有机肥与无机肥在提高土壤肥力中的作用

以在山东禹城试验区持续近20年的定位试验为依据，对长期施用有机肥、无机肥、有机无机结合等不同施肥条件下的土壤养分演变进行了系统总结。结果表明，在同等施肥情况下，有机肥不但在增加土壤有机营养，改善土壤有机质质量等方面具有极其显著的作用，而且随着年限的增长，在增加土壤速效养分方面，有机肥的效果也逐渐超过无机肥。     

长期有机无机肥配施下红壤性稻田水稻产量及土壤有机碳变化特征

利用中国农业科学院红壤实验站红壤稻田长期定位试验,研究了长期有机无机肥配施下双季稻增产潜力和土壤有机碳变化特征。31年的试验结果表明,1）施肥能促进水稻早晚稻稻谷和地上部产量增加,其中,有机肥配施均衡的NPK处理促进作用最大,NPKM处理下稻谷年均产量比NPM、 NKM、 PKM、 M和NPK分别高 5.8%、 10.9%、 16.2%、 15.9%和20.4%。2）施肥能促进水稻土有机碳含量增加,其中,有机肥配施均衡的NPK处理提升效果最为明显, NPKM处理下所测年度土壤有机碳平均含量比NPM、 NKM、 PKM、 M和NPK分别高出2.5%、 3.5%、 2.0%、 0.6%和 32.8%。3）随着试验的进行,单施有机肥对早、 晚稻稻谷和地上部产量的促进效果逐步优于单施化肥氮、 磷、 钾处理（NPK）,对土壤有机碳的提升效果也明显优于单施化肥氮、 磷、 钾。红壤性稻田双季稻生产实践中,有机无机肥配施模式值得推荐,但需均衡配施化肥氮、 磷、 钾。     

Nematode faunal response to long-term application of nitrogen fertilizer and organic manure in Northeast China

Nematode faunal response to the long-term (20-year) application of nitrogen fertilizer and organic manure was monitored in a Hapli-Udic Cambosol of Northeast China, where no fertilizer (C), nitrogen fertilizer (N), organic manure (M) and nitrogen fertilizer plus organic manure (N + M) treatments were compared. The obtained results showed that total nematode abundance responded positively to the M and N + M treatments. The numbers of Acrobeloides increased in the M and N + M treatments at maize jointing and booting stages, and those of Aphelenchoides were higher in the N + M treatment than in the N treatment at maize ripening stage. Early in the growing season, the numbers of bacterivores of cp-1 (cp, colonizer-persister) and cp-2 guilds were higher in the M and N + M treatments than in the N treatment, while those of bacterivores and fungivores of cp-4 guilds were higher in the C treatment than in the N, M and N + M treatments. Except at maize seedling stage, the numbers of fungivores of cp-2 and herbivores of cp-3 guilds were higher in the N + M treatment than in the C treatment. Ratios of the weighted abundance of representatives of specific functional guilds were used as indicators of food web structure, enrichment and decomposition channels. Values of the enrichment index (EI) at maize seedling and jointing stages were higher in the M and N + M treatments than in the C and N treatments, while an opposite trend was observed in the channel index (CI). Higher EI and lower CI suggest an enriched soil food web dominated with bacterial decomposition channels in the M and N + M treatments.     

化肥有机肥配合施用下双季稻田氮素形态变化

为揭示有机无机肥配合施用下稻田氮素的动态及迁移特征,在湘南双季水稻农作区第四纪红土发育的红黄泥稻田上进行了连续6年田间试验。通过比较不施氮肥（PK）、施用有机肥猪粪（M）、化肥（NPK）及有机肥化肥配合（NPKM）,研究稻田表层全氮、无机氮动态变化,不同层次（25—30、55—60、85—90 cm）土壤溶液无机氮动态,耕层土壤无机氮动态等。结果表明,NH4+-N是红壤双季稻田无机氮素存在的主要形态,施用化学肥料处理（NPK）施肥后1～3 d表面水NH4+-N浓度占全氮比例可达0.5～0.9,有机肥处理（M）为0.3左右。不同层次土壤溶液及其土壤氮素浓度呈现一致的特征,即施肥后短期内出现浓度峰值随后迅速下降,且随着往下推移,氮素峰值出现时间延长,表层水全氮及无机氮在施肥后1～2 d出现浓度高峰,耕层土壤及25—30 cm土壤溶液无机氮浓度高峰约在施肥后3～5 d。化肥有机肥配施有利于水稻稳产高产,年产量达12.2 t/hm2,比不施氮肥的对照产量（7.3 t/hm2）增加68%;土壤有机质6年提升18.5%,显著高于化肥。施用有机肥（M）及有机无机肥配合（NPKM）显著降低了稻田表层水全氮及不同层次土壤溶液和耕层土壤NH4+-N峰值浓度,提高水稻产量和培肥土壤,有利于减少当前氮肥过量施用带来的环境负荷。     

