为研究不同有机肥连续施用对土壤质量的影响,综述国内外不同有机肥连续施用对农田土壤理化性质、土壤微生物以及土壤重金属的影响及作用机理,并对有机肥合理利用提出建议。研究表明：连续施用有机肥能显著改善土壤结构,提高土壤的水肥调控能力,增加土壤养分的有效性,平衡土壤养分,提高土壤酸碱缓冲性能,优化土壤微生物群落的结构和功能;但长期施用有机肥会增加土壤和植物中重金属累积风险,特别是畜禽和污泥有机肥。国内外研究大部分是粪肥与污泥和化肥的配施对土壤和作物中重金属含量进行分析,对研究畜禽粪污施用年限以及有机肥长期施用下土壤中重金属的演变特征及机理探讨相对较少,今后还需加深有机肥连续施用对土壤重金属影响机理方面的研究。

施用有机肥是农业生产的重要措施,对绿色农业发展起到积极作用,而且越来越广泛施用。本文介绍了目前有机肥基本概况,重点综述了有机肥对提高土壤肥力、提高作物产量和品质、促进养分利用以及对病虫害发生影响等方面研究的最新进展,分析了当前有机肥施用对耕地质量和农产品安全风险、施肥效率低、以及有机肥品种研发不足、相关质量标准滞后等问题,并对当前有机肥推广应用的形势和发展前景进行了分析和展望。

通过盆栽试验研究了秸秆生物有机肥的施用对土壤供氮能力的影响.结果表明,与原始秸秆相比,秸秆生物有机肥与尿素配合施用能明显提高土壤生物量碳、氮的含量,增幅约为3～4倍;土壤微生物量氮与土壤的供氮能力关系非常密切,前期发生强烈的微生物增殖过程,则中后期必会发生无机氮释放过程.这对作物的生长发育极为重要,同时提高了肥料氮利用率,揭示了秸秆生物有机肥配施无机氮肥改善土壤供氮能力的机理.

旱地农业分布面积广、增产潜力大,在保障我国粮食安全方面占有重要地位,但也面临着水资源短缺、土壤贫瘠、水土流失严重和不可再生资源利用效率低等问题。绿肥不仅具有提高土壤质量、调节土壤养分和增强土壤水分蓄纳能力,从而改善作物生长环境,促进作物持续高产稳产的作用,而且在增加农田生态系统生物多样性、提高地表覆盖度、减少养分向环境中的无效损失、增强农田系统气体调节功能、提高病虫草害的生物防控等方面也具有显著的生态效益。在全球气候变化加剧、生态环境恶化和农产品需求改变等新形势下,以肥用为主要目的的传统绿肥种植应用技术已不能满足当前农业发展的需求,需要加强旱地绿肥种质资源的选育工作,通过研制新的适应新形势的全国绿肥区划,构建适应不同区域的绿肥种植模式,优化和研发适应现代化生产水平的耕作栽培技术,探究绿肥综合效益评价体系,为旱地农业区改善生态环境、提高经济效益,构建资源节约、生态保育型的绿肥应用模式,充分挖掘绿肥效益提供科学依据和技术支撑。

A field study was conducted for 5 yr (1993-1997) to evaluate the effects of green manure residues applied to the soil in 1993 and 1995, on wheat (Triticum aestivum L.) yields and N nutrition as subsequent crop in 1994, 1996 and 1997. The effect of green manure application was also evaluated on soil microbial activity (CO2), on C and N contents of whole soil and on labile (LF) and heavy fractions (HF) of organic matter (OM). The experiment was initiated on a Le Bras silt loam (Humic Gleysol). The green manures, as a main factor, were clover (Trifolium pratense L.), buckwheat (Fagapyrum esculentum L.), millet (Echinicloa crus galli L.), mustard (Brassica hirta Moench), and colza (Brassica campestris L.), and there was a control without green manure. The sub-factors consisted of four N fertilizer rates for wheat in the subsequent years at 0, 30, 60 and 90 kg N ha–1. Broadcast application of 15N- labelled NH4NO3 was made in 90 kg N ha–1 fertilizer treatments. Two green manure applications did not influence the C and N contents of densimetric fractions of OM (LF and HF), but significantly increased those of whole soil, and microbial respiration (CO2). Green manures significantly increased wheat yields and N uptake in 1994 and 1996. Levels of N derived from fertilizer (Ndff) were lower in all green manure treatments as compared to the control, which indicates that the proportion of N derived from soil and green manures (% Ndfs) was higher in these treatments. The contribution of N from green manure varied in the following order: buckwheat < clover < mustard < millet < colza. With the exception of the clover treatment (< 100%), the N recoveries from the other green manure N (NRGM) ranged from 23 to 34% and from 19 to 36% for 1994 and 1996, respectively. Green manure application provided 15 to 24 kg N ha–1 in 1994 and from 16 to 36 kg N ha–1 in 1996 and this contribution accounted for 25 to 31% of the total wheat N uptake. Significant green manure effects on wheat yield and N nutrition were primarily due to the improvement of soil properties and to high N recoveries from the green manure. In the cold temperate climate of Québec, green manure incorporation into soil in late summer or early fall of the preceding year allowed N synchronization with wheat N needs in subsequent cropping seasons. Nitrogen fertilizer rates could be reduced after the incorporation of green manures having high yields and N contents in the previous season. Key words: Green manure, wheat yields and N uptake, N recoveries, microbial respiration, labile and heavy fractions of OM, C and N contents

