施硫肥对内蒙古典型草原放牧生态系统硫循环的影响及硫肥需要量的研究

应用总体平衡(mass-balance)法研究了施硫肥(0, 30及60 kg S/hm2)对内蒙古典型草原放牧生态系统硫循环的影响及在硫肥需要量上的应用.结果表明,施硫肥使牧草硫的吸收量提高了50%,并使放牧系统硫的生物循环速率提高了15%以上.1995和1996年两年内两种硫肥处理30 和 60 kg S/hm2的硫的利用效率分别为74.0% 和 37.6%.当其他硫的来源较低时,土壤中有机硫的矿化是草原有效硫的主要来源,约占整个有效硫输入量的70%.放牧家畜在物质循环中具有重要的生态功能,其硫采食量的90%左右以排泄物的形式返回到土壤,经过排泄物而释放的有效硫量约占硫的生物再循环量的30%.土壤中硫的淋溶损失是放牧系统中硫的主要输出形式;同时,家畜尿和粪中硫的损失(包括转移到非生产区和淋溶损失)也影响着放牧系统硫的平衡状况.因此,应该深入研究粪尿硫的再循环速率及其影响因素.基于总体平衡原则,该地区放牧系统中至少每年应施入10 kg S/hm2才能保持有效硫的平衡状态.     

内蒙古典型草原主要土壤类型和植物硫状况的研究（英文）

通过对内蒙古典型草原4种主要土壤类型及122种主要植物硫含量的分析,并与主要放牧家畜的营养需要相结合,综合评价了内蒙古典型草原硫的营养状况.研究表明4种主要土壤类型不同层次(0.2～0.4m,0.1～0.2m和0～0.1m)的土壤中有机硫的含量变化很大,为17～397μg*g-1,有机硫的含量与土壤中有机碳和全氮含量呈高度正相关.土壤中平均无机硫含量低于10μg*g-1,但黑钙土土壤中无机硫的含量较高,达20μg*g-1左右.土壤中微生物硫含量占土壤中全硫含量的1.78%～2.80%.所测定的122种主要植物中有75%的植物体内硫含量低于0.16%,氮/硫比大于14∶1;与主要放牧家畜的营养需要相比,有约80%的植物缺硫.植物体中硫的含量与土壤中有效硫的含量显著正相关.     

放牧家畜排泄物N转化研究进展

放牧家畜排泄物氮转化是草原生态系统氮循环的关键。自 2 0世纪 70年代以来 ,以提高氮利用效率和减少温室气体排放为目的的家畜排泄物氮转化的研究越来越受到人们的重视。放牧家畜排泄物氮的转化研究主要包括 3个方面 :氮的矿化、硝化与反硝化 ,氮的氨化。家畜粪氮矿化速度慢 ,持续时间长 ;尿氮矿化速度快 ,持续时间短。氮矿化与家畜排泄物 C∶ N比、木质素/氮素比、木质素含量和纤维素含量呈负相关关系 ,而与全氮含量和水溶性氮含量呈正相关 ;土壤动物和微生物可以显著促进氮的矿化过程 ;高温和相对干燥、砂质土壤较壤土和粘土有利于氮的矿化。 4～ 4 0℃氮硝化作用与温度呈正相关 ;硝化作用的底物和产物浓度、土壤溶液渗透压和氯化物浓度的增加对硝化作用有强烈的抑制效应 ;p H6 .0～ 8.0条件下硝化作用强度随着土壤p H值的升高而增加 ,而 p H值高于 8.0或低于 6 .0时硝化作用受到抑制 ;硝化作用与土壤氧气含量呈正相关关系 ,而与土壤含水量呈负相关 ;温暖湿润较干燥炎热的气候条件有利于硝化过程的进行。反硝化作用与土壤氧气浓度呈负相关关系 ,而与土壤含水量和可利用有机碳含量呈正相关 ;0～ 6 5℃反硝化作用强度随温度升高而增大 ,10～ 35℃条件下温度成为影响反硝化作用的关键因素 ;反硝化作用在     