黄淮海地区绿肥与化肥配施对棉花生长和肥料利用率的影响

采用田间土柱模拟试验,研究了绿肥翻压与不同比例化肥配施对棉花生长和肥料利用效率的影响。结果表明: 翻压绿肥处理的棉花花铃期叶片SPAD值较不翻压绿肥显著提高,说明翻压绿肥对棉花叶片叶绿素含量有显著影响; 翻压绿肥有助于棉花氮、 磷和钾素的吸收。翻压绿肥处理与不翻压绿肥相比,籽棉产量增加近30%; 翻压绿肥与70%的化肥配施,不会降低棉株养分积累量、 籽棉产量和肥料利用率,且棉花的化肥农学效率明显高于配施100%和85%的化肥处理。     

Changes in P fractions and sorption in an Alfisol following crop residues application

With the emphasis on sustainable agriculture, attention has been increasingly turning to recycling of crop residues as a component of fertility management strategies for tropical soils. We assessed the effects of soybean residue (SR) and wheat residue (WR) applied either alone or in combination with fertilizer P (FP) on dynamics of labile P, distribution of P fractions, and P sorption in a semiarid tropical Alfisol by conducting a 16 w long incubation experiment. The amount of P added through crop residues, FP or their combinations was kept constant at 10 mg P (kg soil)^–1. Addition of SR or WR resulted in net increase of labile inorganic (P_i) and organic P (P_o) and microbial P throughout the incubation period, except that the WR decreased labile P_i during first 2 w due to P_i immobilization. The P immobilization associated with WR addition was, however, offset when fertilizer P was combined with WR. Generally, the increases in labile‐P fractions were larger with the SR and SR+FP than with the WR and WR+FP. The sequential fractionation of soil P at the end of 16 w indicated that a major part of added fertilizer P transformed into moderately labile and stable P fractions as evident from the increased NaOH‐P_i and HCl‐P in the FP treatment. In contrast, the addition of SR and WR alone or in combination with FP favored a build‐up in NaHCO₃‐P_i and ‐P_o and NaOH‐P_o fractions while causing a decrease in NaOH‐P_i and HCl‐P fractions. The addition of these crop residues also effectively decreased the P‐sorption capacity and hence reduced the standard P requirement of the soil (i.e., the amount of P required to maintain optimum solution P concentration of 0.2 mg P l^–1) by 24%–43%. Results of the study, thus, imply that soybean and wheat crop residues have the potential to improve P fertility of Alfisols by decreasing P‐sorption capacity and by redistributing soil P in favor of labile‐P fractions and promoting accretion of organic P.     

The status and fluxes of alkali and alkaline-earth metals in a savanna Alfisol under long-term cultivation

Information on the status and fluxes of alkali (Na, K and Rb) and alkaline-earth metals (Ba, Ca, Mg and Sr) in cultivated soils is required to predict their responses and sensitivity to acidification. The soils for this study were fertilized with NPK (NPK-plot), farmyard manure (FYM-plot) and combined application of FYM and NPK (FYM+NPK-plot) for 50 years. A control-plot, which neither received NPK nor FYM for 50 years, and a natural site were also sampled. Compared to the natural site, significant losses of alkali and alkaline-earth metals occurred in NPK-plot. The FYM+NPK-plot gained excess mass of Ca and Mg, but incurred losses of Na, Rb, K, Ba and Sr. In the FYM-plot, 4% excess mass of Mg and 65% excess mass of Ca were added to the soil, while in the FYM+NPK-plot, 18% excess mass of Mg and 61% excess mass of Ca were added to the soil. The excess masses of Ca and Mg added to these plots partly accounted for from incidental additions through FYM and NPK fertilization and from aeolian sources which, together, were accounted for between 40% and 56% of the Ca-enrichment and between 45% and 100% of Mg-enrichment. Evidence in the study supports the notion that sole application of NPK fertilizers leads to chemical degradation and increases the risk of acidification of savanna Alfisols under continuous cultivation.     