土壤干层发生机理及其生态环境效应是土壤物理学和生态学及其交叉领域的重要科学问题,也是我国黄土高原开展生态文明建设,实现可持续发展面临的重大生态环境问题之一.通过回顾土壤干层研究取得的重要进展,包括土壤干层的概念与特征,评价指标,形成原因与危害,不同尺度时空分异特征及调控对策等,针对黄土高原水资源短缺和植被退化现状,提出土壤干层研究面临的机遇和挑战,包括建立统一的土壤干层动力学量化指标,干层内土壤水分对植物生长的有效性,土壤干层强度对土壤--植被--大气传输体(SVATs)中水分运移的影响,土壤干层发生发展过程和时空演变规律,土壤干层预测模型及其调控机制.此外,土壤干层的研究应结合当前植被恢复与生态文明建设的国家需求.在气候变化和剧烈人类活动背景下,开展黄土高原土壤干燥化与土壤水资源影响及其调控对策研究,将是水科学与生态学领域长期面临的科学问题之一.

Climate change scenarios forecast increased aridity in large areas worldwide with potentially important effects on nutrient availability and plant growth. Plant nitrogen and phosphorus concentrations (plant [N] and [P]) have been used to assess nutrient limitation, but a comprehensive understanding of drought stress on plant [N] and [P] remains elusive. We conducted a meta-analysis to examine responses of plant [N] and [P] to drought manipulation treatments and duration of drought stress. Drought stress showed negative effects on plant [N] (-3.73%) and plant [P] (-9.18%), and a positive effect on plant N:P (+ 6.98%). Drought stress had stronger negative effects on plant [N] and [P] in the short term (< 90 d) than in the long term (> 90 d). Drought treatments that included drying-rewetting cycles showed no effect on plant [N] and [P], while constant, prolonged, or intermittent drought stress had a negative effect on plant [P]. Our results suggest that negative effects on plant [N] and [P] are alleviated with extended duration of drought treatments and with drying-rewetting cycles. Availability of water, rather than of N and P, may be the main driver for reduced plant growth with increased long-term drought stress.© 2014 The Authors. New Phytologist © 2014 New Phytologist Trust.

土壤微生物在维持陆地生态系统服务中扮演着重要的角色.土壤水分条件是影响微生物活性与生态系统功能的重要因素之一,全球气候变化所引起的极端干旱与降雨必将加速土壤水分的剧烈变化.由于不同土壤微生物对干旱胁迫的耐受性不同及其对水分变化的响应差异,使得土壤水分条件变化直接改变了土壤微生物活性与群落结构,进而对微生物介导的关键过程与土壤生态系统功能造成深刻的影响.因此,全面深入地理解水分条件变化下土壤微生物群落的结构变化特征与响应机制具有重要意义.本文在总结土壤水分条件变化对土壤微生物活性(土壤呼吸与酶活性)和微生物群落结构的影响的基础上,进一步阐述了土壤微生物对干旱胁迫与水分条件变化的响应机制和生态学策略,包括: 1)积累胞内溶质、产生胞外聚合物、进入休眠状态等应对干旱胁迫的细胞生理策略;2)微生物之间、微生物与植物之间相关抗逆性基因的转移及土壤微生物群落的功能冗余等应对水分变化的微生物机制.研究水分条件变化下土壤微生物群落结构及生态系统功能之间的内在联系,不仅有助于进一步剖析微生物介导的土壤生态过程,而且能够为今后陆地生态系统对气候变化的响应研究和模型预测提供理论依据.