半干旱黄土区苜蓿草地轮作农田土壤氮、磷和有机质变化

大田试验研究了多年生苜蓿草地轮作农田2年内的耕层土壤氮、磷养分和有机质变化.结果表明,与苜蓿连作相比,苜蓿草地轮作成农田后,土壤N和有机质消耗增加,2年中耕层土壤全氮含量平均分别下降了5.4%和19.5%、有机质下降了46.8%和28.2%,土壤全磷无显著变化;轮作提高了土壤氮、磷养分有效性及其活化率,土壤硝态氮含量2年分别提高了15.5%和159.1%、速效磷含量提高了44.5%和48.0%,差异显著.不同轮作方式对土壤养分变化有显著影响.苜蓿草地轮作后第2年,种植春小麦与种植玉米相比差异显著,种植马铃薯和休闲处理土壤养分变化幅度处于二者之间.种植春小麦能够维持农田土壤肥力生长季平衡,种植玉米增加了对土壤全氮、有机质和速效磷的消耗,土壤养分含量出现季节性下降,C/N和C/P降低.在半干旱地区多年生苜蓿草地向农田转变过程中,以轮作春小麦为宜,应避免种植玉米作物,以维持农田肥力平衡.     

干旱区内陆河流域尾闾绿洲土壤盐渍化动态预测

针对干旱区尾闾绿洲土壤盐渍化严重发生的现状,运用遥感和GIS技术,基于天山北麓三工河流域平原尾闾绿洲农区0~20 cm耕作层土壤盐渍化特征,利用空间概率模型预测了其今后的发生状态。结果表明:经过长时间的土地利用,土壤盐渍化程度有所加剧;通过空间概率模型χ~2检验,1982—2005年的转移概率模拟值与实际值可靠性要高于1982—1999年的转移概率。模型模拟结果显示,2010年以后到达稳定状态,人工景观的面积增加,自然景观的面积减少,其中轻盐化耕地面积减少,中盐化和重盐化耕地面积增加,在长时间范围内,土壤盐渍化依旧是制约研究区绿洲耕地生产力的主要因素。     

民勤绿洲边缘沙丘生物土壤结皮发育对浅层土壤质地、养分含量及微生物数量的影响

为探明干旱沙区沙丘生物土壤结皮形成及发育对浅层土壤质地、养分含量及微生物数量的影响,以民勤绿洲边缘结皮前期阶段(NCS)、物理-藻类结皮阶段(PACS)、藻类-地衣结皮阶段(ALCS)以及地衣-藓类结皮阶段(LMCS)的0—1 cm层土壤为研究对象,研究了土壤颗粒组成、土壤有机质、全氮、速效磷、速效钾含量以及土壤微生物数量动态变化。结果表明:1)生物土壤结皮在NCS向ALCS的发育过程中,其有效地提高了0—1 cm层土壤细沙粒(0—200μm)含量,同时降低了粗砂粒(200—2000μm)含量;在ALCS向LMCS演替过程中,土壤粒度组成无明显变化。2)土壤结皮形成与发育对0—1 cm层土壤有机质、全氮、速效磷以及速效钾含量均有显著影响(P0.05),4种养分含量均随生物结皮演替逐渐增大。3)在土壤结皮形成与演替过程中,0—1 cm层土壤细菌、放线菌以及真菌数量均呈现出先增大后减小趋势(峰值均出现在PACS),土壤总藻生物量一直处于持续增大趋势;在5—12月期间,土壤微生物数量或生物量变化均呈现出先增大后减小趋势。4)土壤结皮在NCS向PACS演替过程中,土壤颗粒组成的改变是土壤微生物量及养分变化的主要驱动因子;PACS向LMCS演替过程,土壤藻类、地衣、藓类是提高土壤养分含量的主要因子。表明民勤绿洲边缘沙丘生物土壤结皮形成与发育能有效地改善浅层土壤质量,提高土壤肥力,同时对土壤生态系统改善及生态环境保护具有重要作用。     

