Soil properties and crop performance on a kaolinitic Alfisol after 15 years of fallow and continuous cultivation

A long-term field experiment was established on a kaolinitic Alfisol in Ibadan, Nigeria, in 1972. The land was cleared manually from secondary forest and used for (i) continuous no-till cropping with maize (Zea mays L.) and maize/cassava (Manihot esculenta Crantz) intercropping, (ii) planted fallow of guinea grass (Panicum maximum Jacq.), leucaena (Leucaena leucocephala de Wit), and pigeon pea (Cajanus cajan Millsp.), and (iii) natural bush regrowth in a randomized complete block design with three replications. At the end of 15 years, the fallow plots were cleared manually and cropped with maize for three years. The chemical and physical soil properties and crop performance of the newly-cleared plots were compared with those under 15 years of continuous cultivation. A total of 26 woody species were identified on the bush regrowth plots. Above-ground biomass accumulation of the bush plots was 157 Mg ha^-1 containing 1316 kg N ha^-1. Guinea grass, leucaena and natural bush regrowth plots had comparable organic C concentrations (approximately 20 g kg^-1) in the surface soil (0 to 10 cm) after 15 years. The organic C concentration in the surface soil under pigeon pea was the lowest (9.5 g kg^-1) among the four fallow treatments. Soil under 15 years of continuous no-till maize with and without residue mulch, respectively, contained approximately half (10 g kg^-1) and a quarter (5.7 g kg^-1) of the organic C under natural bush or guinea grass fallow. The levels of exchangeable Ca, K, Mg and effective cation exchange capacity (ECEC) were lower in the soils under continuous cultivation than in those under natural bush and planted fallow. Soil acidification occurred in soils under continuous cropping as depicted by the lower pH values and greater exchangeable Al and Mn concentrations compared to the fallow plots. Grain yield of maize (3 to 5 Mg ha^-1) without fertilizer application in the plots newly cleared from natural bush, guinea grass and leucaena fallow was comparable with that of continuous no-till maize with residue mulch and chemical fertilizer (N, P, K, Mg, Zn) applications. Among the four fallow treatments, maize grain and stover yields were the lowest in plots cleared from pigeon pea fallow.     

Acidification and alkalinization of lakes by experimental addition of nitrogen compounds

Fertilization of a small lake with ammonium chloride for four years as part of a eutrophication experiment caused it to acidify to pH values as low as 4.6. Implications for acidification of lakes via precipitation polluted with ammonium compounds are discussed.When phosphate was supplied with the ammonium, biological nitrogen uptake, apparently by phytoplankton, was the main mechanism causing acidification. When ammonium was applied without phosphate, it accumulated to high concentrations in solution, after which nitrification caused rapid acidification. In both cases, the whole-lake efficiency of acidification was low, averaging about 13% of the potential acidification of supplied ammonium chloride (Table 2).Subsequent application of phosphate plus sodium nitrate for two years caused the pH of the lake to increase. The efficiency of alkalinization was higher than for acidification, averaging 69% of the potential alkalinization of the supplied sodium nitrate.     

Role of biological nitrogen fixation in legume based cropping systems; a case study of West Africa farming systems

