Time Course of Nitrogen in Soil Solution and Nitrogen Uptake in Maize Plants as affected by Form and Application Time of Fertilizer Nitrogen

Field experiments with silage maize were conducted in 1987 and 1988 on a loess-derived Luvisol in southwest Germany. Four nitrogen fertilizer treatments were compared: application of preplanting NH₄ N (plus a nitrification inhibitor, dicyandiamide as Didin) and preplanting NO₃-N, split application of NO₃-N (preplanting and side dressed 45 days after planting) and a control without nitrogen fertilizer in 1987 and with 64 kg N ha^?1 as calcium ammonium nitrate in 1988. The total amounts of soil mineral nitrogen (N_min+ fertilizer N) were 200 kg N ha^?1 in 1987 and 240 kg N ha^?1 in 1988. Suction cups and tensiometer were installed at five depths and samples were taken in regular intervals. Nitrate concentrations in the suction solution steeply increased at 15 cm and 45 cm soil depth 3-4 weeks after fertilizer application (1987 up to 160mgNl^?1; 1988 up to 170mgN l^?1) and steeply decreased up to 75 cm depth with the onset of intensive N uptake at shooting. Ammonium concentrations in the suction solution were very low (0-0.16 mg N l^?1). Compared to preplanting NCyN application, preplanting NH₄-N and split NO₃-N application decreased nitrate concentrations in the suction solution in spring 1987. In 1988, however, nitrate concentrations in the suction solution of preplanting NH₄-N and split NO₃-N application plots did not fall below 50mgNl^?1 at 15 cm depth during the growing season. Nitrate concentrations of split NO₃-N application increased again in autumn 1988 and hence doubled the calculated N losses by leaching during the winter months compared to preplanting N applications. At shooting, plants of the preplanting NH₄-N treatment had lower nitrate concentrations in leaf sheaths compared to plants of preplanting NO₃-N application. Total N uptake of maize between shooting and early grain filling of preplanting NH₄-N and split NO₃ -N application tended to be higher compared to preplanting NO₃-N application, reflecting the higher N availability in the soil later in the season. However, final dry matter yields and N uptake were not significantly affected by N form or time of N application. Since N losses by nitrate leaching between N application and onset of N uptake by plants were negligible on the experimental site, preplanting NH₄-N application and split NO₃-N application showed no agronomic advantages. High amounts of side dressed NO₃-N may increase nitrate leaching during the winter months, especially in years with delayed rainfall after application.     

Einfluß des Zeitpunktes der K-Düngung auf die Dynamik des nach der Gülledüngung spezifisch gebundenen NH4-N der Tonminerale*

Influence of the time of K fertilization on the dynamics of NH₄-N fixed by clay minerals after slurry application In a pot experiment with topsoil and subsoil of a luvisol derived from loess the influence of the time of K fertilization on the fixation of NH₄-N supplied with slurry as well as on the leaching and the availability of NH₄-N fixed by clay minerals after slurry application was investigated. The following results were obtained: In both soils K fertilization before slurry application resulted in a reduced fixation of the added NH₄⁺.In the topsoil 8 % of the NH₄⁺ supplied with the slurry could be detected in spring as nonexchangeable NH₄⁺ when slurry was added in October and 13 % when slurry was added in January in the treatment K after slurry, when in the treatment K. before slurry the NH₄⁺ fixed after slurry application had been mobilized totally. In the subsoil 45 % of the NH₄⁺ fixed after slurry application in October were mobilized until spring in the treatment K before slurry and only 20 % in the treatment K after slurry. When slurry was applied in January 30 % and 12 %, respectively, were mobilized. In spite of the reduced nitrogen leaching in the treatments K after slurry yield and N uptake of grass were lower as compared to the treatments K before slurry.     