艾比湖流域小尺度农田土壤养分的空间分布和盐渍化风险评价

为了解绿洲经济迅速发展背景下新疆典型尾闾绿洲-艾比湖流域小尺度农田土壤的养分和盐渍化状况,对该地区典型农田土壤中有机质、碱解氮、速效磷和速效钾等养分元素的空间分布、影响因素以及盐渍化风险状况进行了评价。结果表明:(1)农田土壤中有机质、碱解氮、速效磷和速效钾的含量均较高。所有土壤样点中总盐分含量属于高度变异,其他指标属于低度变异。(2)半方差函数分析表明土壤中碱解氮、速效磷和速效钾含量的空间变异性主要受施肥和灌溉等随机性因素的影响;而有机质和总盐分含量的空间变异性则受植被覆盖和土壤质地等结构性因素以及施肥、灌溉等随机性因素的共同影响。(3)空间分析表明,总体看农田土壤中有机质、碱解氮、速效磷和速效钾含量较高区域主要分布在中部和北部,受施肥、灌溉方式和植被盖度等因素的影响;而盐分含量较高区域主要分布在研究区南部和边缘区域,主要受地形、土壤质地和植被盖度的影响。(4)相关分析表明农田土壤中有机质、速效钾、速效磷、碱解氮和总盐分含量呈显著的负相关关系。盐渍化风险评估表明土壤中总盐分含量属于低度到中度的盐渍化风险,不会对主要作物棉花的生长产生危害,但应改进灌溉方式和种植制度,同时采用增施有机肥、进行秸秆还田等措施促进棉花作物的稳产、高产。     

黑河中游荒漠绿洲区土地利用的土壤养分效应

土地利用影响地表覆被状况和生态过程,关系到土壤肥力与土壤碳库功能"源-汇"关系的改变。黑河中游甘州区和临泽县是我国西北干旱区典型的荒漠绿洲区,以土壤表层(0-20 cm)养分变化为对象,利用2011-2012年甘州区和临泽县的土壤野外调查数据和该区全国第二次土壤普查数据,对两时期土壤表层养分(土壤有机质、全氮、全磷、全钾及pH值)的变化特征进行比较研究。结果表明:研究区土壤有机质、全磷含量分别降低了3.54%和12.5%;而全氮、全钾和pH值分别增加了74.4%、98.2%和4.9%。全国第二次土壤普查时期,荒漠、耕地与草地三者在各土壤养分上没有显著差异,但林地在土壤有机质、全氮、全钾上显著高于前三者。2011-2012年,耕地土壤的全磷、全氮与其它土地利用存在显著差异。土地利用的保持和改变对土壤养分变化有着重要影响,耕地的长期耕作使得土壤有机质含量降低4.94%,全氮增加86.93%,全磷减少5.02%,土壤碱性增强;荒漠植被的自然演替使土壤有机质含量增加66.21%,全氮增加71.70%,全磷含量减少37.33%,土壤碱性变弱。所以,耕地扩张及其长期耕作活动将导致地力退化并有盐碱化风险,而荒漠等自然生态系统保护有利于土壤肥力的改善和土壤固碳功能的发挥。     

玉米/花生间作对土壤微生物和土壤养分状况的影响

通过大田试验,研究了玉米/花生间作对玉米和花生根区土壤微生物和土壤养分状况的影响.结果表明：与单作相比,间作能显著提高玉米和花生根区的土壤细菌数量;间作花生根区土壤真菌和放线菌数量与单作无显著差异;间作玉米根区土壤真菌和放线菌数量比单作明显提高;间作作物根区微生物群落功能多样性和代谢活性比单作有所改善.玉米/花生间作不同程度提高了整个间作系统根区的土壤碱解氮、速效磷、有机质含量及EC值,其中,间作玉米根区土壤养分的增加更为明显,说明玉米/花生间作可以较明显地改善两种作物根区的微生物和养分状况,土壤微生态环境的改善又会促进作物地上部的生长.     