Nitrogen (N) has been gradually depleted from West African soils and now poses serious threats to food production. Many ways of increasing N supply (e.g. judicious use of inorganic fertilizers and nitrogen-fixing plants) have been tried in West African farming systems. Herbaceous and woody legumes commonly contribute 40–70 kg N ha^–1 season. This represents about 30% of the total N applied as residues. Nevertheless and despite repeated demonstrations of the usefulness of green manures in enhancing soil fertility, their practices and adoption are still limited. Promiscuous soyabeans are being used to develop sustainable cropping systems in the moist savannah. Reliable estimates of N₂ fixed by soyabeans and their residual N benefits to subsequent cereal crops in the savannah zone of southern Guinea have only infrequently been made. The actual amounts measured varied between 38 and 126 kg N ha^–1 assuming that only seeds of soyabeans are removed from the plots, the net N accrual of soil nitrogen ranges between minus 8 kg N ha^–1 and plus 47 kg N ha^–1 depending on the soyabean cultivar. Residual soyabean N values of 10–24 kg N ha^–1 (14–36% of the total N in maize) were obtained in a soyabean-maize rotation. Although cereal yields following legume cultivation have been attributed to greater N accumulation, our data show that the relative increase in maize N was smaller than the relative increase in dry-matter yield. Hence, the increased yields of maize following soybeans are not entirely due to the carry-over of N from soyabean residues (as well as to conservation of soil N) but to other rotational effects as well. It is thus clear that the Nbenefit of grain legumes to non-legumes is small compared to the level of N fertilizer use in more intensive cereal production systems but is nevertheless significant in the context of the low amounts of input in subsistence farming.     

Response of cereals to nitrogen in sole cropping and intercropping with different legumes

The response of sole and intercropped cereal to nitrogen fertilization was compared in three contrasting cropping systems, sorghum/pigeonpea, maize/groundnut, and sorghum/cowpea. The cereal in these systems responded to nitrogen similarly as in sole cropping, although different legumes affected the cereal differently. There was no current season benefit from the legume, whether it matured earlier or later than the cereal, and for high yields the cereal in intercropping needs fertilizer application. Response to nitrogen varied with the amount and distribution of seasonal rainfall. With increased nitrogen fertilizer applied to the intercropped cereal, the legume yields were suppressed. The optimum dose for the intercropped cereal was similar to that for sole cropping but it was 50% less in a dry year particularly, on a shallow Alfisol. The combined yields of both crops made intercropping more profitable than sole cropping. The relative advantage of intercropping was high in the sorghum/pigeonpea system (40 to 70%) because of the greater temporal difference between species, and moderate in the maize/groundnut (13 to 35%), and sorghum/cowpea (18 to 25%) systems. Although the relative advantage of intercropping (expressed as Land Equivalent Ratio (LER)) decreased with N, the economic value, of the advantage was little affected within the optimum N range because absolute yields increased with fertilization.     

不同水肥耦合下双季稻氮磷吸收、利用与流失差异

为优化双季稻水肥管理措施,在福建省东部双季稻区设置田间径流小区试验,研究了T₀(对照,未施肥+常规灌溉)、T₁[习惯施肥(273 kg N·hm^-2, 59 kg P·hm^-2, 112 kg K·hm^-2)+常规灌溉]、T₂[优化施肥(240 kg N·hm^-2, 52 kg P·hm^-2, 198 kg K·hm^-2)+常规灌溉]和T₃(优化施肥+节水灌溉)4种水肥耦合处理下双季稻产量、养分吸收利用及田面水氮、磷流失变化。结果表明: 与T₀相比,T₁、T₂和T₃处理早稻稻谷产量显著提高了0.7、1.0和1.1倍,晚稻稻谷产量显著提高了0.9、1.1和1.0倍;T₁、T₂和T₃处理早、晚稻植株地上部分,尤其稻谷氮、磷吸收量增加显著,早稻稻谷氮吸收量分别增加1.1、1.2和1.2倍,磷吸收量增加0.9、1.4和1.6倍,晚稻稻谷氮吸收量增加0.8、1.0和1.0倍,磷吸收量增加0.7、0.9和0.9倍。T₃比T₁处理早稻氮、磷肥农学利用率分别显著增加71.1%和69.2%,晚稻分别显著增加26.4%和25.0%,但田面水可溶性总氮流失量减少了16.0%,并以硝态氮流失为主;T₂与T₃处理早晚稻氮、磷肥农学利用率差异均不显著。本试验中的优化水肥管理措施(T₃)既能促进水稻氮、磷吸收利用,提高双季稻产量,又能降低早稻田面水氮素尤其是硝态氮的流失。本研究可为福建省东部双季稻区水肥利用管理和氮、磷面源污染防治提供理论支持。     