不同氮素用量对黄瓜幼苗生长及养分吸收的影响

为确定黄瓜幼苗对氮素用量及氮素形态的响应特性以指导育苗期间合理施肥,以硝酸铵磷（NO3--N:NH4+-N为0.9:1.0）为供试肥料,研究同时提供NO3--N和NH4+-N的情况下,不同氮素用量对黄瓜幼苗生长及养分吸收的影响。结果表明：与不施氮对照相比,氮素施用可显著增加植株叶面积和株高,但各施氮处理之间差异不明显（50~200 mg N/株）;植株幼苗茎粗和地上部干物质累积量不同处理间差异不显著;施用氮素黄瓜幼苗根系的根长、根表面积和干物质累积量降低（尤其氮用量100 mg/株）,根系直径在0.5~1.3 mm和1.8~2.6 mm范围内的根长下降明显。氮素用量显著影响了地上部氮、磷、钾的浓度及吸收量,对根系的磷、钾浓度和氮、磷、钾的吸收量影响较小;综合地上部和根系的生长状况,氮素用量在50 mg/株及150 mg/株时,黄瓜幼苗的生长健壮。     

施用生活污泥对滩涂土壤性质及重金属含量的影响

为了探讨应用生活污泥改良滩涂土壤的可行性,明确生活污泥对滩涂土壤理化性质及环境效应的影响,采用符合农用标准的城市生活污泥为材料,通过盆栽培养试验,研究了施用不同用量（0、2.5%、5%、10%、15%、20%,土壤、污泥均以干基计）的生活污泥对滩涂土壤性质及重金属含量的影响。结果表明,施用生活污泥可显著提高滩涂土壤的总氮、总磷、碱解氮、速效磷等养分含量,其中总氮、碱解氮增加的倍数很接近,速效磷增加的倍数远远高于全磷的增加倍数。施用生活污泥显著增加了滩涂土壤的有机质含量,降低了pH值,对土壤可溶性总盐含量无显著影响。施用生活污泥,增加了滩涂土壤Ni、Cd、Zn、Cu、Cr重金属的全量及有效态含量,在实际应用过程中应根据生活污泥重金属的含量确定施用量。     

氮素形态及供应时期对马铃薯生长发育与产量的影响

选用马铃薯克新1号和费乌瑞它2个品种,于2013-2014年在沙培条件下,研究了氮素形态及供应时间对马铃薯植株生长、块茎形成及发育的影响。结果表明,在块茎形成前供应NO₃-N与NH₄-N两种条件下,马铃薯植株高度、叶面积、叶片SPAD值、整株干物质积累量以及块茎重量无显著差异,而块茎形成后供应NH₄-N的马铃薯叶片SPAD值、植株生长速度及块茎产量均显著高于NO₃-N处理;块茎形成前供应NO₃-N的植株结薯数显著高于NH₄-N处理,但是氮素形态对干物质在马铃薯块茎中的分配比例无显著影响。因此,马铃薯的氮素养分管理应根据商品薯和种薯生产的不同目标,在块茎形成前后分别供应适宜形态的氮素。     

Turnover and fate of 15N-labelled cattle slurry ammonium-N applied in the autumn to winter wheat

