水分胁迫对紫花苜蓿根系吸水与光合特性的影响

变水条件下(利用PEG-6000模拟水分胁迫48 h,ψs=0.2MPa,之后复水48 h),测定紫花苜蓿(Medicago sattva L,品种阿尔冈金和陇东苜蓿)幼苗根系水力学导度与光合参数变化规律,旨在研究变水条件下紫花苜蓿光合作用的响应机制、植株水分吸收能力的变化规律及地上与地下部可能的相关关系.结果表明:干旱胁迫使得紫花苜蓿根系水力学导度(Lpr)受到显著影响.随着水分胁迫时间的延长,根系吸水能力呈现快速--缓慢下降趋势,即根系水力学导度逐渐下降,气孔导度(Gs)、蒸腾速率(Tr)、净光合速率(Pn)和叶片水势亦随之而显著降低,胞间二氧化碳浓度(Ci)先随之降低但最终上升而累积.复水后,根系水导呈现缓慢--慢速的恢复趋势,Pn、Gs、Tr、叶片水势随着根系水导速率的增加而逐渐恢复;Ci则随复水时间的延长而逐渐下降.但各参数除Ci外,均没有恢复到胁迫前水平.紫花苜蓿根系水导与光合参数在复水后的恢复程度说明,紫花苜蓿对干旱逆境的抵御与适应能力相对较弱,但陇东苜蓿对水分胁迫的忍耐能力强于阿尔冈金.     

Trickle and sprinkler irrigation of potato (Solanum tuberosum L.) in the Middle Anatolian Region in Turkey

The potato (Solanum tuberosum L.) is widely planted in the Middle Anatolian Region, especially in the Nigde-Nevsehir district where 25% of the total potato growing area is located and produces 44% of the total yield. In recent years, the farmers in the Nigde-Nevsehir district have been applying high amounts of nitrogen (N) fertilizers (sometimes more than 900 kg N ha⁻¹) and frequent irrigation at high rates in order to get a much higher yield. This situation results in increased irrigation and fertilization costs as well as polluted ground water resources and soil. Thus, it is critical to know the water and nitrogen requirements of the crop, as well as how to improve irrigation efficiency. Field experiments were conducted in the Nigde-Nevsehir (arid) region on a Fluvents (Entisols) soil to determine water and nitrogen requirements of potato crops under sprinkler and trickle irrigation methods. Irrigation treatments were based on Class A pan evaporation and nitrogen levels were formed with different nitrogen concentrations.The highest yield, averaging 47,505 kg ha⁻¹, was measured in sprinkler-irrigated plots at the 60 g m⁻³ nitrogen concentration level in the irrigation treatment with limited irrigation (480 mm). Statistically higher tuber yields were obtained at the 45 and 60 g m⁻³ nitrogen concentration levels in irrigation treatments with full and limited irrigation. Maximum yields were obtained with about 17% less water in the sprinkler method as compared to the trickle method (not statistically significant). On the loam and sandy loam soils, tuber yields were reduced by deficit irrigation corresponding to 70% and 74% of evapotranspiration in sprinkler and trickle irrigations, respectively. Water use of the potato crop ranged from 490 to 760 mm for sprinkler-irrigated plots and 565–830 mm for trickle-irrigated treatments. The highest water use efficiency (WUE) levels of 7.37 and 4.79 kg m⁻³ were obtained in sprinkle and trickle irrigated plots, respectively. There were inverse effects of irrigation and nitrogen levels on the WUE of the potato crops. Significant linear relationships were found between tuber yield and water use for both irrigation methods. Yield response factors were calculated at 1.05 for sprinkler methods and 0.68 for trickle methods. There were statistically significant linear and polynomial relationships between tuber yield and nitrogen amounts used in trickle and sprinkler-irrigated treatments, respectively. In sprinkler-irrigated treatments, the maximum tuber yield was obtained with 199 kg N ha⁻¹. The tuber cumulative nitrogen use efficiency (NUE_cu) and incremental nitrogen use efficiency (NUE_in) were affected quite differently by water, nitrogen levels and years. NUE_cu varied from 16 to 472 g kg⁻¹ and NUE_in varied from 75 to 1035 g kg⁻¹ depending on the irrigation method. In both years, the NH₄-N concentrations were lower than NO₃-N, and thus the removed nitrogen and nitrogen losses were found to be 19–87 kg ha⁻¹ for sprinkler methods and 25–89 kg ha⁻¹ for trickle methods. Nitrogen losses in sprinkler methods reached 76%, which were higher than losses in trickle methods.     