盐胁迫下施肥对棉花生长及氮素利用的影响

利用海水配制不同含盐量(0、0.15%、0.3%)的土壤盆栽棉花,在可移动遮雨棚内研究了不同施肥(N、NK、NP、NPK)处理对棉花生长、氮素吸收与利用的影响.结果表明: 盐胁迫和施肥均影响棉花生物产量、棉株氮素农学利用效率、氮素生物利用效率和氮素积累量,且两者存在显著的互作效应.施肥能提高盐胁迫下棉株氮素利用效率及氮素积累量,并显著增产,不同施肥处理中以N、P、K肥料配合施用的效果最好;施肥效果受盐胁迫程度的影响,低盐胁迫(0.15%)下的施肥效果好于中度盐胁迫(0.3%).     

施肥对麦田土壤可溶性有机氮的影响

利用长期定位试验,研究施肥和小麦生长对土壤可溶性有机氮(EON)的影响。长期不同施肥土壤包括不施肥(No-F)、施用化肥(NPK)和有机肥与化肥配施(MNPK)3种。EON含量范围为7.5—29.3 kg/hm~2,No-F、NPK和MNPK土壤中EON分别占可溶性总氮的40%、56%和56%。长期有机肥与化肥配施显著提高0—15 cm土层EON含量,但对30 cm以下土层EON含量无影响。在小麦开花期,可溶性有机氮的含量及其相对含量显著高于拔节期和收获期。虽然施用氮肥对当季EON含量无显著影响,但同位素示踪微区试验表明,土壤耕层(0—15 cm)中仍有0.4%—2.8%的可溶性有机氮来源于当季施入的肥料氮。可见,化学氮肥向可溶性有机氮的转化缓慢,但农田土壤中可溶性有机氮含量与矿质态氮含量相当,发生淋溶损失的风险大。     

Redistribution of nitrogen in an ecosystem due to long-term fertilization and continuous cropping

Summary When a leguminous crop like cowpea was included in a crop rotation of Ganga 5 maize, CO 7 ragi and CO 2 cowpea, the total nitrogen content in the soil was considerably increased even in the unfertilized plots. The leguminous crop fixed atmospheric nitrogen at the rate of 205 kg N/hectare/year. Potassium did not influence the status whereas phosphorus, over a background of N, improved it. Considerable quantity of N fixed was observed to have been redistributed in the soil which depended on the fertilization pattern.     

氮肥运筹对稻茬冬小麦土壤无机氮时空分布及氮肥利用的影响

以宁麦9号和豫麦34号为材料,研究了氮肥基追比对土壤无机氮时空变化、氮素表观盈亏和氮肥利用率的影响。结果表明,施用基肥提高了越冬期0-60 cm土层NO3--N和NH4+-N含量,拔节期追肥对孕穗期各土层无机氮含量无显著影响,追施孕穗肥显著提高了开花期0-60 cm土层硝态氮含量和0-20 cm土层铵态氮含量。不施氮处理各生育阶段均表现为氮素亏缺,施氮处理氮素盈亏呈明显的阶段性,播种至孕穗阶段出现氮素盈余,孕穗至成熟阶段出现氮素亏缺;全生育期氮素表观盈余量两品种平均以5∶5处理最低,7∶3处理最高。两品种氮肥农学效率、氮肥表观回收率和产量均随基肥比例的增加呈先增后降的趋势,均以5∶5处理最高。因此,在小麦生产中应适当减少基施氮肥用量,在小麦拔节孕穗期适当增加追肥比例有利于提高产量和氮肥利用效率,并降低土壤氮素损失。     