The fate of ¹⁵NH₄-N labelled cattle slurry applied before sowing in September of a winter wheat crop was studied on a loamy sand soil. The aim was to quantify immobilization of slurry NH₄-N into microbial biomass, the speed at which nitrate derived from the slurry NH₄-N was transported down the soil profile, and the utilization of slurry NH₄-N by the winter wheat crop. Cattle slurry was applied at a rate corresponding to 75 kg NH₄-N ha⁻¹ , with very little loss by volatilization (<4%) due to rapid incorporation by ploughing. The slurry amendment resulted in a doubling of soil surface CO₂ flux, an index of microbial activity, over non-amended soil within the first c. 2 weeks, but ceased again after c. 4 weeks, due to depletion of the easily degradable substances, e.g. volatile fatty acids, in the slurry. Nitrification of the applied NH₄-N was fast and complete by 3 weeks from application, and at this time, the maximum immobilization of slurry NH₄-N into the microbial biomass (23% of applied ¹⁵NH₄-N) was also observed, although no significant increase in total microbial biomass was observed. Rapid turnover of the microbial biomass quickly diluted the assimilated ¹⁵N, with only 6% of applied ¹⁵NH₄-N remaining in the microbial biomass by next spring. Downwards transport of nitrate was rapid in spite of lower than normal precipitation, and slurry-derived ¹⁵NO₃-N appeared in ceramic suction cups installed at 60 cm depth already 2 months after slurry application. Due to the unusually low winter precipitation in the experimental year, wheat yields were high, and the recovery of N in above-ground plant biomass derived from slurry NH₄-N at harvest reached 32%. An additional 45% of the applied slurry NH₄-N could be found in the soil to a depth of 100 cm (mostly in organic form in the plough layer), indicating that 23% had been lost by leaching or in gaseous form. It was concluded that although significant immobilization of slurry NH₄-N did occur, this was not sufficient to prevent leaching of slurry-derived N over the winter and that the relatively high recovery of slurry-derived N in the wheat crop was due partly to lower than normal winter percolation and partly to a relatively high rooting depth on this particular site.     

氮素供应对小麦锌吸收、转运和向籽粒累积影响的研究进展

为进一步实现小麦籽粒锌(Zn)营养强化和氮肥(N)优化管理提供参考,归纳了氮素供应对小麦锌吸收、转运和向籽粒累积的影响。得出：（1）氮素供应是否通过增加锌吸收载体数量（如金属转运蛋白ZIPs家族中的类铁调控IRT-like蛋白）提高根系对锌的吸收;是否通过促进木质部中与锌螯合的含氮化合物如尼克酰胺(NA)和有机酸如柠檬酸的合成,或通过提高锌转运载体（如重金属腺苷三磷酸酶HMA和类黄色条纹YSL家族蛋白）的数量促进锌从根系向地上部的转运;是否通过提高NA或YSL的数量促进锌从营养器官向籽粒的再转移,均值得进一步研究。（2）应加强不同形态氮素（如硝态和铵态氮）和叶面喷施的研究,将¹⁵N和^67/68Zn同位素标记结合定量化深入研究氮素的影响。     

Der Einsatz von Reststoffen der Altpapieraufbereitung auf landwirtschaftlich genutzten Flächen als Bodenverbesserungsmittel

The application of secondary paper mill sludges on arable soils to improve soil fertility
In field investigations the application of secondary paper mill sludges on arable soils was tested. No deterioration could be verified with regard to soil and plant growth. However an improvement was not significant.
Accumulation of heavy metals in soils or plants was not observed. There was no risk of soils and plants, because the contents of organic halogen compounds were much lower than the common administrative threshold values. The carbonate content of the sludges was variing very much. This is why a prognosis of the pH-effect was difficult. Nitrogen was fixed in the soil during decomposition of the sludge, which was poor in nitrogen.
An application of secondary paper mill sludge on arable soils have to be connected with a fertilization to equalize nitrogen supply. Industrial process should guarantee always a similar carbonate content in the sludge to avoid micronutrients deficiency.     

氮肥形态及氮钾施用措施对水稻生长 和养分吸收的影响

为探明不同氮（NH4-N和NO3-N）源下，不同施钾水平及氮钾施用次序对水稻生长和养分吸收的影响，进行了温室盆栽试验。结果表明：在水稻生长早期（20d左右时），以NO3-N作为N源时水稻的生物产量和氮钾养分吸收量均显著高于NH4-N作N源的处理，但随着生长时期的延长，NH4-N源更能促进水稻的生长和养分吸收，因此，从整个营养生长时期来讲，铵态氮肥作为水稻N源更具有优越性。结果同时表明，氮肥施用效果与钾肥的施用水平有很大关系，在一般盆栽试验氮肥用量（纯N用量0.15 g/kg）水平下，施钾（K2O）量达到0.51g/kg时会导致水稻的生长及养分吸收量显著下降。铵钾施用次序对水稻的营养生长及养分吸收均有一定的影响，特别是施钾量较高时，铵钾在土壤中的交互作用会导致水稻因氮素供应不足而影响生长和养分吸收。     