硫加树脂包膜尿素控释肥对小麦干物质积累分配及产量的影响

在田间高产条件下,设置硫加树脂包膜尿素控释肥(SRCU)、树脂包膜尿素控释肥(RCU)、普通尿素加硫磺粉(SU)、普通尿素(U)处理,研究硫和SRCU对冬小麦干物质积累与分配及产量的影响.结果表明:施用RCU处理的植株干物质积累量和籽粒产量与分期施氮不施硫处理相比无显著差异.在土壤有效硫含量为43.2 mg·kg-1的条件下,施硫量为91.4 kg·hm-2的SRCU处理与相同施硫量分期施氮处理相比,花后干物质积累与分配及产量无显著差异;与无硫的RCU处理相比,花后同化物输入籽粒量、籽粒灌浆中期的灌浆速率、千粒重和产量均显著提高.在土壤有效硫含量为105.1 mg·kg-1的条件下,施硫量为120kg·hm-2的SRCU处理籽粒产量显著高于相同施硫量分期施氮处理,与不施硫分期施氮处理和RCU处理无显著差异.说明SRCU释放的氮素对冬小麦干物质积累、分配和产量的调节作用与速效氮素分期施用的效果一致.SRCU释放的硫素对冬小麦的调节作用受土壤有效硫含量高低的影响,在有效硫含量为43.2 mg·kg-1的条件下,能促进花后干物质积累和籽粒灌浆,显著提高籽粒产量;在有效硫含量为105.1 mg·kg-1的条件下,则无显著增产作用,过多施用硫磺粉还可导致产量显著降低.     

有机-无机态肥氮在微型农业生态系统的转移和循环研究

本文应用~(15)N示踪法研究了有机态和无机态肥料氮在微型农业生态系统中循环的机理,以及配施下各自的功能和相互影响。初步结果表明,在土壤-黑麦草-兔亚系统中,草对硫铵~(15)N利用率达59.36％;以草饲兔,所收集兔粪~(15)N回收率为11.78％,尿为17.98％。兔粪尿N与硫铵N以1:0,0.5:0.5,0.3:0.7和0.1配施种稻,结果表明,在土壤-水稻亚系统中:(1)0.5:0.5配施促进穗头和根系发育;(2)稻株吸收有机态和无机态肥料N的比例,受配施比例的影响;(3)与单施无机肥料氮比较,配施下无机肥料氮利用率未提高或甚至下降;(4)0.3:0.7配比使有机态肥料N利用率提高;(5)0.5:0.5配比,有机肥能明显地促进无机态肥料N从秆向谷运输;(6)有机肥使无机态肥N在土壤中的固化作用增加,从而使无机肥料氮向环境转移量下降。农业生态系统具有多组分和牧食-碎屑复合食物链,氮素再循环指数达0.5,生态稳定性和发育程度优于单一种植系统。     

模拟放牧斑块与氮素添加对半干旱草原群落植物生长的影响

放牧时,动物采食及其排泄物会影响植物的生长,但动物彩食及其排泄物的空间异质性可能会影响这咱效应.在位于我国北方典型农牧交错区的内蒙古多伦县,我们研究了模拟入牧斑块和施氧肥对植物生长的影响,实验采用模拟放牧采食斑块(观割半径分别0、10、20、40和8cm)和土壤施氮(分别为0、5、20Gn\m2)两种处理,植物地上部收获后分为绿体和立柯两部分,并分析其含氮量.结果表明,刈割降低了植物的生物量(40.5%),而施氮可增加生物量(57.8%)刈割交通规则植物生长的抑制作用在面积最水又施肥的斑块上表现更明显.土壤施氮可以促进杜物生长并且影响刈割效应.同时植物的绿-枯比阻碍施氮水平的增回而增回,因此氮会延迟植物的衰老.以上结果表明,刈割(模拟动物采食)斑块的大小会影响草原植物的生长,土壤施氮(模拟动物尿氮)可以提高草原生态系统的初级生产力,并影响刈割效应.     

控释肥硫膜降解对微域土壤性质的影响

硫包膜控释肥在农业上的大面积应用,引起了硫膜降解产物对土壤环境影响的广泛关注。选用山东有代表性的耕作土壤棕壤和潮土,设置处理包括硫加树脂残膜、硫残膜、硫磺片,采用尼龙滤网分隔法获取受控释肥硫膜影响较强的微域土壤,对比研究了硫膜对微域和非微域土壤某些化学性质的影响。结果表明,在棕壤上施用各含硫材料会显著影响微域土壤的pH值,微域各含硫材料的氧化高峰期出现在60d左右。硫膜降解对潮土pH值影响与棕壤相比不显著,但肥际微域与非微域相比下降明显。硫残膜对土壤中的微量元素能起到一定的活化作用,尤其是对潮土肥际微域有效铁的影响最为显著,培养结束时硫加树脂残膜处理是空白处理的6.58倍。潮土中施用含硫包膜控释肥可活化土壤养分,从而提高土壤中有效硫和有效磷的含量。控释肥硫膜降解对土壤性质影响显著的区域是在硫膜≤5mm范围内的土壤,而对非肥际微域土壤的化学性质无显著影响。     