密度与氮肥对关中灌区夏玉米(Zea mays L.)群体光合生理指标的影响

合理的密度是玉米构建良好群体结构、优化群体光合生理功能的基础,适宜的氮肥施用量是玉米进行光合生产的营养物质保障.运用作物群体生理学的方法,采用二次饱和D试验设计,研究了关中灌区夏玉米密度与氮肥耦合和群体光合生理指标的关系及其效应,明确了在关中灌区夏播条件下,在45000～75000株/hm2的密度范围内,密度与玉米籽粒产量、总干物质积累量(DMA)、吐丝期叶面积指数(MLAI)、总光合势(LAD)、平均作物生长率(CGR)为正相关,在45000～60000株/hm2的密度范围内,密度与玉米叶片平均净同化率(NAR)为正相关,而在60000～75000株/hm2的密度范围内,密度与玉米NAR为负相关;在氮素施用量≤600.0 kg/hm2的范围内,氮素施用量与玉米籽粒产量、DMA、CGR为正相关,在氮素施用量≤260.55 kg/hm2的范围内,氮素施用量与玉米MLAI、LAD为正相关,与玉米NAR为负相关,而在氮素施用量260.55～600.0kg/hm2的范围内,氮素施用量与玉米MLAI、LAD为负相关,与玉米NAR为正相关.密度对其影响较大的指标为:籽粒产量、DMA、LAD、CGR和MLAI , 影响较小的指标为:NAR;氮肥对其影响较大的指标为:DMA、CGR、籽粒产量、NAR,影响较小的指标为:LAD和MLAI .对籽粒产量和群体生理指标的综合影响效应,密度显著大于氮肥,玉米生产中,尤其要重视合理密植.通过对回归模型的解析,筛选确定了陕单8806玉米在关中灌区夏播中,实现高产的密度与氮肥耦合优化技术方案:合理密度为61713～66177株/hm2,适宜纯氮施用量为309.88～569.02kg/hm2.     

不同氮素水平下CO_2倍增对转Bt棉花氮素代谢的影响

通过开顶式CO_2气室研究了盛蕾期转Bt棉花新棉33~B及其对照亲本DP5415的生长势和氮素代谢特征对土壤氮素水平(100和200 mg N·kg~(-1))和CO_2浓度倍增(750和375μl·L~(-1))的生理生态响应.结果表明:CO_2浓度升高可显著提高2种棉花的株高和茎粗,增加生物产量;氮素水平提高可显著增加转Bt棉花的株高、茎粗,以及茎和蕾的鲜质量,而对亲本棉花DP5415的影响不显著;对照棉花DP5415的谷氨酰胺合成酶(GS)活力随大气CO_2浓度的升高而显著降低,随氮素营养的提高而升高,转Bt棉花新棉33~B在低氮条件下,GS活力随大气CO_2浓度的升高而显著增加;大气CO_2浓度升高及氮素营养的增加使盛蕾期转Bt棉花的硝酸还原酶(NR)活力显著增加,DP5415的NR活力也随大气CO_2浓度的升高而显著提高;大气CO_2浓度对2种棉花的亚硝酸还原酶(NiR)活力都有明显的抑制作用,其中,高CO_2浓度条件下,DP5415的NiR活力还随氮素营养的增加而显著下降.可见,大气CO_2浓度升高下,土壤氮素水平变化对转Bt棉花的生长势影响显著,但对其氮素代谢生理的影响较对照亲本棉花小.生产中(尤其是高浓度CO_2环境下),应进一步加强转Bt棉花的氮肥优化管理.