干旱区绿洲农田不同种植模式和秸秆管理下土壤质量评价

研究干旱区绿洲农田不同种植模式和秸秆管理下土壤有机碳及其酶活性的变化,揭示农业管理措施对土壤质量的影响,以期为干旱区农业资源高效利用及可持续发展提供理论依据.在作物种植规划区,选择新疆主要农作物棉花、小麦、玉米,设计长期连作及轮作试验.结果表明:轮作处理土壤有机碳(SOC)、微生物生物量碳、易氧化有机碳、水溶性有机碳、热水溶性有机碳含量较连作处理分别提高了3.6%~9.9%、41.8%~98.9%、3.3%~17.0%、11.1%~32.4%、4.6%~27.5%;秸秆还田处理较秸秆不还田处理分别提高了12%~35.9%、22.4%~49.7%、30.7%~51.0%、10.6%~31.9%、41.0%~96.4%.轮作处理土壤过氧化氢酶、脱氢酶、β-葡萄糖核苷酶、蔗糖酶、纤维素酶活性较连作处理分别提高了6.4%~10.9%、6.6%~18.8%、5.9%~15.3%、10.0%~27.4%、28.1%~37.5%;秸秆还田处理较-秸秆不还田处理分别提高了31.4%~47.5%、19.9%~46.6%、13.8%~20.7%、19.8%~55.6%、54.1%~70.9%.相关性分析表明,SOC及其活性组分与土壤酶活性之间有极显著的正相关关系,利用土壤活性有机碳组分和酶活性变化可有效表征农田SOC和土壤质量变化.通过因子分析综合评价得知,在干旱区农业生产中,短期连作棉花兼实施秸秆还田可提高SOC及其活性组分含量和酶活性,合理轮作可有效缓解连作障碍,使土壤质量得到进一步改善,有利于农田土壤的可持续利用.     

额济纳绿洲土壤养分的空间异质性

利用地统计学方法研究了额济纳绿洲土壤有机质、全氮、全磷、全钾的空间异质性.结果表明:土壤养分含量分布均有较大的空间异质性,土壤有机质的理论模型为指数模型,全氮、全磷和全钾的理论模型均为球状模型;额济纳绿洲土壤有机质、全氮、全钾主要受结构性因子的影响,全磷受结构性因子和随机因子的共同影响;全氮、全磷和全钾的变程在7.68～7.86 km,土壤有机质的变程较小,为5.4 km.土壤养分的空间分布表现为南北高,中间低的分布格局.     

塔克拉玛干沙漠南缘荒漠绿洲过渡带不同土地利用影响下土壤化学计量特征

荒漠绿洲过渡带在维护绿洲生态安全和绿洲稳定上具有重要作用。垦荒等土地利用的增强使得荒漠绿洲过渡带的健康稳定受到了巨大的挑战。以塔克拉玛干沙漠南缘典型荒漠绿洲过渡带为研究对象,系统分析了不同土地利用方式(桑田、半自然柽柳林、瓜地、棉花-玉米地)对土壤养分化学计量特征的影响。土壤取样沿农田到荒漠方向进行,分5层进行。研究发现,土壤各养分指标均受土地利用方式(4种)、土层(5层)和与农田边缘垂直距离(4梯度)的显著影响,且存在一定的交互作用。土地利用方式显著影响土壤各养分元素含量。随土层由浅到深,有机碳(C)、有效氮(N)和有效磷(P)基本呈下降趋势,全N具有波动变化,而全P变化不显著。随与农田边缘垂直距离的增加,各养分含量基本呈递减趋势。对同一土层(共选择三层)不同土地利用方式下土壤养分具体分析表明,棉花-玉米地这一利用方式在农田内部具有最高的土壤有机C和全N含量,其次为桑田。随着与农田边缘垂直距离的增加,土壤C、N含量优势减弱。除农田内部样地(0 m)外,三层土壤全P含量基本呈桑田柽柳林棉花-玉米地趋势。表层有效N含量在农田内部样地(0 m)瓜地最高,其他距离处(大于等于20 m)棉花-玉米地高,下层土壤有效氮含量在农田内部各土地利用方式间无差异。在各距离样点处不同土地利用类型间土壤有效P含量的变化无明显规律,在农田内部以瓜地有效P含量最高。棉花-玉米地土壤全量N/P在农田内部和与农田边缘垂直距离20 m处含量最高。三土层土壤有效N/P在农田内部以柽柳林最高,随着与农田边缘垂直距离增加,土壤有效N/P显著改变。综合来看,土地利用对荒漠绿洲过渡带土壤营养含量的增加具有正向作用,由土壤养分变化带来的生态效应值得关注。     

干旱区农田不同利用强度下土壤质量评价

基于2005—2007年典型干旱区塔里木盆地南缘的策勒绿洲的试验数据,根据当地农民的耕作习惯选择4种典型的农田利用强度（高投入农田、常规投入农田、新垦农田和绿洲内部农户农田）,利用产量可持续性指数(SYI)、土壤改良指数(SI)和土壤综合质量指数(QI)分析了不同土地利用强度下农田土壤质量的变化情况.结果表明：各样地的土壤有机质（SOM）、碱解氮（AN）和速效磷（AP）含量均存在显著差别;位于绿洲边缘的新垦农田在所有评价中均处于最低水平,而绿洲内部农田则处于相对较高水平.本研究结果不但有利于当地农田的合理开发利用,同时有利于农田生态环境的保护.     