硫肥对春油菜幼苗生理指标和土壤酶活性的影响

该研究以春油菜幼苗为材料,采用土壤盆栽试验,设7个不同施硫(0、35、70、105、140、175、210mg·kg^-1)处理,通过测定春油菜幼苗的株高、植株鲜重、叶绿素含量、MDA含量、SOD、POD、CAT活性、土壤全氮含量、pH、蔗糖酶、过氧化氢酶和脲酶活性指标,分析不同施硫量对春油菜幼苗生理生化指标和土壤相关酶活性的影响。结果表明:在春油菜苗期施用硫肥对幼苗的农艺性状、生理生化指标和土壤酶活性均产生了一定影响。施硫量在35~105mg·kg^-1范围时,对植株鲜重有明显的促进作用;施硫量在70~105mg·kg^-1范围时,类胡萝卜素含量达到最高;施硫量在70~105mg·kg^-1范围时,叶片中POD和CAT的活性明显升高,而MDA含量明显下降;经相关分析,MDA含量与POD活性呈极显著负相关(r=-0.92,P<0.01),与CAT活性呈显著负相关(r=-0.72,P<0.05),说明叶片MDA含量受POD和CAT活性变化的影响;施硫量高于105mg·kg^-1时,土壤脲酶和蔗糖酶活性受到抑制;施硫量高于140mg·kg^-1时,土壤过氧化氢酶活性受到抑制;随着施硫量的增加,土壤pH值和叶片SOD活性逐渐下降;经相关性分析,土壤脲酶活性和全氮含量间呈极显著正相关(r=1,P<0.01),表明土壤全氮含量受土壤脲酶活性变化的影响。由此可知,在低硫(35~105mg·kg^-1)条件下对春油菜幼苗生理生化指标及土壤酶活性具有一定的促进作用,而在高硫(>105mg·kg^-1)条件下则产生抑制。     

长期施肥对红壤和黑土硫形态演变的影响

以红壤和黑土肥力与肥料效益监测站土壤为研究对象,研究了长期(21年)不同施肥(不施肥对照、施用氮磷钾、氮磷钾配施有机肥)处理下,表层(0～20 cm)和亚表层(20～40 cm)土壤硫素形态组成、分布及演变规律.结果表明: 长期施用化肥及化肥配施有机肥处理下,表层土壤全硫比对照分别增加42%、33%(红壤)和6%、76%(黑土);除红壤氮磷钾处理外,亚表层土壤全硫受施肥影响较小,且明显低于相应表层土壤.有效硫和盐酸可提取态硫分别为红壤和黑土中的主要无机硫形态.施用化肥及化肥配施有机肥的红壤表层有效硫比对照分别增加了447%和102%,并促进了有效硫向亚表层的迁移、累积;而施用化肥及化肥配施有机肥处理的黑土表层有效硫仅比对照分别增加54%和93%,其对亚表层土壤有效硫的影响也不大.有机硫形态在两种土壤中都以酯键硫和残渣态硫为主.长期施肥影响下的表层和亚表层土壤中残渣态硫含量比对照分别增加了32%和55%以上;土壤中性质相对活跃的酯键硫和碳键硫受施肥影响不显著,而与土壤有机碳含量呈显著正相关关系(P<0.05).此外,长期施肥试验表明大气硫沉降对土壤硫素输入的影响值得重视.     