Abstract：

By using open-top chambers, this paper studied the physiological and ecological re-sponses of transgenic Bt cotton cv. 33~B and its parent line non-transgenic cotton cv. DP5415 in their growth potential and nitrogen metabolism to doubled CO_2 concentration (750 μl·L~(-1) vs.375 μl·L~(-1)) and nitrogen fertilization level (200 mg N·kg~(-1)vs. 100 mg N·kg~(-1)). Doubled CO_2 concentration promoted the height-and stem growth and the biomass production of the two eultivars significantly, whereas doubled N fertilization level only had significant positive effects on 33~B. The leaf glutamine synthetase activity (GSA) of DP5415 decreased significantly under doubled CO_2 concentration but increased significantly under doubled N fertilization level, while the GSA of 33~B was significantly higher under doubled CO_2 concentration and low nitrogen fertili-zation level. Both the doubled CO_2 concentration and the doubled nitrogen fertilization level in-creased the leaf nitrate reductase activity (NRA) of 33~B significantly, and the NRA of DP5415 also had a significant increase under doubled CO_2 concentration. Doubled CO_2 concentration had significant inhibitory effects on the leaf nitrite reductase activity (NiRA) of both 33~B and DP5415. The NiRA of DP5415 decreased significantly under doubled CO_2 concentration and N fertilization level. All the results suggested that under doubled CO_2 concentration, N fertilization level had significant effects on the growth potential of transgenic Bt cotton but lesser effects on its nitrogen metabolism, compared with the control non-transgenic cotton. Therefore, in the planting of transgenic Bt cotton, especially,under elevated CO_2 condition, optimized N fertilization should be made.     

控释尿素条施深度对鲜食玉米田间氨挥发和氮肥利用率的影响

为提高鲜食玉米一次性施肥的氮肥利用率并降低氮肥的环境影响,通过田间试验,以不施氮处理为对照(CK),研究了控释尿素不同条施深度(0、5、10、15、20 cm)对鲜食玉米田间土壤氨挥发特征、鲜穗产量和氮肥利用率的影响. 结果表明: 玉米种植带和宽行非施肥带的土壤氨挥发主要发生在施肥后的前2周,而窄行施肥带的土壤氨挥发在施肥后持续约1个月. 与CK相比,控释尿素表施(0 cm)处理不仅大幅度地提高了窄行施肥带的氨挥发损失量,同时也显著增加了玉米种植带和宽行非施肥带的氨挥发损失量. 不同深度施肥处理全生育期土壤氨挥发损失总量差异较大,为3.1～25.5 kg N·hm^-2,占施氮量的1.7%～14.2%.其中控释尿素条施10、15和20 cm深度处理的全生育期土壤氨挥发损失总量相差不大,分别较表施(0 cm)和浅施(5 cm)处理显著降低了85.9%～87.8%和67.0%～71.6%. 在一定范围内增加控释尿素条施深度有利于提高鲜穗产量、植株氮积累量以及氮肥偏生产力、氮肥农学利用率和氮肥表观利用率,各指标均以15 cm深度处理最高. 综上所述,控释尿素合理深施可以显著降低氨挥发损失,提高鲜穗产量和氮肥利用效率,本研究条件下控释尿素的最适宜施用深度为15 cm.     

Alley cropping with Senna siamea in South-western Nigeria: I. Recovery of 15N labeled urea by the alley cropping system