Yield performance of spring wheat improved by regulated deficit irrigation in an arid area

A field experiment was conducted in 2003 and 2004 growing seasons to evaluate the effects of regulated deficit irrigation on yield performance in spring wheat (Triticum aestivum) in an arid area. Three regulated deficit irrigation treatments designed to subject the crops to various degrees of soil water deficit at different stages of crop development and a no-soil-water-deficit control was established. Soil moisture was measured gravimetrically in the increment of 0–20 cm every five to seven days in the given growth periods, while that in 20 increments to 40, 40–60, 60–80, and 80–100 cm depth measured by neutron probe. Compared to the no-soil-water-deficit treatment, grain yield, biomass, harvest index, water use efficiency (WUE), and water supply use efficiency (WsUE) in spring wheat were all greatly improved by 16.6–25.0, 12.4–19.2, 23.5–27.3, 32.7–39.9, and 44.6–58.8% under regulated deficit irrigation, and better yield components such as thousand-grain weight, grain weight per spike, number of grain, length of spike, and fertile spikelet number were also obtained, but irrigation water was substantially decreased by 14.0–22.9%. The patterns of soil moisture were similar in the regulated deficit treatments, and the soil moisture contents were greatly decreased by regulated deficit irrigation during wheat growing seasons. Significant differences were found between the no-soil-water-deficit treatment and the regulated soil water deficit treatments in grain yield, yield components, biomass, harvest index, WUE, and WsUE, but no significant differences occurred within the regulated soil water deficit treatments. Yield performance proved that regulated deficit irrigation treatment subjected to medium soil water deficit both during the middle vegetative stage (jointing) and the late reproductive stages (filling and maturity or filling) while subjected to no-soil-water-deficit both during the late vegetative stage (booting) and the early reproductive stage (heading) (MNNM) had the highest yield increase of 25.0 and 14.0% of significant water-saving, therefore, the optimum controlled soil water deficit levels in this study should range 50–60% of field water capacity (FWC) at the middle vegetative growth period (jointing), and 65–70% of FWC at both of the late vegetative period (booting) and early reproductive period (heading) followed by 50–60% of FWC at the late reproductive periods (the end of filling or filling and maturity) in treatment MNNM, with the corresponding optimum total irrigation water of 338 mm. In addition, the relationships among grain yield, biomass, and harvest index, the relationship between grain yield and WUE, WsUE, and the relationship between harvest index and WUE, WsUE under regulated deficit irrigation were also estimated through linear or non-linear regression models, which indicate that the highest grain yield was associated with the maximum biomass, harvest index, and water supply use efficiency, but not with the highest water use efficiency, which was reached by appropriate controlling soil moisture content and water consumption. The relations also indicate that the harvest index was associated with the maximum biomass and water supply use efficiency, but not with the highest water use efficiency.     

Soil N and salinity leaching after the autumn irrigation and its impact on groundwater in Hetao Irrigation District,China

Soil water and salinity are crucial factors influencing crop production in arid regions. An autumn irrigation system employing the application of a large volume of water (2200–2600 m³ ha⁻¹) is being developed in the Hetao Irrigation District of China, since the 1980s with the goal to reduce salinity levels in the root zone and increase the water availability for the following spring crops. However, the autumn irrigation can cause significant quantities of NO₃⁻ to leach from the plant root zone into the groundwater. In this study, we investigated the changes in soil water content, NO₃–N and salinity within a 150 cm deep soil profile in four different types of farmlands: spring wheat (F_W), maize (F_M), spring wheat–maize inter-planting (F_W–M) and sunflower (F_S). Our results showed that (1) salt losses mainly occurred in the upper 60 cm of the soil and in the upper 40 cm for NO₃–N; (2) the highest losses of salt and NO₃–N could be observed in F_W, whereas the lowest losses were found in F_W–M.NO₃–N concentration, pH and electrical conductivity (EC) in the groundwater were also monitored before and after the autumn irrigation. We found that the autumn irrigation caused the groundwater concentration of NO₃–N to increase from 1.73 to 21.6 mg L⁻¹, thereby, exceeding the standards of the World Health Organization (WHO). Our results suggest that extensive development of inter-planting tillage might be a viable measure to reduce groundwater pollution, and that the application of optimized minimum amounts of water and nitrogen to meet realistic yield goals, as well as the timely application of N fertilizers and the use of slow release fertilizers can be viable measures to minimize nitrate leaching.     

有机与无机肥料对山地梨枣品质的影响

设置不同无机肥料(氮肥、磷肥、钾肥和氮磷钾混合肥施用)、不同有机肥(沼肥和腐熟油渣肥)和不施肥(对照),研究不同施肥方法对梨枣的水分含量,总糖、可溶性固形物、还原型抗坏血酸和总抗坏血酸、质构特性以及有机酸的影响。结果表明:肥料对梨枣的水分含量没有显著性影响,显著降低了梨枣的苹果酸,柠檬酸和有机酸总含量。有机肥沼肥和腐熟油渣肥可显著提高梨枣的果皮果肉硬度和咀嚼性以及可溶性固形物、总糖含量、抗坏血酸含量,酒石酸含量却显著降低。无机肥料氮肥、磷肥、钾肥中,钾肥有利于梨枣的可溶性固形物、总糖、抗坏血酸,苹果酸和柠檬酸的含量积累,而酒石酸含量却减少。表明增施有机肥和钾肥有利于山地梨枣品质的提高。     