Impact of long-term organic and inorganic nutrient managements on the biological properties and eubacterial community diversity of the Indian semi-arid Alfisol

Intensive cropping with limited nutrient management options in low fertile semi-arid tropical soils will have agricultural sustainability problems in future. A better understanding of soil variables as influenced by long-term nutrient amendments could lead to the identification of more precise indicators to monitor soil fertility that would promote sustainability. Long-term nutrient experiment in semi-arid Alfisol at Coimbatore, India was investigated in two successive years, 2009 and 2010 to assess the enduring effects of organic (OM) and inorganic (IC) nutrient managements on soil variables. The organic amendments induced higher microbial population and enzyme activity compared to IC and control soils. The principal component analysis of observed variables revealed that soil organic carbon, microbial biomass carbon (MBC), dehydrogenase and alkaline phosphatase activity and diazotrophs population could be the possible indicators for predicting soil fertility resulting from long-term nutrient managements. The eubacterial community profile assessed by 16S rRNA gene sequence polymorphism revealed that the abundance and relative ratio of phyla belonging to Proteobacteria, Actinobacteria, Acidobacteria and Firmicutes were considerably affected due to either organic manures or inorganic fertilizers, and organic nutrient management favours bacterial community diversity. These results emphasize the importance of organic nutrient management to maintain soil biological properties in semi-arid Alfisol.     

CO2 emission in an intensively cultivated loam as affected by long-term application of organic manure and nitrogen fertilizer

A long-term field experiment was conducted to examine the influence of mineral fertilizer and organic manure on the equilibrium dynamics of soil organic C in an intensively cultivated fluvo-aquic soil in the Fengqiu State Key Agro-Ecological Experimental Station (Fengqiu county, Henan province, China) since September 1989. Soil CO₂ flux was measured during the maize and wheat growing seasons in 2002-2003 and 2004 to evaluate the response of soil respiration to additions and/or alterations in mineral fertilizer, organic manure and various environmental factors. The study included seven treatments: organic manure (OM), half-organic manure plus half-fertilizer N (NOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (PK) and control (CK). Organic C in soil and the soil heavy fraction (organo-mineral complex) was increased from 4.47 to 8.61 mg C g⁻¹ and from 3.32 to 5.68 mg C g⁻¹, respectively, after the 13 yr application of organic manure. In contrast, organic C and the soil heavy fraction increased in NPK soil to only 5.41 and 4.38 mg C g⁻¹, respectively. In the CK treatment, these parameters actually decreased from the initial C concentrations (4.47 and 3.32 mg C g⁻¹) to 3.77 and 3.11 mg C g⁻¹, respectively. Therefore, organic manure efficiently elevated soil organic C. However, only 66% of the increased soil organic C was combined with clay minerals in the OM treatment. Cumulative soil CO₂ emissions from inter-row soil in the OM and NPK treatments were 228 and 188 g C m⁻² during the 2002 maize growing season, 132 and 123 g C m⁻² during the 2002/2003 wheat growing season, and 401 and 346 g C m⁻² yr⁻¹ in 2002-2003, respectively. However, during the 2004 maize growing season, cumulative soil CO₂ emissions were as high as 617 and 556 g C m⁻², respectively, due to the contribution of rhizosphere respiration. The addition of organic manure contributed to a 16% increase in soil CO₂ emission in 2002-2003 (compared to NPK), where only 27%, 36% and 24% of applied organic C was released as CO₂ during the 2002 and 2004 maize growing seasons and in 2002-2003, respectively. During the 2002/2003 wheat growing season, soil CO₂ flux was significantly affected by soil temperature below 20 °C, but by soil moisture (WFPS) during the 2004 maize growing season at soil temperatures above 18 °C. Optimum soil WFPS for soil CO₂ flux was approximately 70%. When WFPS was below 50%, it no longer had a significant impact on soil CO₂ flux during the 2002 maize growing season. This study indicates the application of organic manure composted with wheat straw may be a preferred strategy for increasing soil organic C and sequestering C in soil.     