Improved cropping systems with in-situ production of organic matter require the input of additional inorganic N to maintain crop production in a sustainable way. For proper management of this fertilizer-N, it is necessary to quantify how the applied fertilizer N is used by the various components of the system and by the system as a whole. The fate of a single application of ¹⁵N labeled urea-N through the different components (crop, hedgerow, surface litter, soil profile up to 150 cm) of a Senna siamea alley cropping system, intercropped with maize in the first and cowpea in the second season, was followed for a period of 1.5 years (1994–1995), equivalent to 2 maize and 1 cowpea crop. Special attention was given to the role of the particulate organic matter (POM) in the cycling of urea-N through the soil organic matter (SOM). The maize crop recovered 26.5 and 1.7% of the applied urea-N at harvest in 1994 and 1995, respectively. The cowpea pods recovered only 0.7% of the applied urea-N at harvest. The highest proportion of applied urea-N recovered by the hedgerow occurred at 38 days after 1994 maize planting (DAP) (3.8%), while at later dates, recoveries of applied urea-N were always below 1%. This indicates that the Senna hedge is not a strong competitor for the applied urea-N during crop growth, i.e. while the Senna canopy is pruned at regular intervals. At 21 DAP, 12.7% of the applied urea-N was recovered in the surface litter and this value dropped significantly to 1.6% at 107 DAP and remained below 1% up to 480 DAP. The top 10 cm of soil contained 21% of the applied urea-N at 21 DAP and this value dropped to 9% at 480 DAP. Significantly more urea-N was recovered in the top 10 cm of soil than in the deeper soil layers at all sampling times. At 21 DAP, 11% of the applied urea-N was recovered in the 120–150 cm layer. This fast movement of urea-derived N to deep soil layers must have happened by preferential flow in macropores as the rainfall between urea application and the first sampling (74.2 mm) was not high enough to explain downward movement of N with the mobile water. Significant linear relationships between the proportion of urea-N in the different soil layers (excluding 0–10 cm) and the anion exchange capacity (AEC) and silt+clay content of the respective layers were found at 67, 107, 347 and 480 DAP. The total N content of the POM fraction increased significantly between 0 and 101 DAP from 127 to 171 mg N kg^–1 and decreased to 92 mg N kg^–1 at 480 DAP. The highest recovery of applied urea-N in the POM pool was measured at 101 DAP (3.6%) and this value decreased to 1.8% at 480 DAP. The total recovery of applied urea-N was 81% at 21 DAP, and decreased to values varying between 53 and 60% up from 38 to 347 DAP. At 480 DAP, the recovery decreased further to 47%. The fast movement of a substantial amount of urea-N may be responsible for this incomplete recovery, already at 21 DAP. Although the soil N status in the fertilized alley cropping system appears to be favourable for plant growth, this may be short-lived in the absence of further urea additions, as the soil-derived maize uptake in 1995 was already significantly lower than in 1994, and as the labile POM pool decreased significantly between the maize harvest in 1994 and 1995.     

长期施肥对潮棕壤有机氮组分的影响

依托长期定位试验(从1990年开始)的4个施肥处理(CK,不施肥;M,循环猪圈肥;NPK,单施化肥;NPK+M,化肥配施循环猪圈肥),探讨了长期施肥对潮棕壤有机氮各组分的影响并揭示了其年际变化特征.结果表明: 从试验开始至2015年,不同施肥模式下各有机氮组分呈现不同的变化趋势,其中酸解有机氮基本上表现为逐年增加的趋势;M和NPK+M处理氨基酸态氮也逐年上升,而CK和NPK处理氨基酸态氮持续下降,这可能与微生物对土壤中氨基酸的利用有关.在整个试验过程中(1990—2015年的平均值),NPK处理酸解铵态氮大幅度增加,比CK增加31.1%;在施加有机肥的2个处理中(M和NPK+M)有机氮各组分均有所提高.与M相比,NPK+M处理各有机氮组分增加的幅度更加明显,这表明有机无机肥配施能有效增加土壤有机氮,进而增强土壤供氮能力,提高土壤肥力水平.     

氮素对高大气CO2浓度下小麦叶片光合作用的影响

通过测定小麦拔节期叶片的光合气体交换参数和光强-光合速率（P_n）响应曲线,研究了氮素对长期高大气CO₂浓度（760 μmol·mol^-1）下小麦叶片光合作用的影响.结果表明：在长期高大气CO₂浓度下,增施氮肥能提高小麦叶片P_n、蒸腾速率（T_r）和瞬时水分利用效率（WUE_i）;与正常大气CO₂浓度相比,高大气CO₂浓度下小麦叶片的P_n和WUE_i增加,气孔导度（G_s）和胞间CO₂浓度(C_i）降低.随光合有效辐射的增强,高大气CO₂浓度下小麦叶片的P_n和WUE_i均高于正常大气CO₂浓度处理,G_s则较低,而C_i和T_r无显著变化.高氮水平下小麦叶片G_s与P_n、T_r、WUE_i呈线性正相关,G_s与C_i在正常大气CO₂浓度下呈线性负相关,但高大气CO₂浓度下二者无相关性;低氮水平下小麦叶片的G_s与P_n、WUE_i无相关性,而与C_i和T_r呈线性正相关,表明高大气CO₂浓度下低氮水平的小麦叶片P_n由非气孔因素限制.     