内蒙古典型草原生态系统定位研究最新进展

中国科学院内蒙古草原生态系统定位研究站最近几年在草原生态系统多功能、草原生态系统碳循环与温室气体、气候变化对植物群落结构影响长期观测、草原生态系统退化与恢复过程、草原生态系统硫生物地球化学循环、放牧生态系统管理等领域取得较大进展。研究结果指出,农垦活动使有机碳损失34%,草原植被——土壤系统是甲烷的弱汇;20多年来,这一地区气候变化有变暖趋势,冬季增温明显,春季干旱进一步加剧,影响初级生产力生产;系统提出草原退化是草原生态系统退化,并对退化阶段进行了划分;在内蒙古冷蒿小禾草退化草原施用硫肥对提高初级生产力与羊毛性能方面有明显效果。     

Nitrogen cycling in low input legume-based agriculture,with emphasis on legume/grass pastures

Low input legume-based agriculture exists in a continuum between subsistence farming and intensive arable and pastoral systems. This review covers this range, but with most emphasis on temperate legume/grass pastures under grazing by livestock. Key determinants of nitrogen (N) flows in grazed legume/grass pastures are: inputs of N from symbiotic N₂ fixation which are constrained through self-regulation via grass/legume interactions; large quantities of N cycling through grazing animals with localised return in excreta; low direct conversion of pasture N into produce (typically 5–20%) but with N recycling under intensive grazing the farm efficiency of product N: fixed N can be up to 50%; and regulation of N flows by mineralisation/immobilisation reactions. Pastoral systems reliant solely on fixed N are capable of moderate-high production with modest N losses e.g. average denitrification and leaching losses from grazed pastures of 6 and 23 kg N ha^–1 yr^–1. Methods for improving efficiency of N cycling in legume-based cropping and legume/grass pasture systems are discussed. In legume/arable rotations, the utilisation of fixed N by crops is influenced greatly by the timing of management practices for synchrony of N supply via mineralisation and crop N uptake. In legume/grass pastures, the spatial return of excreta and the uptake of excreta N by pastures can potentially be improved through dietary manipulation and management strategies. Plant species selection and plant constituent modification also offer the potential to increase N efficiency through greater conversion into animal produce, improved N uptake from soil and manipulation of mineralisation/immobilisation/nitrification reactions.     

Long-term effect of superphosphate on accumulation of soil phosphorus and exchangeable cations on a grazed,irrigated pasture site

The annual herbage dry matter yield, herbage P concentrations and quantities of P, K, Mg and Ca cycled by grazing sheep were calculated for a 37 year-old grazed pasture supplied with superphosphate at rates of 0, 188 and 376 kg ha^-1 annually. The amount and distribution of inorganic and organic P and exchangeable K, Mg and Ca in the soil below the three grazed treatments was also measured and compared with that below a wilderness area which had not been used for agriculture. Increasing rates of superphosphate increased herbage dry matter yield, herbage P concentrations and thus the amounts of P ingested and, in turn, excreted by the grazing sheep. Annual quantities of K, Mg and Ca cycled back to the pasture in the form of excreta were also increased. The increased cycling of K by animals induced by increasing superphosphate applications resulted in greater losses of K and consequently concentrations of exchangeable and non-exchangeable ‘fixed’ K in soil decreased in the order wilderness > control > 188 > 376. Differences were evident to a depth of 20 cm. Some losses of Mg during cycling also occurred and concentrations of exchangeable Mg followed the order: wilderness > control >188=376. Concentrations of exchangeable Ca increased with pasture development due to additions of Ca in lime and superphosphate. Concentrations of total soil organic P (0–4 cm) increased in the order: wilderness < control <188<376 but for inorganic P and total P the control had a lower content than wilderness indicating losses of P during cycling in the grazed control treatment. Phosphorus fractionation suggested that with increasing superphosphate rates inorganic P primarily accumulated in a form adsorbed to Al hydrous oxides and as calcium phosphate compounds whilst organic P accumulated in both labile forms and forms associated with humic compounds. In the fertilised sites both inorganic and organic P accumulated in the soil profile to a depth of 20 cm.     