气候变化对甘肃省粮食生产的影响研究进展

甘肃省气候自1986年起向整体暖干化、局部暖湿化转型突变.与1960年相比,转型后2010年平均气温升高了1.1 ℃,平均降水量减少了28 mm,干旱半干旱区南移约50 km.气候变暖使甘肃省主要作物生育期有效积温增加,生长期延长,熟性、布局和种植制度改变,宜种区和种植海拔增加,多熟制北移,夏粮面积缩小,秋粮面积增大.弱冬性、中晚熟品种逐步取代强冬性、中早熟品种,有利于提高光温利用率,增加产量.暖湿型气候增加了绿洲灌区作物的气候生产力,暖干型气候降低了雨养农业区的气候产量,水分和肥力条件是决定因素.以提高有限降水利用率和利用效率、改善和提升土壤质量及肥力为核心,选育强抗逆、弱冬性、中晚熟、高水分利用效率的作物新品种,建立适温、适水的种植结构和种植制度,是甘肃省应对气候变化进行粮食生产的主要发展方向.     

塔里木河上游典型绿洲不同连作年限棉田土壤质量评价

开展农业生态系统土壤质量评价是保证生态农业持续高效发展的重要内容。以塔里木河上游阿拉尔垦区为典型样区,选择0a、3a、8a、12a、20a、30a等不同连作年限棉田为研究对象,综合考虑土壤物理、化学和生物学性质,分析了12个土壤理化及酶活性指标;基于因子分析和聚类分析法评价棉田间土壤质量的差异并划分等级,利用产量持续指数验证评价结果。研究表明：不同连作年限的棉田土壤的理化性质和酶活性均存在一定差异;棉田的土壤质量随年限呈先上升后下降的趋势,8a、12a棉田土壤质量相对较高,20a、30a土壤质量有退化趋势;土壤质量评价值与产量持续指数变化趋势一致,后者略显滞后效应。     

Winter oilseed production for biofuel in the US Corn Belt: opportunities and limitations

Interest from the US commercial aviation industry and commitments established by the US Navy and Air Force to use renewable fuels has spurred interest in identifying and developing crops for renewable aviation fuel. Concern regarding greenhouse gas emissions associated with land‐use change and shifting land grown for food to feedstock production for fuel has encouraged the concept of intensifying current prominent cropping systems through various double cropping strategies. Camelina (Camelina sativa L.) and field pennycress (Thlaspi arvense L.) are two winter oilseed crops that could potentially be integrated into the corn (Zea mays L.)–soybean [(Glycine max (L.) Merr.] cropping system, which is the prominent cropping system in the US Corn Belt. In addition to providing a feedstock for renewable aviation fuel production, integrating these crops into corn–soybean cropping systems could also potentially provide a range of ecosystem services. Some of these include soil protection from wind and water erosion, soil organic C (SOC) sequestration, water quality improvement through nitrate reduction, and a food source for pollinators. However, integration of these crops into corn–soybean cropping systems also carries possible limitations, such as potential yield reductions of the subsequent soybean crop. This review identifies and discusses some of the key benefits and constraints of integrating camelina or field pennycress into corn–soybean cropping systems and identifies generalized areas for potential adoption in the US Corn Belt.     