Decomposition of cowpea and millet amendments to a sandy Alfisol in Niger

Current inputs of organic materials to cropped lands on sandy Alfisols and Entisols in Sahelian West Africa are insufficient to arrest soil organic matter (SOM) decline. Crop residues and green manures require proper management in order to maximize their contribution to nutrient supply and SOM maintenance. The objectives of this study were to quantify the rates of C and N mineralization from cowpea (Vigna unguiculata (L.) Walp.) green manure, cowpea residue, and millet (Pennisetum glaucum (L.) R.Br.) residue under field conditions in Niger and to determine the effect of these organic amendments on pearl millet yield. Millet was grown (1) as sole crop, (2) as intercrop with cowpea, (3) as intercrop with cowpea that was incorporated as green manure during the second half of the growing season, (4) with incorporated cowpea residue (2000 kg ha^–1), (5) with millet residue mulch (3000 kg ha^–1), and (6) with N fertilizer. Carbon loss as CO₂ from soil with and without organic amendment was measured three times per week during the growing season. Nitrogen fertilizer increased millet yield only in a year with a favorable rainfall distribution. Cowpea grown in intercrop with millet during the first part of the growing season and subsequently incorporated as green manure between millet rows increased millet grain yield in a year with sufficient early rainfall, which could be attributed to the rapid rate of decomposition and nutrient release during the first 3 weeks after incorporation. In a year with limited early rainfall, however, densely planted green manure cowpeas competed for water and nutrients with the growing millet crop. Incorporated cowpea residue and millet residue mulch increased millet yield. Surface applied millet residue had high rates of decomposition only during the first 3 days after a rainfall event, with 34% of the millet residue C lost as CO₂ in one rainy season. Recovery of undecomposed millet residue at the end of the rainy season was related to presence or absence of termites, but not to seasonal C loss. Millet residue mulch increased soil organic C content of this sandy Alfisol in Niger. Cowpea and millet residues had a greater effect on SOM and millet yield than cowpea green manure due to their greater rate of application and slower rate of decomposition.     

The Effects of Crop Rotation and Nitrogen Fertilization on Soil Chemical and Microbial Properties in a Guinea Savanna Alfisol of Nigeria

The impacts of crop rotation and inorganic nitrogen fertilization on soil microbial biomass C (SMBC) and N (SMBN) and water-soluble organic C (WSOC) were studied in a Guinea savanna Alfisol of Nigeria. In 2001, fields of grain legumes (soybean and cowpea), herbaceous legume (Centrosema pascuorum) and a natural fallow were established. In 2002, maize was planted with N fertilizer rates of 0, 20, 40 and 60 kg N ha⁻¹ in a split-plot arrangement fitted to a randomized complete block design with legumes and fallow as main plots and N fertilizer levels as subplots. Surface soil samples were taken at 4 weeks after planting and tasselling stage of the maize. Inorganic N fertilization had no significant (P>0.05) effect on SMBC, SMBN and WSOC, while crop rotation significantly (P<0.0001) affected both SMBC and WSOC. These results demonstrate that crop rotation do not necessarily influence the gross soil microbial biomass, but may affect physiologically distinct subcomponent of the microbial biomass. The soils under the various rotations had a predominance of fungi community as indicated by their wide biomass C/N ratio ranging from 9.2 to 20.9 suggesting fungi to be mainly responsible for decomposition in these soils. Soil microbial biomass and WSOC showed significant (P<0.05) correlation with both soil pH and organic carbon but no relationship with total N. Based on these results, it appears that the soil pH and organic carbon determined the flux of the soil microbial biomass and amount of WSOC in these soils.     