Impact of long-term application of fertilizer, manure and lime under intensive cropping on physical properties and organic carbon content of an Alfisol

Intensive cropping with conventional tillage results in a decline of soil organic carbon (SOC) with consequent deterioration of soil physical properties. Some studies indicate that this decline in SOC can be arrested by way of organic manure application and improved nutrient management practices. This study was conducted to find out the long-term effects of inorganic fertilizer, manure and lime application on organic carbon content and physical properties of an acidic Alfisol (Typic Haplustalf) under an annual soybean-wheat crop rotation. Six treatments namely, control (CON), nitrogen fertilization (NIT), nitrogen and phosphorus (NP), nitrogen, phosphorus and potassium (NPK), NPK plus manure (NPKM) and NPK plus lime (NPKL) from a long-term fertilizer experiment continuing at Ranchi, India, were chosen for this study. Soil samples were collected from the selected treatments after 29 crop cycles and analyzed for physical and chemical properties. The results indicated that SOC content in all the treatments decreased from initial levels, but the decrease was considerably less in NPKM (8.7%) and NPKL (10.9%) treatments than that in NIT (28.3%) treatment. The SOC at 0-15 and 15-30 cm depth was lowest in NIT and CON. The NPKM, NPKL and NPK treatments up to 30 cm soil depth recorded significantly higher SOC than NIT and CON. Application of balanced fertilizer along with manure (NPKM) or lime (NPKL) improved soil aggregation, soil water retention, microporosity and available water capacity and reduced bulk density of the soil in 0-30 cm depth over CON. In contrast, soil aggregate stability, microporosity and available water capacity were significantly lower in the NIT plots than that in CON. The study thus suggests that soil management practices in acidic Alfisols should include integrated use of mineral fertilizer and organic manure or lime to maintain the organic carbon status and physical environment of soil.     

Long‐term effects of organic manure and manufactured fertilizer additions on soil quality and sustainable productivity of finger millet under a finger millet–groundnut cropping system in southern India

In a 20‐yr‐old long‐term experiment, the impact of continuous application of organic manures and inorganic fertilizers on soil quality and the sustainability of finger millet production was conducted on two cropping systems: finger millet and finger millet–groundnut on an Alfisol of semi‐arid southern India. The study was conducted from 1992 to 2011 at the All India Coordinated Research Project for Dryland Agriculture, UAS, Bangalore, using a randomized block design. The treatments comprised of T₁: control [no fertilizer and no farmyard manure (FYM) applied], T₂: FYM 10 t/ha, T₃: FYM 10 t/ha + 50% of recommended NPK (50:50:25 kg/ha), T₄: FYM 10 t/ha + 100% of recommended NPK and T₅: 100% recommended NPK. Comparison of long‐term yield data between treatments was used to calculate a ‘sustainability yield index’ (SYI), which was greatest for T₄ (FYM 10 t/ha + 100% of recommended NPK), in both rotational (0.68) and monocropping (0.63) situations. Soil quality indices were determined using principal component analysis linear scoring functions. The key indicators which contributed to the soil quality index (SQI) under rotation were organic C; potentially available N; extractable P, K and S; exchangeable Ca and Mg; dehydrogenase activity and microbial biomass C and N. The largest SQI (7.29) was observed in T₄ (FYM 10 t/ha + 100% NPK), and the smallest (3.70) SQI was for the control. Application of 10 t/ha FYM together with NPK (50:50:25 kg/ha) sustained a mean yield of 3884 kg/ha.     

Cattle manure and inorganic nitrogen fertilizer application effects on soil hydraulic properties and maize yield of two soils of Murewa district,Zimbabwe

