冬小麦近轴和远轴叶面气孔对土壤水分胁迫反应的敏感性

当根层土壤水分含量不足,作物体内出现水分胁迫时,小麦叶片两面气孔的反应有明显差异。远轴叶面气孔对水分胁迫的反应比近轴叶面气孔敏感。当出现水分胁迫时,远轴叶面气孔首先收缩,且收缩的程度比近轴叶面气孔大。远轴与近轴叶面气孔阻力的比值(r_(ab)/r_(ab))与根层平均土壤水势(Ψ_s)有关,当Ψ_s大于-50 kPa时,r_(ab)/r_(ad)基本稳定在1.5左右,而当Ψ_s小于-50 kPa时,r_(ab )/r_(ab)随Ψ_s降低而明显增加。     

小麦条锈病罹病植株对水分胁迫的响应

水分胁迫时,小麦条锈病病叶的叶片扩散阻力（ＬＤＲ）明显增大,蒸腾速率（Ｔｐ）、相对含水量（ＲＷＣ）、水势（Ψｗ）、渗透势（Ψπ）和压力势（Ψｐ）明显降低。亲和与不亲和性反应寄主病叶对水分胁迫的反应明显不同。亲和性反应寄主叶片在水分胁迫时表现出较低的反应型,产孢期推迟;Ｔｐ、ＬＤＲ、ＲＷＣ、Ψｗ、Ψｐ和Ψπ在产孢前轻微下降或高;在开始产孢后病叶Ｔｐ急剧升高,ＬＤＲ、Ｔｐ、ＲＷＣ、Ψｗ、Ψπ和Ψｐ大幅     

土壤干旱胁迫对作物影响的模拟研究进展

用于模拟土壤干旱胁迫对作物影响的模型分为两类,一是水分管理模型,此类模型并不模拟作物的生长发育,但可以用于灌溉管理;二是作物生长模拟模型,这类模型模拟作物生长的主要过程(如叶片生长、生物量的积累与分配等),通常以实际蒸腾与潜在蒸腾的比值估算土壤干旱胁迫对作物光合的影响,近年来发展的耦合模型将植物的碳同化、蒸腾、能量平衡以及气孔行为相耦合,使得土壤干旱胁迫对作物影响的模拟更具机理性。本文从不同模型模拟土壤干旱对作物影响的原理入手,阐述了水分管理模型(FAO水分生产函数模型)、作物生长模型(Aqua Crop模型、CERES-Maize模型、WOFOST模型、EPICphase模型、耦合模型)等具有代表性模型是如何模拟土壤干旱胁迫对作物生长发育和(或)产量影响的,提出了作物模型模拟土壤干旱胁迫影响时应着力解决的问题:完善干旱对作物物候的影响模拟;考虑花期不遇对作物产量影响的模拟;考虑后续持续影响的模拟机制;发展更加基于物理和生理过程的模型。提出:作物模型的发展还需要多领域如模型程序员、田间试验、植物生理学家的相互协同与发展,田间试验研究是作物模型发展不可或缺的数据来源与坚实基础。     

冬小麦不同生育期最小冠层阻力的估算

作物最小冠层阻力是研究农田蒸发和作物缺水的一个重要参数。使用作物的冠层红外温度信息,将作物在充分灌溉情况下冠层温度与空气温度之差与空气的饱和水汽压差的经验关系同其理论解释相结合,通过实验数据,估算了在华北平原气候条件下的冬小麦（Triticum aestivum L.）的平均最小冠层阻力,为基于这种阻力的应用共基础,研究表明冬小麦最小冠层阻力随发育期而不同,并且抽穗前后差异明显,给出了冬小麦不同生育阶段的平均最小冠层阻力。     

考虑土壤水分限制的春小麦生长简化模型

建立了以日长（Ｌ）和日总辐射（ＴＤＲ）为自变量的春小麦（Ｔｒｉｔｉｃｕｍ ａｅｓｔｉｖｕｍ Ｌ．）碳同化和干物质累积（ＤＭＡ）的简化模型,考虑了水分限制下光能利用效率（ａ）,碳传输导度（ｇｃ）均被降低的设定,将反映春小麦水分状况的叶水热（Ψ）作为参数纳一模型,Ψ则通过多元回旭由８０ｃｍ土层相对含水量（θＲ,８０＿,气温（Ｔａ）水汽压差（ＶＰＤ）,低于－１．５ＭＰａ叶水势之和（Ψｃ,１．５）给出。讨     

典型喀斯特区不同植被恢复方式苔藓功能性状及其对土壤因子的响应

苔藓功能性状反映了苔藓对生长环境的响应与适应,对其所在土壤表层的功能特性具有重要指示意义。但喀斯特地区植被恢复初期苔藓功能性状与土壤因子关系还缺乏深入认识。以典型喀斯特峰丛洼地人工林、牧草和人工林+牧草3种植被恢复方式下苔藓为研究对象,分析了苔藓功能性状及其与土壤因子的关系。结果表明：（1）苔藓单位面积冠层质量（CMA）、冠层密度（CD）、生物量和饱和吸水量在牧草地有最大值。苔藓冠层高度在牧草地显著低于人工林和人工林+牧草,且牧草地苔藓营养元素含量较低。（2）人工林和人工林+牧草表层土壤（0-2 cm）养分含量和土壤含水量（SWC）较高,牧草地表层土壤养分含量和SWC较低。（3）冗余分析表明,苔藓营养性状（营养元素含量及化学计量比）与土壤因子主要呈正相关关系,而CMA、CD及生物量关联指标与土壤因子主要呈负相关关系,土壤交换性镁和SWC是影响苔藓功能性状的主要土壤因子。研究结果表明,苔藓通过不同的性状组合适应不同植被类型生境,其中牧草地更适宜苔藓拓殖和生长,可考虑将苔藓应用于牧草地对喀斯特退化生态系统进行修复。     