水分管理和氮肥运筹对水稻养分吸收、转运及分配的影响

在高产施氮量180 kg hm^-2条件下,以杂交稻冈优527为材料,通过“淹水灌溉”(W₁)、“湿润灌溉(前期)+浅水灌溉(孕穗期)+干湿交替灌溉(抽穗至成熟期)”(W₂)和“旱种”(W₃) 3种灌水及不同的氮肥运筹处理,研究水分管理和氮肥运筹对水稻养分吸收、转运、分配及产量的影响,并探讨各养分间及其与产量的相互关系。结果表明,水分管理和氮肥运筹对水稻主要生育期氮、磷、钾的累积、转运、分配及产量的影响均存在显著的互作效应,水氮互作条件下各生育期氮、磷、钾间的吸收存在显著的协同效应;抽穗期氮、磷、钾的累积与各养分在结实期转运总量间,以及结实期各养分转运间均呈极显著正相关,且氮、钾在抽穗前期的累积对促进结实期各养分向籽粒的转运和提高产量影响显著,但氮肥后移比例过重(N₄处理)及W₃处理均会导致结实期叶片和茎鞘各养分转运总量的显著降低,氮、磷、钾降幅分别达2.73%~18.00%、8.03%~19.70%、6.52%~17.02%。据产量及其与养分吸收、转运间关系的表现,W₁模式下氮肥后移量以占总施氮量的40%~60%为宜,W₂模式与氮肥运筹方式为基肥:蘖肥:孕穗肥(倒四、二叶龄期分2次等量施入)=3∶3∶4组合是本试验最佳的水氮耦合运筹模式,W₃模式下,应减少氮肥的后移量,氮肥后移量占总施氮量的20%~40%为宜。     

水分、磷肥耦合对小麦各生育期土壤中氮磷养分的影响

通过田间试验,研究了施磷量、施磷深度和不同水分条件对冬小麦不同生育期土壤中氮、磷养分含量的影响。结果表明,在3种处理条件下,土壤中NO3-_N随小麦各生育期对氮素需求量而变化,在返青期和灌浆期,其在土壤中的含量均出现最低谷;土壤中的NH4 _N的含量在孕穗期出现高峰,其他生育期含量变化无明显影响;同样,土壤中有效磷含量在返青期和灌浆期出现低谷,而拔节或孕穗期达到高峰。根据土壤中氮磷养分的动态变化,推荐整个生育期灌水2次,施磷量及施磷深度分别为225 kg/hm2和30 cm。     

小麦/玉米/大豆和小麦/玉米/甘薯套作对土壤氮素含量及氮素转移的影响

为探讨小麦/玉米/大豆套作对氮素营养的种间促进机制, 采用叶片¹⁵N富积标记法研究了小麦/玉米/大豆(A1)和小麦/玉米/甘薯(A2) 2种套作系统中不同施氮水平下的土壤培肥效果和氮素转移规律。结果表明,施氮可以提高小麦、玉米的土壤总氮含量,以施纯氮150~300 kg hm^-2处理最高;大豆较甘薯更有利于保持土壤肥力,施氮0、150、300和450 kg hm^-2水平下种植大豆后的土壤总氮含量比种植大豆前(小麦收获后)高38.6%、20.2%、9.4%和16.7%,而种植甘薯则降低总氮含量3.1%、1.8%、14.0%和3.8%。A1系统中小麦和玉米季土壤中NO₃-N含量低于A2系统,且随施氮量的增加而增加;大豆季土壤中NO₃-N含量高于甘薯季。A1和A2系统均存在¹⁵N的双向转移,¹⁵N转移量随施氮量的增加而降低,且A1的¹⁵N净转移量和转移强度高于A2;A1系统中小麦、玉米和大豆的¹⁵N净转移量比A2系统的¹⁵N净转移量分别高3.3%~12.1%、27.0%~166.2%和26.2%~78.7%。玉米与小麦之间的¹⁵N净转移方向为从玉米向小麦,玉米与大豆之间的¹⁵N净转移方向为从大豆向玉米,玉米与甘薯之间的¹⁵N净转移方向为从玉米向甘薯。     