干旱区城郊种植业水足迹分析与适宜耕地规模测算——以乌鲁木齐市为例

水足迹方法能够完整、清晰地描述种植业的耗水特征。以干旱区绿洲城市乌鲁木齐市为例,运用水足迹模型分析种植业产品耗水特征,构建水足迹强度系数以探讨种植业耗水对本地水资源的影响度,进而从作物水足迹和水源类型角度建立绿洲耕地规模测度模型测算乌鲁木齐市适宜耕地规模,研究发现:①作物生长期水足迹受土壤水分胁迫和产量损减影响呈现差异化;②2005-2011年间,绿水强度系数波动剧烈,蓝水强度系数均值超出容量极限,作物生长期对蓝水资源依赖性较强,从而进一步加剧了蓝水资源的匮乏;③乌鲁木齐市合理耕地规模约为6万hm²,2005-2011年种植业实际耕地规模均处于超载状态,超载量变化呈现先降后升的特征,现状种植业发展模式对绿洲生态系统扰动不断加剧。     

Main interspecific competition and land productivity of fruit-crop intercropping in Loess Region of West Shauxi

Taking the four typical fruit-crop intercropping models, i.e., walnut-peanut, walnut-soybean, apple-peanut, and apple-soybean, in the Loess Region of western Shanxi Province as the objects, this paper analyzed the crop (peanut and soybean) photosynthetic active radiation (PAR), net photosynthetic rate (P(n)), yield, and soil moisture content. Comparing with crop monoculture, fruit-crop intercropping decreased the crop PAR and P(n). The smaller the distance from tree rows, the smaller the crop PAR and P(n). There was a significantly positive correlation between the P(n) and crop yield, suggesting that illumination was one of the key factors affecting crop yield. From the whole trend, the 0-100 cm soil moisture content had no significant differences between walnut-crop intercropping systems and corresponding monoculture cropping systems, but had significant differences between apple-crop intercropping systems and corresponding monoculture cropping systems, indicating that the competition for soil moisture was more intense in apple-crop intercropping systems than in walnut-crop intercropping systems. Comparing with monoculture, fruit-crop intercropping increased the land use efficiency and economic benefit averagely by 70% and 14%, respectively, and walnut-crop intercropping was much better than apple-crop intercropping. To increase the crop yield in fruit-crop intercropping systems, the following strategies should be taken: strengthening the management of irrigation and fertilization, increasing the distances or setting root barriers between crop and tree rows, regularly and properly pruning, and planting shade-tolerant crops in intercropping.     

Soil mercury accumulation and transference to different crop grains

Mercury contamination in agro-ecosystems is one of the most important environmental issues. Farmland soil mercury accumulation and transference to crops in Changshu City, eastern China, were investigated to identify mercury migration capacity from soil to crops. The mean content of mercury for soil samples slightly increased year after year. The mercury accumulation capacity of rice grown (bioaccumulation factor (BAF) 0.028) in submerged soils under reductive conditions was stronger than that of wheat (BAF 0.0073) in dried soils under oxidative conditions. There were clear relationships between soil mercury with organic matter (OM), cation exchange capacity (CEC), and CaCO₃ of soil samples, while apparent negative relationships between Hg in rice grain with OM, CEC, and CaCO₃ of soil existed. No clear association for Hg between crops and soil was found, indicating that mercury in crop grains is mostly affected by other factors besides soil mercury. Also, soil properties and farming patterns affected mercury transference from soil to crop grains and mercury enrichment capacity in crop grains. The results suggested that appropriate selection of crop species and water management are two major possible ways to reduce total mercury accumulation in crop grains grown in mercury-contaminated regions.     

