下对N₂O排放无显著影响;无论何种培养条件下,经过UV-B辐射处理的小麦秸秆对土壤呼吸都未产生显著影响.     

UV-B辐射增强对小麦秸秆化学成分及其施用后土壤N2O排放的影响

在室外试验的基础上,研究了地表UV-B辐射增强条件下小麦秸秆成分的变化,及在室内不同培养条件下施用UV-B辐射处理后小麦秸秆对土壤N₂O排放的影响.室外试验结果表明：地表UV-B辐射增强减少了小麦地上部分生物量,显著增加了小麦秸秆木质素和全氮含量,增幅分别达94.2%和12.3%,降低了其C/N.室内培养试验结果表明：与常规小麦秸秆相比,UV-B辐射处理后的小麦秸秆显著提高了旱地和淹水条件下N₂O的排放量;施用秸秆同时伴施硝态氮条件下,经过UV-B辐射处理的小麦秸秆显著促进了旱地条件下N₂O的排放,其排放量为常规秸秆处理的3.2倍,但在淹水条件下对N₂O排放无显著影响;无论何种培养条件下,经过UV-B辐射处理的小麦秸秆对土壤呼吸都未产生显著影响.