稻田田面水氮磷素动态特征研究

为了合理运筹施肥,防控农业面源污染,通过独立排灌系统的田间试验,设计了6个不同氮肥水平,研究了施肥后水稻田田面水氮素和磷素的动态变化特征。结果表明,施肥后田面水中的总氮(TN)、NH4+-N和NO3--N浓度随着施肥量的增加而增加,随着时间的推移三者的浓度呈现上升后下降的趋势,7天后趋于稳定;施入基肥后,NH4+-N浓度在第2天达到峰值后迅速下降,第3天即下降到峰值的25.69%~36.80%;NO3--N浓度远远低于NH4+-N浓度,3个施肥时期峰值分别为8.87 mg/L、1.91 mg/L和1.50 mg/L,且出现在施肥后第3~5天。田面水NH4+-N/TN随着施氮量的增加而增加,且在施肥后第2~3天达到峰值后下降。不同施氮量,相同施磷量处理条件下,田面水中TP浓度随着施氮量增加而增加;施肥后第1天,田面水中TP浓度达到峰值3次施肥后TP浓度峰值逐渐降低。     

Strategies to Improve the Use Efficiency of Mineral Fertilizer Nitrogen Applied to Winter Wheat

Recovery of fertilizer nitrogen (N) applied to winter wheat crops at tillering in spring is lower than that of N applied at later growth stages because of higher losses and immobilization of N. Two strategies to reduce early N losses and N immobilization and to increase N availability for winter wheat, which should result in an improved N use efficiency (= higher N uptake and/or increased yield per unit fertilizer N), were evaluated. First, 16 winter wheat trials (eight sites in each of 1996 and 1997) were conducted to investigate the effects of reduced and increased N application rates at tillering and stem elongation, respectively, on yield and N uptake of grain. In treatment 90‐70‐60 (90 kg N ha^?1 at tillering, 70 kg N ha^?1 at stem elongation and 60 kg N ha^?1 at ear emergence), the average values for grain yield and grain N removal were up to 3.1 and 5.0 % higher than in treatment 120‐40‐60, reflecting conventional fertilizer practice. Higher grain N removal for the treatment with reduced N rates at tillering, 90‐70‐60, was attributed to lower N immobilization (and N losses), which increased fertilizer N availability. Secondly, as microorganisms prefer NH₄⁺ to NO₃^? for N immobilization, higher net N immobilization would be expected after application of the ammonium‐N form. In a pot experiment, net N immobilization was higher and dry matter yields and crop N contents at harvest were lower with ammonium (ammonium sulphate + nitrification inhibitor Dicyandiamide) than with nitrate (calcium nitrate) nutrition. Five field trials were then conducted to compare calcium nitrate (CN) and calcium ammonium nitrate (CAN) nutrition at tillering, followed by two CAN applications for both treatments. At harvest, crop N and grain yield were higher in the CN than in the CAN treatment at each N supply level. In conclusion, fertilizer N use efficiency in winter wheat can be improved if N availability to the crops is increased as a result of reduced N immobilization (and N losses) early in the growth period. N application systems could be modified towards strategies with lower N applications at tillering compensated by higher N dressing applications later. An additional advantage is expected to result from use of nitrate‐N fertilizers at tillering.     