Distribution and budget of nutrients in a commercial apple orchard

Summary Data on the dry matter distribution and nutrient reserves (N, P, S, Cl, K, Ca, Mg and Na) in the standing biomass of a grassed-down 14 year-old apple orchard are presented together with mean estimates of nutrient inputs, returns and losses over a 2 year period.The major inputs of N P K and S were through fertilizer additions. The major inputs of Na and Cl were in bulk precipitation plus irrigation whilst both sources were important for Mg and Ca. Total inputs by precipitation plus irrigation plus fertilizer in kg/ha/yr were: N, 81; P, 20; S, 42; Cl, 58; K, 64; Ca, 35; Mg, 10 and Na, 33. Nutrient returns to the orchard floor were dominated by those from returns of herbage clippings orginating from the mowing of the orchard pasture. Autumn leaf fall also contributed significant quantities to the total nutrient returns. Total nutrient returns to the orchard floor through petal fall, fruit drop, leaf fall, foliar leaching (includes leaf washing) and pasture clippings in kg/ha/yr were: N, 545; P, 33; S, 41; Cl, 107; K, 442; Ca, 147; Mg, 35 and Na, 16. The major loss of Na, Mg, Ca, Cl and S was through leaching (this may include a certain amount of chemical weathering). In contrast, the major loss of P and K was in the harvested fruit crop, while for N, losses were about equally divided between the fruit crop and leaching. Total nutrient losses from the orchard by removal of the fruit crop and pruning wood plus leaching losses were estimated in kg/ha/yr at: N, 58; P, 5; S, 28; Cl, 81; K, 124; Ca, 55; Mg, 39 and Na, 80. Inputs minus losses in kg/ha/yr were positive for N, P and S(+23, +16 and +14 respectively and negative for Cl, K, Ca, Mg and Na (–24, –60, –19, –30 and –47 respectively).     

Nitrogen relationships in intensively managed temperate grasslands

Summary Most studies of N relationships in grassland have used cut swards. These have shown that for annual inputs of 200 to 400 kg N/ha from fertilizer or fixation, 55 to 80% of the N is recovered in harvested herbage. Generally, no more than 5 to 15% is lost through leaching and denitrification with most of the remaining N incorporated into soil organic matter. The relatively high efficiency of N use by cut swards reflects rapid uptake of N and the removal of a large part of the input in herbage. Inclusion of the grazing ruminant alters the efficiency of N use; only 5–20% of the input is recovered in meat or milk, and 75 to 90% of the N ingested is excreted, mainly as urea in urine. Application of N in urine ranges from 30–100 g/m². Too much N is voided for effective recovery by the sward whilst soils usually contain insufficient C to allow appreciable immobilization. The surfeit is lost. Hydrolysis of urea is usually complete within 24 h of urine deposition. For urine-treated pasture in New Zealand (NZ) losses by NH₃ volatilization of up to 66% of applied N are found during warm dry weather, with an average of 28% for a range of seasonal conditions. In the UK, the average rate of NH₃ loss from an intensively grazed ryegrass sward was 0.75 kg N/ha/day during a 6-month season. NH ₄ ⁺ remaining in the soil may be nitrified, nitrification being complete within 3 to 6 weeks. Although some NO ₃ ^– is recovered by plants, a substantial portion is leached and/or denitrified. On average such losses were 42%, with only 30% of the added N recovered by plants in urine-treated pasture in NZ. In the UK annual leaching of 150 to 190 kg N/ha has been observed for grazed swards receiving 420 kg N/ha/yr. Low retention of N by grazing ruminants results in a breakdown of N relationships in intensively managed grasslands. The substantial losses through NH₃ volatilization, leaching and denitrification have serious agronomic, economic and environmental implications.     

地植物多样性间的关系

用显微技术法分别在放牧率为 1 .33,4 .0 0和 6.67只 / hm2下对内蒙古细毛羊的食性进行了研究。结果表明 ,随着放牧率的增大 ,草场的植物种类组成及其相对比例发生了明显的变化。由于不同牧草的可利用性不同 ,其食性选择也发生了明显的变化。在重牧条件下 ,原先为随意采食的冷蒿和厌食的寸草苔则升级为“喜食”的植物 ,星毛委陵菜的选择性指数也有较大提高 ;且星毛委陵菜成为主要的食物资源 ,占全部食物的 80 %以上。这说明放牧率的增大和绵羊选择性的采食是草场植物种类组成发生变化的主要原因之一。食物的选择性主要与草地牧草的相对生物量、高度和频度显著相关 ;当草地植物多样性指数较高时 ,放牧绵羊的食物选择性较大。不同放牧率条件下 ,在以冷蒿和小禾草为主的退化草原上 ,草地植物多样性指数随放牧率的增大而显著降低 ,但食物多样性指数以放牧率 4 .0 0只 / hm2 的处理最高。     

Options for reducing the negative effects of nitrogen in agriculture

After addition to farms by fertilizer, crop residues, biological fixation and animal excreta, nitrogen can be lost through gaseous emission, runoff and leaching to contaminate the atmosphere and water bodies, and cause adverse health effects. The efficiency of fertilizer hitrogen can be increased and losses reduced, by matching supply with crop demand, optimizing split application schemes, changing the form to suit the conditions, and use of slow-release fertilizers and inhibitors. In addition, agronomic practices such as higher plant densities, weed and pest control and balanced fertilization with other nutrients can also increase efficiency of nitrogen use. Efficiency of use by animals can be increased by diet manipulation. Feeding dairy cattle low degradable protein and high starch diets, and grazing sheep and cattle on grasses high in water soluble carbohydrate result in less nitrogen excretion in urine and reduced ammonia volatilization.     