Effects of agricultural cropping systems on micronutrients transformation

Summary The effect of cropping systems of wheat-maize (WM), wheat-rice (WR), wheat-groundnut (WG), gram-bajra (GrB), potato-guara (PGu), and raya-mash (RaMa) in combination with treatments of dummy (uncultivated area) and applied Zn 0.0 (Zn₀), 2.8 (Zn₁), 5.6 (Zn₂) 11.2 (Zn₃) kg/ha was studied on the transformation of labile Zn fractions: exchangeable (Exch.), adsorbed (TAd) [weakly (WAd), moderately (MAd), strongly (SAd)], and organic matter (OM) in different layers of sandy loam soil. The added Zn stayed largely in the 0–30 cm layer and was associated with the WAd- and OM-Zn fractions. About 70% of the total labile Zn (PAv) remained in the WAd- and OM-Zn, that is, 33 and 39% in 0–15 cm layer, and 33–39% and 31–36% in 16–150 cm layer. All the Zn fractions in 0–15 cm layer, and only of WAd in 16–30 cm layer, significantly increased with rates of Zn addition. These were also significantly higher in Zn_1–3 than Zn₀ and dummy treatments because of the residual Zn. Diverse effects of cropping systems on soil properties, residual Zn, and labile Zn fractions were found. The influence was strong in 0–15 cm layer decreasing gradually with soil depth due largely to differences in Zn requirement, crop intake of various Zn fractions and the cultural practices of the systems. All the crops and rotations appreciabilly responded to Zn application. Uptake of Zn by crops markedly and successively increased with increasing rates of Zn application. The WR caused a significant increase in soil organic matter whereas WR and WM in CaCO₃. The WR, WM and GrB resulted in a decrease in pH while WG and GrB in CaCO₃. The RaMa and PGu maintained much higher residual Zn than other systems. The systems which caused the maximum decrease in Zn fractions were: cereal-cereal (WM) in Exch. legume-millet (GrB) in all the adsorbed, PAv and the Zn associated with CaCO₃, vegetable-legume (PGu) also in MAd and SAd; and cereal-legume (WG) in OM and PAv. Hence GrB, WG and WM in that order will cause the deficiency of Zn much earlier than the other systems due to greater use and or transformation of WAd- andOM-Zn. Such effects were least under RaMa because it increased the WAd-, MAd- and OM-Zn.     

Plant-Soil-Contaminant Specificity Affects Phytoremediation of Organic Contaminants

The objective of this study was the evaluation of seven forage and conservation crop species for phytoremediation of trinitrotoluene (TNT) and pyrene-contaminated soils. TNT and pyrene were added to soil at 100 mg kg^-1. Crop species screening studies were conducted in a greenhouse and growth chambers on two soil types with different organic matter contents. Under high soil organic matter conditions, adsorption or covalent binding to the soil organic matter appeared to be a dominant force of removal limiting TNT and pyrene availability. In both soil types, pyrene dissipation could not be attributed to the presence of plants. However, in soils with lower organic matter content, all of the plant species treatments showed a significantly higher degree of TNT transformation compared with the unplanted control. Statistically significant differences in TNT transformation were observed among crop species grown in the low OM soil. Reed canary grass (Phalaris arundinacea L.) and switchgrass (Panicum virgatum L.) were the most effective species in enhancing TNT transformation. Our data indicated that use of plants was effective for phytoremediation of TNT-contaminated low OM content soils, but did not have any significant effect on pyrene dissipation. Based on these observations, it appears that plant-soil-contaminant interactions are very specific, and this specificity determines the effectiveness of phytoremediation schemes.     

东北三江平原覆盖作物种植效果

以土壤紧实度、冬前生物量、根系性状、植株氮累积量等为指标对供试12种覆盖作物(豆科:紫花苜蓿、光叶苕子、毛叶苕子、红三叶、白三叶、箭筈豌豆;非豆科:苏丹草、青萝卜、Nitro radish、甘蓝型油菜、羽衣甘蓝、菊苣)在东北三江平原地区的种植效果及应用潜力进行综合评价。结果表明: 12种覆盖作物在试验播期均能正常生长,不同覆盖作物与对照相比均有利于降低土壤紧实度,其中青萝卜、Nitro radish和苏丹草土壤紧实度下降最显著,分别较对照下降了47.1%、43.4%和33.4%;覆盖作物群体冬前鲜生物量为3.38～13.98 kg·m^-2,干生物量为0.78～2.43 kg·m^-2,非豆科覆盖作物的生物量显著高于豆科覆盖作物;覆盖作物的群体根系体积以萝卜、油菜、菊苣较大,尤其Nitro radish的根体积高达4018.5 cm³·m^-2,苏丹草的根系横向延展范围最宽;豆科覆盖作物的灰分含量显著低于非豆科覆盖作物,能提供更多易分解的有机物质;覆盖作物总氮积累量为18.72～53.09 g·m^-2,其中,羽衣甘蓝和菊苣的氮积累量最高,且生物量相对较大,有利于氮的积累和固定。在三江平原地区根据主栽作物的类型与冠层结构,选择豆科的三叶草、苕子、紫花苜蓿和非豆科的萝卜、羽衣甘蓝、苏丹草作为覆盖作物进行行间或行内混播的种植方式,可以在调控土壤结构的同时促进养分循环,有利于三江平原黑土地力的提升。