This study set out to determine the effects of cattle manure and inorganic N‐fertilizer application on the hydraulic properties and maize yield of a clay and sandy soil in a smallholder farming area of Zimbabwe. Four fields classified as homefields (HF: more fertile and closer to homesteads) and outfields (OF: less fertile and further from the homesteads) were selected on clay and sandy soil. They were subjected to four treatments, control (no fertility amendment), 5, 15 and 25 t/ha cattle manure + 100 kg/ha N (as ammonium nitrate) for 7 years. A two‐way randomized complete block design was used with fertility and field type as the two factors. Clay soil hydraulic properties, which included density of macropores with a diameter >300 μm, unsaturated hydraulic conductivity, steady‐state infiltration rate, moisture retention under low suction and maize grain yield, were significantly improved (P < 0.05) by fertility management compared with the control and were generally comparable between the HF and OF. Fertility management significantly improved maize grain yield on sandy soils but did not enhance hydraulic parameters, thereby indicating poor responsiveness in structural build‐up. On the other hand, significantly different hydraulic parameters between the sandy soil HF and OF suggested effects of other factors not related to soil fertility and field type treatments. We therefore concluded that application of a high rate (25 t/ha) of cattle manure and inorganic N‐fertilizer is beneficial for fertility restoration to the degraded OFs with associated comparable hydraulic properties on HFs and OFs on clay soil, unlike on sandy soil.     

Nitrous oxide emissions after application of inorganic fertilizer and incorporation of green manure residues

Abstract. Emissions of N₂O were measured after application of NH₄NO₃ fertilizer and incorporation of winter wheat and rye green manures in two field experiments in southeast England. Incorporation of green manure alone resulted in temporary immobilization of soil N, small N₂O emissions and also low availability of N for the following crop. Emissions were increased after application of inorganic fertilizer, and were further increased from integrated management treatments whereby green manure residues were incorporated after fertilizer application. The highest emission was from the incorporated winter wheat green manure plus fertilizer treatment, with 1.5 kg N₂O-N ha⁻¹ (0.6% of N applied) being emitted over the first 55 days after incorporation. This high emission was attributed to the supply of C in the residues providing the energy for denitrification in the presence of large amounts of mineral N and the creation of anaerobic microsites during microbial respiration.     

生物有机肥和有机无机复混肥的研制及应用

介绍了利用麦草、鸡粪生产生物有机肥、有机无机复混肥的方法,并在多种农作物上进行了应用效果试验。结果表明,生物有机肥和有机无机复混肥不仅可以提高果品品质,而且在多种作物上具有明显的增产作用。因此,利用麦草、鸡粪等农业废弃物生产的生物有机肥、有机无机复混肥的应用能够减少目前我国农业生产对化肥的过度依赖,有助于我国绿色农业产业的发展。     

定位化肥牛粪配施对设施蔬菜产量和土壤肥力的影响

采用定位施肥方式,连续多次在同一保护地块化肥减量配施牛粪,通过大棚蔬菜种植试验,设置对照(CK,单施复合肥2250 kg/hm2)、低(L,66.7％CK+有机肥30000 kg/hm2)、中(M,33.3％CK+有机肥4500 kg/hm2)及高(H,单施有机肥60000 kg/hm2)4个不同化肥减量配施有机肥底肥...     

猪粪氮素有效性与替代化肥氮当量研究

采用温室盆栽试验,初步研究了猪粪氮素的有效性和替代氮肥的替代当量,并结合田间试验对等有效氮条件下有机无机配施与单施化肥的效果进行了比较。盆栽试验表明,随着猪粪用量的增加,氮素回收率逐渐降低,回收率为22.5%～38.3%,平均30.6%。当猪粪用量为N 120 mg/kg时,其氮素相对于化肥的相对有效性为27%。不同用量下猪粪的替代氮肥当量也具有一定差异,相对替代当量为24.0%～40.8%,平均32.9%。田间试验表明,利用猪粪中的有效氮替代30%的化肥氮对春玉米干物质和籽粒产量以及氮素吸收量没有影响,与100%化肥氮处理相当。     

Changes in amount of organic and inorganic fractions of nitrogen in an Eutrochrept soil after long‐term cropping with different fertilizer and organic manure inputs

