炔草酯的控草效果和对油菜田间光照、养分、水分及 产量的影响

为明确15%炔草酯WP在油菜田的应用前景,建立油菜田的杂草管理体系,研究了不同开沟深度、不同时期施用15%炔草酯WP对油菜田杂草的控制作用以及炔草酯与其他药剂混用的效果,同时研究了该药剂对田间光照、养分、水分和油菜产量的影响。结果表明,开深沟有利于药效的发挥。在禾本科杂草处于1～2叶期时进行药剂处理,一般可以获得比较理想的除草效果。炔草酯与草除灵混用对禾本科杂草和双子叶杂草都具有良好的防除效果。施用15%炔草酯WP能显著提高油菜田间的透光率,降低杂草对田间养分和水分的吸收。15%炔草酯WP的施用对油菜株高、千粒重没有显著影响,但对油菜第一分枝高度、单株分枝数、角果数影响较大,能显著提高油菜产量。     

不同种植方式对织金县玉米产量性状的影响

研究不同种植方式对杂交玉米新品种毕单15号产量性状的影响,结果表明:玉米的果穗性状、植株性状、产量、根系数量和分布范围、叶面积大小和保绿期等均受种植方式影响。其中,以玉米实行宽窄行双行单株错位定向移植效果最佳,比其他几种移栽方式和直播增产显著。     

拟南芥AtCOR15a转化烟草及后代抗寒性研究

【目的】研究拟南芥AtCOR15a基因的抗寒功能。【方法】构建pCAMBIA1301-COR15a的植物表达载体,利用农杆菌介导的叶盘法转化烟草,通过抗生素筛选和PCR检测获得转基因烟草。低温胁迫后,利用蒽酮法和酸式茚三酮法测定转基因烟草后代与野生型烟草的可溶性糖和脯氨酸含量,同时观察其抗寒能力。【结果】转基因烟草后代可溶性糖含量和脯氨酸含量均比野生型烟草有所提高,并在第5 d达到峰值。低温处理后转基因烟草后代能正常生长,而野生型烟草则全部死亡。【结论】生理生化指标的测定发现,可溶性糖含量与脯氨酸含量的变化趋势与烟草的抗寒性呈正相关,AtCOR15a基因导入烟草中可以明显提高烟草对低温胁迫的抵抗力。     

开垦年限对黑土氮初级转化速率和净转化速率的影响

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。     

Role of nitrite and nitric oxide in the processes of nitrification and denitrification in soil: Results from N tracer experiments

Recent research has proven soil nitrite to be a key element in understanding N-gas production (NO, N₂O, N₂) in soils. NO is widely accepted to be an obligatory intermediate of N₂O formation in the denitrification pathway. However, studies with native soils could not confirm NO as a N₂O precursor, and field experiments mainly revealed ammonium nitrification as the source of NO. The hypothesis was constructed, that the limited diffusion of NO in soil is the reason for this contradiction. To test this diffusion limitation hypothesis and to verify nitrite and NO as free intermediates in native soils we conducted through-flow (He/O₂ atmosphere) ¹⁵N tracer experiments using black earth soil in an experimental set up free of diffusion limitation. All of the three relevant inorganic N soil pools (ammonium, nitrite, nitrate) were ¹⁵N labelled in separate incubation experiments lasting 81 h based on the kinetic isotope method. During the experiments the partial pressure of O₂ was decreased in four steps from 20% to about 0%. The net NO emission increased up to 3.7 μg N kg⁻¹ h⁻¹ with decreasing O₂ partial pressure. Due to the special experimental set up with little to no obstructions of gas diffusion, only very low N₂O emission could be observed. As expected the content of the substrates ammonium, nitrate and nitrite remained almost constant over the incubation time. The ¹⁵N abundance of nitrite revealed high turnover rates. The contribution of nitrification of ammonium to the total nitrite production was approx. 88% under strong aerobic soil conditions but quickly decreased to zero with declining O₂ partial pressure. It is remarkable that already under the high partial pressure of 20% O₂ 12 % of nitrite is generated by nitrate denitrification, and under strict anaerobic conditions it increases to 100%. Nitrite is present in two separate endogenous pools at least, each one fed by the nitrification of ammonium or the denitrification of nitrate. The experiments clearly revealed that nitrite is almost 100% the direct precursor of NO formation under anaerobic as well as aerobic conditions. Emitted N₂O only originated to about 100% from NO under strict anaerobic conditions (0-0.2% O₂), providing evidence that NO is a free intermediate of N₂O formation by denitrification. To the best of our knowledge this is the first time that NO has been detected in a native soil as a free intermediate product of N₂O formation at denitrification. These results clearly verify the “diffusion limitation” hypothesis.     

Nitrogen contribution by multipurpose trees to rice and cowpea in an alley cropping system in Sierra Leone

In an alley cropping experiment, a study was carried out on N₂ fixation by Gliricidia sepium, nitrogen (N) accumulation by prunings of Gliricidia, Senna siamea (formerly Cassia siamea) and Gmelina arborea, and the N contribution to associated crops of rice and cowpea.Total N accumulated by the hedgerow trees ranged from 297–524 kg N ha^–1 on average but varied between tree species and depended on the growing season. Gliricidia sepium accumulated 370 kg N ha^–1 on average and more than half of this came from fixation. Senna siamea and Gmelina arborea served as reference trees for estimating N₂ fixation. The estimates of N₂ fixation using Gmelina as a reference gave higher estimates than those using Senna.Although the dry matter and nitrogen yields of prunings from the hedgerow trees were high, their relative nitrogen contribution to the associated crops was generally low ranging from 5 to 29%. Higher crop yields and nitrogen contribution were observed with Gliricidia sepium prunings. The low N contribution from prunings was attributed to the lack of synchronization between the N released from the prunings and the crop's demand for N.     