Options for reducing the negative effects of nitrogen in agriculture

After addition to farms by fertilizer, crop residues, biological fixation and animal excreta, nitrogen can be lost through gaseous emission, runoff and leaching to contaminate the atmosphere and water bodies, and cause adverse health effects. The efficiency of fertilizer nitrogen can be increased and losses reduced, by matching supply with crop demand, optimizing split application schemes, changing the form to suit the conditions, and use of slow-release fertilizers and inhibitors. In addition, agronomic practices such as higher plant densities, weed and pest control and balanced fertilization with other nutrients can also increase efficiency of nitrogen use. Efficiency of use by animals can be increased by diet manipulation. Feeding dairy cattle low degradable protein and high starch diets, and grazing sheep and cattle on grasses high in water soluble carbohydrate result in less nitrogen excretion in urine and reduced ammonia volatilization.     

Options for reducing the negative effects of nitrogen in agriculture

After addition to farms by fertilizer, crop residues, biological fixation and animal excreta, nitrogen can be lost through gaseous emission, runoff and leaching to contaminate the atmosphere and water bodies, and cause adverse health effects. The efficiency of fertilizer nitrogen can be increased and losses reduced, by matching supply with crop demand, optimizing split application schemes, changing the form to suit the conditions, and use of slow-release fertilizers and inhibitors. In addition, agronomic practices such as higher plant densities, weed and pest control and balanced fertilization with other nutrients can also increase efficiency of nitrogen use. Efficiency of use by animals can be increased by diet manipulation. Feeding dairy cattle low degradable protein and high starch diets, and grazing sheep and cattle on grasses high in water soluble carbohydrate result in less nitrogen excretion in urine and reduced ammonia volatilization.     

Herbage intake,methane emissions and animal performance of steers grazing dwarf elephant grass v. dwarf elephant grass and peanut pastures

Management strategies for increasing ruminant legume consumption and mitigating methane emissions from tropical livestock production systems require further study. The aim of this work was to evaluate the herbage intake, animal performance and enteric methane emissions of cattle grazing dwarf elephant grass (DEG) (Pennisetum purpureum cv. BRS Kurumi) alone or DEG with peanut (Arachis pintoi cv. Amarillo). The experimental treatments were the following: DEG pastures receiving nitrogen fertilization (150 kg N/ha as ammonium nitrate) and DEG intercropped with peanut plus an adjacent area of peanut that was accessible to grazing animals for 5 h/day (from 0700 to 1200 h). The animals grazing legume pastures showed greater average daily gain and herbage intake, and shorter morning and total grazing times. Daily methane emissions were greater from the animals grazing legume pastures, whereas methane emissions per unit of herbage intake did not differ between treatments. Allowing animals access to an exclusive area of legumes in a tropical grass-pasture-based system can improve animal performance without increasing methane production per kg of dry matter intake.     

控释尿素减施对双季稻田氮素渗漏淋失的影响

大量施用氮肥引起的土壤氮素淋失是稻田氮素损失的一个重要途径.为探究自然降雨过程中典型双季稻田氮渗漏淋失特点,采用田间渗漏池法,通过大田小区试验,研究控释尿素减施对稻田土壤60 cm深处渗漏水中氮淋失和水稻产量的影响.结果表明: 施肥初期出现氮渗漏淋失峰值,这是防控的关键时期;双季稻生长季控释尿素减氮20%(0.8CRU)和减氮30%(0.7CRU)处理全氮淋失量分别为42.3和37.7 kg·hm^-2,均显著低于常规尿素(CU)处理(53.9 kg·hm^-2),且0.7CRU处理显著低于等氮量控释尿素(1.0CRU)处理(51.3 kg·hm^-2);各施氮处理全氮渗漏淋失率为11.9%～13.5%,处理间差异不显著.0.8CRU和0.7CRU处理较CU处理明显提高了水稻产量和氮肥吸收利用率,显著增加了氮收获指数.总之,控释尿素减氮 20%～30%能保证水稻产量和防控稻田氮渗漏淋失.