半湿润农田生态系统长期施肥对土壤团聚体中有机氮组分的影响

通过对黄土高原半湿润农田生态系统25年的田间肥料定位试验,研究了长期不同施肥模式对土壤有机氮组分及其在各级团聚体中分布的影响.结果表明:长期施肥对水解氨态氮、水解未知氮在土壤各级团聚体中分布的影响最大,对氨基酸态氮的分布有一定影响,而对氨基糖态氮分布的影响较小.长期施用化肥和有机肥能有效地影响水解氨态氮和水解未知氮与团聚体的结合作用,而氨基糖态氮在土壤氮循环转化过程中具有较强的稳定性.长期施肥条件下土壤水解全氮与有机碳、全氮以及团聚体分形维数均呈极显著正相关,其r分别为0.942,0.981,0.910(P<0.001),说明土壤有机氮组分对土壤团聚体的形成和性质具有显著影响.相关分析表明,土壤全氮或有机质对1～2mm和0.25～1mm土壤团聚体中各有机氮组分的影响较大.     

Effect of nitrogen fertilization and cropping system of the reference crop on estimation of N2 fixation by vetch using15N methodology

This study was conducted to examine the effects of varying N rates and cropping systems (mixedversus pure stand) on the suitability of oats (Avena sativa L.) for estimating N₂ fixed in sequentially harvested vetch (Vicia sativa L.) over two growing seasons (1984–85 and 1985–86). The N rates were, 20 and 100 kg N ha^–1 in 1984–85 and 15 and 60 kg N ha^–1 in 1985–86. In the 1984–85 season, vetch at maturity derived 76 and 63% N from fixation at the high and low N rates respectively. The corresponding values for the second season were 66 and 42%. Except in the 1985–86 season when some significantly higher values of % N₂ fixed were estimated by using the reference crop grown at the higher (A-value approach) than at the lower N rate (isotope-dilution approach), both approaches resulted in similar measurements of N₂ fixed. In the 1984–85 season, similar values of N₂ fixed were obtained using either the pure or mixed stand oats reference crops. Although in the 1985–86 season, the mixed reference crop occasionally estimated lower % N₂ fixed than pure oats, total N₂ fixed estimates were always similar (P<0.05). Thus, in general, N fertilization and cropping system of the reference crop did not significantly influence estimates of N₂ fixation.     

长期不同施肥下水稻产量及土壤有机质和氮素养分的变化特征

利用开始于1982年的湖南祁阳官山坪水稻长期(1982-2010年)定位试验,研究不同施肥条件下水稻产量及土壤有机质、氮素养分的动态变化特征,试验设置NPK、NPKM(M为牛粪)、 NPM、NKM、PKM、M和CK等7个处理.28年长期不同施肥处理结果表明：肥料的施用均能提高土壤有机质、全氮、碱解氮含量和水稻产量.氮、磷、钾化肥+有机肥(NPKM)处理的水稻产量一直保持最高水平,氮、磷、钾化肥(NPK)处理随着试验年限的延长呈下降趋势,其水稻产量逐渐低于其他施肥处理.单施有机肥或有机无机肥配施各处理土壤有机质含量在试验开始后的前16年有一个快速增加的过程,之后略有下降,然后仍保持增长趋势;NPK化肥处理土壤有机质含量仅在试验开始后的前8年增加较快,之后在一个相对稳定的范围内波动.各施肥处理在试验开始后的前8年内土壤全氮含量均呈快速积累趋势,以NPKM处理增幅最大.各施肥处理土壤碱解氮含量在试验开始后的前12年增加较慢,平均每年增加0.66～2.25 mg·kg^-1,1994-1998年增加较快,平均每年增加6.45～32.45 mg·kg^-1;1998年之后,各施肥处理土壤碱解氮含量均略有下降,其中,有机无机肥配施处理增加较快,单施化肥处理增加较慢.表明有机肥的施用是红壤性水稻土有机质和氮素营养水平稳定提升的关键措施,是红壤稻田土壤可持续利用的重要保障.