Carbon and nitrogen dynamics under windrowed residues during the establishment phase of a second-rotation hoop pine plantation in subtropical Australia

The dynamics of carbon (C) and nitrogen (N), derived from the decomposition of windrowed harvest residues, was examined in the establishment phase of a second rotation (2R) hoop pine (Araucaria cunninghamii Aiton ex A. Cunn) plantation in subtropical Queensland, Australia. Following harvesting and site preparation, when residues were formed into windrows, in situ N mineralisation was measured in positions along the three tree-planting rows formed between the windrows. The position above the windrow had a higher nitrification rate than the other positions, averaging about 18 kg N ha⁻¹/month compared with 12 and 9 Kg N ha⁻¹ for the positions between and below the windrow positions, respectively. This position also had consistently greater soil moisture.

Macroplots were formed extending 5 m above and 10 m below a windrow. Windrowed residues within the macroplots were replaced by ¹⁵N-labelled material comprising hoop pine foliage, branch and stem. Hoop pine trees were planted within each macroplot with foliar samples taken at 12 and 24 months. Differences in foliar ¹⁵N enrichment between positions within macroplots were <1‰. Soil samples were taken from positions along the macroplots at 6-monthly intervals. Samples revealed an initial release of labile C and N but soil δ¹⁵N showed that residue-derived N was largely immobilised within the windrows for the 30-month sampling period. Whilst the use of windrows may act as a barrier to the down-slope movement of water, the residue N within the windrows may not be available to the trees of the following rotation for a considerable period following planting. Trees closest to the windrows may be able to introduce roots under the windrows thereby gaining access to the available N, but trees in the central tree planting row are unlikely to derive any significant benefit from the decomposition of windrowed residues.     

用~(15)N示踪法研究不同土壤水分条件下小麦对氮的吸收利用

本研究结果表明,同一施氮量处理小麦地上生物量、茎叶产量和籽粒产量随土壤水分含量的增加而提高,在同一土壤含水量下,这３ 种产量则随氮素肥料施用量的增加而增加。小麦成熟后地上部吸收总氮量的方差分析显示出施氮处理和水分处理对小麦吸氮量的影响达到显著水平,同一施氮处理小麦地上部吸氮总量随土壤含水量的增加而增加,在３ 种土壤水分含量条件下,小麦的吸氮量均随施尿素氮肥量的增加而提高。施尿素处理的土壤Ａ 值随土壤含水量的增加而降低;尿素与猪粪配施处理的土壤Ａ 值则随土壤含水量的增加而增加。在相同施肥量下,尿素氮的利用率随土壤含水量的增加而提高,当田间持水量分别为５０ ％ 、７０ ％ 和９０ ％ 时,小麦对土壤中氮素利用率分别为１３３０ ％ 、２７９７ ％ 和３２２６ ％ ,尿素与猪粪配施处理在３ 种土壤水分条件下的氮肥利用率分别为１９９６ ％ 、２９９０ ％ 和３４３９ ％ 。说明在水分缺乏的情况下,尿素氮的利用率受土壤水分条件的制约,土壤水分充足及无机氮肥与有机肥配施可以提高氮肥的利用率。     

Gross nitrogen transformations and N_2O emission sources in sandy loam and silt loam soils

The soil type is a key factor influencing N(nitrogen) cycling in soil; however, gross N transformations and N_2O emission sources are still poorly understood. In this study, a laboratory ~(15)N tracing experiment was carried out at 60% WHC(water holding capacity) and 25℃ to evaluate the gross N transformation rates and N_2O emission pathways in sandy loam and silt loam soils in a semi-arid region of Heilongjiang Province, China. The results showed that the gross rates of N mineralization, immobilization, and nitrification were 3.60, 1.90, and 5.63 mg N/(kg·d) in silt loam soil, respectively, which were 3.62, 4.26, and 3.13 times those in sandy loam soil, respectively. The ratios of the gross nitrification rate to the ammonium immobilization rate(n/ia) in sandy loam soil and silt loam soil were all higher than 1.00, whereas the n/ia in sandy loam soil(4.36) was significantly higher than that in silt loam soil(3.08). This result indicated that the ability of sandy loam soil to release and conserve the available N was relatively poor in comparison with silt loam soil, and the relatively strong nitrification rate compared to the immobilization rate may lead to N loss through NO_3~– leaching. Under aerobic conditions, both nitrification and denitrification made contributions to N_2O emissions. Nitrification was the dominant pathway leading to N_2O production in soils and was responsible for 82.0% of the total emitted N_2O in sandy loam soil, which was significantly higher than that in silt loam soil(71.7%). However, the average contribution of denitrification to total N_2O production in sandy loam soil was 17.9%, which was significantly lower than that in silt loam soil(28.3%). These results are valuable for developing reasonable fertilization management and proposing effective greenhouse gas mitigation strategies in different soil types in semiarid regions.