黄土丘陵植被恢复区不同植被类型对土壤物理性质的影响

通过对比研究了山西吴起县植被恢复区不同植被类型的林草地和农田的土壤物理性质,包括土壤容重、土壤孔隙度、土壤水稳性团粒结构。结果表明:不同植被类型的土壤容重为1.17~1.21 g/cm3,差异较小,但均比农田(1.31 g/cm3)低约11%,不同植被类型地各层土壤不同粒径的土壤团粒结构百分含量高于相应的天然草地和农田。实施植被修复后,与农田相比,林地土壤物理性质得到明显改善,混交林的土壤物理性质好于纯林林,天然草地和农田较差,天然草地略好于农田。     

黄土丘陵区流域主要植被类型养分循环特征

以黄土丘陵沟壑区典型小流域纸坊沟流域为例,系统研究流域在植被稳定恢复期1种乔木、4种灌木和9种草地植被类型的养分循环平衡特征。结果表明,乔灌植被类型的叶片养分含量明显高于当年的新生枝条,新生枝条则明显高于枝干;乔木植被类型的生物量、氮磷养分累积量明显高于灌木植被类型,灌木植被类型则高于草地植被类型;乔木的氮养分循环速率是0.789,灌木为0.742,草地为1.000;乔木P2O5循环速率是0.881,灌木为0.758,草地为1.000。乔木的氮养分年盈余量是333.0 kg/km2,灌木为508.5 kg/km2,草地为597.0 kg/km2;乔木的P2O5年盈余量是333.0 kg/km2,灌木为423.0 kg/km2,草地为531.0 kg/km2。     

晋西黄土区主要造林树种耗水量测算与分析

依据水量平衡原理,采用盆栽试验分别测算了晋西黄土区主要造林树种侧柏、刺槐、杏树和梨树在其生长季(4～10月)成熟单株树木的耗水量,并根据林地土壤水分动态及土壤水分特征曲线标定的各树种无效水界值,分析了各树种土壤水分供耗特点及其有效性.结果表明:①2002贫水年生长季降水量430.7 mm,试验树种同期耗水量约为430～470 mm,树木供耗失衡;2003丰水年降水量870.2 mm,耗水量约为450～510 mm,但降雨分配不均,5月和10月树木供耗也略有失衡.②不同树种年内土壤含水量变化趋势相近,而同月耗水量差异较大,同一树种不同月耗水量差异也较大,丰水年各试验地土壤水分状况要好于贫水年.③侧柏、刺槐、杏树和梨树无效水界值为8.0%,8.4%,9.4%和10.9%,侧柏较其它树种利用水分能力最强.贫水年林外单株树木土壤含水量在一段时间内低于对应树种的无效水界值,影响树木正常生长.单株树木依靠冬季和次年春季降水补充,生长季初期都能恢复到速效水水平.     

应用可拓学原理评价黄瓜根分泌物的化感潜势

 对黄瓜组培根分泌物的化感潜势进行可拓评价, 得出黄瓜组培根分泌物对菜豆幼苗生长有显著促进作用, 而对其它3种作物有明显的毒害作用, 毒害程度为黄瓜>甜瓜>番茄。同时, 建立了黄瓜组培根分泌液的化感效应的数学模型R_E = [ k₁R_p0 / ( k₂ - k₁ ) ] ( e^{- k1t} - e^{- k2t} ) ( e- ^k1a - e^{- k2a} ) , 说明了黄瓜组培根分泌液的化感效应与组培根培养时间( t) 以及根分泌液浓度( a) 显著相关。黄瓜根分泌物对4种受体作物显示出显著的化学干扰差异, 论证了植物种内(间) 发生的干扰作用与植物的品种(系) 有关, 从理论上得出菜豆可以作为黄瓜的间套作物或下茬作物。     

覆膜和钾肥对马铃薯铁素吸收分配的影响

通过田间试验研究了覆膜和钾肥对马铃薯不同生育时期体内铁的浓度、吸收累积量及其分布的影响.结果表明:马铃薯全株、叶、茎、块茎中铁的浓度从苗期到成熟期呈波浪式变化;铁的累积量在整个生育时期呈现先增大后减小的变化规律,均在块茎膨大期达到峰值;而铁素在马铃薯体内的分布情况表现为:前4个时期在各个器官中分布的顺序为叶＞茎＞块茎,到成熟期表现为茎＞叶＞块茎.覆膜对叶中铁的分布有减小的作用,即它能增大茎和块茎中铁的分布,随着生育时期的向前推进,块茎中铁的分布明显增大,它对块茎中铁的累积也有一定的增大效果;钾肥在成熟期之前的一段时间内能在一定程度增大铁在块茎中的分布,但是此二因素对马铃薯体内铁的影响作用均未达到一定的显著水平.