施用河道污泥对水稻氮素吸收利用的影响

为了探索污染河道污泥农业资源化利用的有效途径,本研究以河道污泥为研究对象,设计施N量为120、240 kg/hm2 2 个水平,研究河道污泥农田施用对不同生育时期水稻氮素含量、氮素吸收、氮素分配和氮素利用效率的影响。结果表明：（1）施用河道污泥使不同生育时期水稻植株含氮率显著提高,使各生育时期氮素累积量显著提高;（2）使水稻抽穗后氮素在茎鞘中的分配比例显著提高,使水稻抽穗后氮素在叶片和穗中的分配比例明显下降;（3）使不同生育时期水稻氮素干物质生产效率以及氮素籽粒效率均显著或极显著降低,但对水稻氮素收获指数影响不显著;（4）河道污泥×N的互作效应对稻株氮素吸收利用无显著影响。施用河道污泥使水稻植株含氮率、氮素累积量显著增加,而水稻氮素干物质生产效率和氮素籽粒效率则显著降低。     

氮磷钾对红花草固氮根瘤菌生长及种植后土壤肥力的影响

为了发展有机水稻,以红花草-有机水稻轮作培肥水田土壤肥力,研究氮、磷、钾对红花草固氮根瘤菌生长及种植后土壤肥力的影响,为红花草的合理种植、培肥地力提供依据。2012—2013 2年稻后茬种植红花草,过冬前分别单独施用不同用量的氮肥、磷肥、钾肥,以不施肥为对照,探讨不同肥料不同用量对红花草产草量、固氮根瘤菌数量、固氮根瘤菌重量的影响及种植后的土壤肥力变化状况。研究结果表明：红花草前期补施氮、磷、钾,氮素对红花草的影响较大,在施氮75 kg/hm²(N 46%)时,产草量最高,固氮根瘤菌数量最多,固氮根瘤菌重量大;种植后土壤全氮变化表现为不同施氮量增幅随肥料用量增加而增加,施磷、施钾各处理增幅随肥料用量增加而先降后升;土壤速效磷变化为施氮、施磷各处理增幅随肥料用量增加而增加,施钾各处理增幅趋势表现不明显;土壤速效钾变化表现为施氮、施磷各处理增幅变化趋势是随肥料用量增加先升后降,在施氮150 kg/hm²(N 46%)、施磷300 kg/hm²(P₂O₅ 12%)时,土壤速效钾增幅达最大;土壤有机质变化表现为增幅随肥料用量增加而增加。所以,种植红花草,前期适当补施氮、磷、钾,可以提高红花草产草量,有效提高土壤肥力。     

滴灌水肥一体化下施氮量对小麦氮素吸收及土壤硝态氮含量的影响

为探明华北地区山前平原水肥一体化条件下小麦合理的氮肥运筹。于2013-2015年2个小麦生长季,设置4个滴灌施氮量(N0-不施氮、N1-120 kg/hm~2、N2-240 kg/hm~2、N3-360 kg/hm~2)处理,研究滴灌水肥一体化下施氮量对小麦氮素吸收积累和土壤硝态氮含量的影响。结果表明:施氮量N1、N2和N3处理的小麦干质量及产量较处理N0显著增加,N1、N2和N3处理间无显著差异;施氮量对小麦茎秆的氮含量影响较大,但对籽粒氮含量的影响差异不显著;处理N3的小麦总吸氮量分别显著高于处理N0、N1和N2,但处理N1和N2之间无显著差异;氮肥收获指数以N2处理最高,氮肥当季回收利用率、氮肥农学效率、氮肥生产效率和氮肥利用效率均表现出随施氮量增加而降低的趋势;施氮量超过240 kg/hm~2,土壤硝态氮含量增加,且随种植年限的延长更加明显。采用一元二次方程拟合,获得小麦最高产量的施氮量为238.46~250.78 kg/hm~2,经济施氮量为174.28~207.18 kg/hm~2。综合考虑经济效益和生态效益,该条件下小麦滴灌经济施氮量以174~207 kg/hm~2为宜。     