The influence of 30 years of cropping with different fertilizer and farmyard manure (FYM) inputs on the contents and depth distribution of organic C, total N (N_t), soil mineralizable N, and organic and inorganic N fractions was investigated in an Eutrochrept. Continuous application of 100 %NPK(+S), 150 %NPK(+S), and 100 %NPK(+S)+FYM led to a marked increase in organic C, total N, hydrolyzable N (viz., amino acid N, hydrolyzable NH₄‐N, hexose amine N, and unidentified hydrolyzable N), and nonhydrolyzable N as compared to an adjacent fallow. The contents of the various organic N fractions were largest in surface soil and thereafter decreased with the depth. However, at 30 – 45 cm depth the content of organic C was not affected by the different treatments except 100 %NPK(+S)+FYM. On the other hand, continuous cropping without fertilization resulted in a depletion of total hydrolyzable N in control over fallow by 27.2 % (0–15 cm), 19.6 % (15–30 cm), and 4.7 % (30–45 cm). The incorporation of FYM with 100 %NPK(+S) resulted in greater contents of soil mineralizable N as compared to 100 %NPK(+S) (0–15, 15–30 cm). The proportion of hydrolyzable N (57–76 % of N_t) decreased and that of nonhydrolyzable N (22–40 % of N_t) increased with depth. The proportion of amino acid N (19–26 % of N_t), hexose amine N (2.1–3.5 % of N_t) and unidentified hydrolyzable N (17–27 % of N_t) decreased with depth. All organic soil N fractions including even nonhydrolyzable N in surface and subsurface soils were highly significantly correlated with soil mineralizable N derived from incubations under waterlogged and aerobic conditions. The best correlation to mineralizable N was found for amino acid N and the least significant correlation for nonhydrolyzable N.     

有机-无机肥长期配施对潮土土壤肥力和作物产量的影响

以24年(19812～004年)的肥料长期定位试验为基础,分析探讨了有机-无机肥长期配施对潮土土壤肥力和作物产量的影响。研究结果表明,除增施秸秆外,增施化肥也能提高土壤有机质的含量,但同时增施化肥和秸秆更有利于土壤有机质的积累。在提高有机质复合量方面,施用化肥的效果好于施用秸秆,而有机-无机肥结合效果较单一施用秸秆或化肥都要高;随秸秆或化肥施用量的增加有机质的复合度逐渐降低,但有机-无机肥结合施用可以提高有机质的复合度。有机-无机结合有利于改善土壤的物理性状,降低了土壤容重,提高了土壤田间持水量和饱和含水量,增加了土壤总孔隙度和毛管孔隙。单施秸秆肥和单施化肥均有显著的增产效应,而化肥的增产幅度远远大于秸秆肥,有机-无机结合的增产幅度在同等施肥量下较单独施用秸秆或化肥的产量都要高。结果表明,有机-无机结合较单一施用秸秆肥或化肥能更有效地提高潮土的土壤肥力,提高作物产量。     

氮肥与有机肥配施协调土壤固定态铵与可溶性氮的研究

【目的】 土壤固定态铵是肥料氮的一个“临时贮藏库”,可逐渐释放以供作物利用,土壤可溶氮则是土壤固定态铵的重要来源,因此研究设施条件下氮肥与有机肥配施对土壤固定态铵和可溶性氮含量的动态变化以及相互关系的影响,对于设施生产中安全高效的施肥管理有着重要意义。 【方法】 以番茄为试材,温室内连续两年进行田间小区试验,设不施肥(CK)、施N量0、187.5、375. 562.5 kg/hm2 (N0、N1、N2、N3)、单施有机肥(M,75000 kg/hm2)以及有机肥与氮肥配施处理(MN0、MN1、MN2、MN3)。分析了土壤固定态铵和可溶性氮(土壤矿质氮和可溶性有机氮)含量动态变化。 【结果】 施肥显著提高了0-30 cm土层土壤固定态铵和可溶性氮的含量(P < 0.01);各施肥处理均以第1穗果膨大期时含量最高。总体来看,不施有机肥条件下,土壤固定态铵和矿质氮、可溶性有机氮的含量均以施N 375.0 kg/hm2处理为最高,而在氮肥与有机肥配施条件下,以施N 375.0 kg/hm2与有机肥75000 kg/hm2配施处理和施N 562.5 kg/hm2与有机肥75000 kg/hm2配施处理的土壤固定态铵和矿质氮、可溶性有机氮含量为最高,但未发现氮肥施用量对土壤固定态铵含量产生显著影响;除收获期20-30 cm土层外,整个生长季内土壤固定态铵和矿质氮含量之间均有显著的正相关关系(P < 0.05),部分土层土壤固定态铵与可溶性有机氮之间也有显著的正相关关系(P < 0.05)。 【结论】 设施番茄栽培条件下,土壤固定态铵和可溶性氮在土壤氮素的固持与释放方面极显著相关,施无机N 375.0 kg/hm2配合有机肥75000 kg/hm2,可较好地提高土壤中的氮的有效性,更好地协调土壤供氮能力。