水氮互作对夏玉米氮素积累运转及利用的影响

[目的]为探索水氮高效利用、减少农田氮肥污染途径,[方法]设置了不同水分和不同施氮水平的互作试验,研究其对夏玉米植株氮素积累运转及氮肥利用的影响。[结果]结果表明,与不施氮相比,施氮处理显著提高了植株氮素积累量,最终氮素积累量增加了24%～35%;施氮增加了茎叶及整株等营养器官花前贮藏氮素运转量,灌水增加了茎、叶、穗及全株花前贮藏氮素运转量,同时施氮和灌水均明显增加籽粒氮素积累总量,且处理间均表现为处理2＞处理1＞处理0。与处理0比,施氮处理籽粒氮素总量增加26.31%,灌水处理增加24.89%;施氮和灌水明显提高了氮素吸收效率和氮肥农学效率,对氮素利用效率影响结果不一。[结论]综合本试验研究结果,以N1W2处理综合表现最优,可以考虑生产中推广应用。     

不同氮素处理对中麦175和京冬17产量相关性状和氮素利用效率的影响

本研究旨在了解我国黄淮和北部冬麦区不同施氮量和施氮模式对氮高效吸收和利用的影响,以及中麦175和京冬17产量对不同施氮处理的响应。2013-2014和2014-2015连续两年在河北吴桥和北京顺义两地种植两品种,观测不同施氮量和基追比处理下,冬小麦的群体特性、产量相关性状,以及氮素吸收效率(NUpE)和氮素利用效率(NUtE)。在吴桥点设0、60+0、120+0、120+60、120+120、120+180 kg hm?2 (基肥+拔节肥) 6个处理,在顺义点仅设前5个处理。在总施氮量0~240 kg hm?2 (吴桥)和0~180 kg hm?2 (顺义)范围内,随施氮量增加,归一化植被指数(NDVI)和气冠温差(CTD)提高,群体总粒数和成熟期生物量增加,进而产量提高;但继续增加施氮量会导致粒重、开花前干物质向籽粒转运量、转运率、对籽粒贡献率、收获指数、氮肥偏生产力、氮素吸收和利用效率降低。在不同施氮水平下,中麦175的产量和稳定性均优于京冬17,表现出穗数多、穗粒重稳定性好、群体活力持久、生物量和收获指数高、花前干物质积累量高和花后干物质转运能力强、氮素吸收效率高,这可能是其高产高效的重要基础。考虑到产量回报和经济效益,推荐中麦175和京冬17在黄淮麦区(北片)施氮量为180~240 kg hm?2,在北部冬麦区施氮量为120~180 kg hm?2。灌浆中后期,NDVI和CTD与穗数、产量和生物量相关性高,可作为快速评价品种氮肥敏感性的指标。     

施用污泥对土壤中重金属含量的影响

随着城市污水处理厂数量的迅速增加,污泥的处置及其环境影响受到越来越多的关注。污泥土地利用因具有处理费用低廉及高效性的特点,已成为重要的污泥处理方式。然而污泥中的重金属元素是限制其大规模农田利用的重要因素。施污土壤中重金属的形态研究可以用来评价土壤中重金属的生物有效性以及它们在土壤中的移动性。用修正BCR三步连续提取法进行分步提取研究了施污后的水稻田土壤中Cu、Pb、Cd、Zn的形态分布状况。与对照相比,在直接施用污泥的水稻田土壤中Cu、Pb、Cd、Zn的含量显著增加。但即使是在施污60t hm-2的土壤中,Cu、Pb、Zn的含量亦远低于我国土壤环境质量标准。在施污的水稻田土壤中4种重金属元素的形态分布规律为：残渣态＞可氧化态＞可还原态＞可交换态和弱酸溶解态。这些重金属元素在水稻田土壤中相对稳定性顺序为Zn＞Cu＞Cd=Pb。