涡度相关法研究土壤水分状况对沙地杨树人工林生态系统能量分配和蒸散日变化的影响

为了解位于北京大兴区林场杨树人工林在不同的土壤水分环境条件下的水汽交换过程和能量的分配差异及其与环境因子关系,运用涡度相关（Eddy covariance,EC）法开路系统、常规微气象观测系统及土壤热通量板等设施对生态系统生长季内典型水分胁迫和无水分胁迫条件下蒸散日变化、能量分配以及与各环境因子的关系进行了测定分析和比较。结果表明,在水分严重胁迫日（以7月7日为例）,蒸散日变化过程为单峰曲线,全天（24h）蒸散量为2.4mm;而在无水分胁迫典型日（以7月25日为例）,蒸散日变化过程呈多峰曲线,全天蒸散量为4．5mm。能量平衡分析显示,无水分胁迫条件下潜热通量（LE）占净辐射通量（Rn）的比例远高于水分胁迫条件下潜热通量占净辐射通量的比例,说明水分充足时,能量的大部分用于蒸散。水分胁迫条件下蒸散速率与各环境因子的相关性均低于无水分胁迫条件下蒸散速率与环境因子的相关性。水分胁迫条件下,蒸散速率主要与净辐射和下垫面因子关系显著,而与其它因子的相关性较小;无水分胁迫条件下,蒸散速率与下垫面土体含水量和各气象因子均表现出较强的相关性。大气温度对于两个典型日蒸散速率的影响均很小;土壤含水量与水分胁迫日的蒸散速率几乎没有相关性,反应出土壤水分含量低至对蒸散几乎没有贡献了。     

冬小麦不同生育期最上冠层阻力的估算

作物最小冠层阻力是研究农田蒸发和作物缺水的一个重要参数.使用作物的冠层红外温度信息,将作物在充分灌溉情况下冠层温度与空气温度之差与空气的饱和水汽压差的经验关系同其理论解释相结合,通过实验数据,估算了在华北平原气候条件下的冬小麦(Triticum aestivum L.)的平均最小冠层阻力,为基于这种阻力的应用提供基础.研究表明冬小麦最小冠层阻力随发育期而不同,并且抽穗前后差异明显,给出了冬小麦不同生育阶段的平均最小冠层阻力.     

水分胁迫对芒果(Mangifera indica L.)幼叶细胞活性氧伤害的影响

对芒果进行了水分干旱胁迫处理,结果表明,水分胁迫使芒果幼叶的相对含水量ＲＷＣ（ｒｅｌ－ａｔｉｖｅ ｗａｔｅ ｃｏｎｔｅｎｔ）和叶水势ΨＴ下降,芒果幼叶的超氧离子Ｏ＾－２产生速率随水分胁迫处理强度加大而增加,丙二醛ＭＤＡ（ｍａｌｏｎｄｉａｌｄｅｈｙｄｅ）含量的变化趋势与Ｏ＾－２产生速率的变化趋势相似超氧经歧化酶ＳＯＤ（ｓｕｐｅｒｏｘｉｄｅ ｄｉｓｍｕｔａｃｅ）,这氧化物酶ＰＯＤ（ｐｅｒｏｘｉｄａｓｅ     

基于红外热像仪的棉花水分状况诊断方法

冠层温度信息是作物水分状况诊断信号之一,红外热像仪能实时准确地获取较大区域的温度分布.本文以棉花为研究对象,针对红外热像仪获取冠层温度的主要影响因素(方位、角度和距离)开展试验,研究了不同水分处理下不同方法获取的作物水分胁迫指数(CWSI)与土壤含水率(SWC)、叶水势(LWP)和气孔导度(g_s)之间的相互关系.结果表明： 逆太阳光与冠层45°夹角获取的CWSI与SWC、LWP和g_s具有较好的相关性,是观测冠层温度的适宜方法;随着距离的增大,冠层温度会表现出衰减的现象,远距离的拍摄需要进行必要的校准工作;通过分析干湿参考表面温度与冠层温度之间的关系,提出了适合华北地区棉花水分胁迫指数的简化计算模式.     

Modeling soil water regime and corn yields considering climatic uncertainty

Real time estimation of soil moisture and crop yield plays an important role for best irrigation management practices especially in arid and semiarid regions. A simulation model able of real time estimating and forecasting soil water storage and corn yield response to soil moisture was developed by combining two existing models. Soil water storage was estimated through the soil water balance equation considering the uncertainty of evapotranspiration and combing with Kalman filter technique. Crop dry matter and grain yield were simulated by using a functional relationship between yield and soil moisture. Some improvements have been made in the response function by considering different impacts of moisture stress on crop growth and yield for the different growing stages. Four years data sets collected in an experimental station in the North China Plain were used to calibrate and test the model. Results indicate that soil moisture storage in the soil profile estimated and predicted by the model agrees well with the measured data, and the relative error of yield prediction is around 10%, which means that the combined model and the methodology applied are capable of predicting crop yield and soil water storage dynamics.     

Oxygation Enhances Growth, Gas Exchange and Salt Tolerance of Vegetable Soybean and Cotton in a Saline Vertisol

Impacts of salinity become severe when the soil is deficient in oxygen. Oxygation (using aerated water for subsurface drip irrigation of crop) could minimize the impact of salinity on plants under oxygen-limiting soil environments. Pot experiments were conducted to evaluate the effects of oxygation (12% air volume/volume of water) on vegetable soybean (moderately salt tolerant) and cotton (salt tolerant) in a salinized vertisol at 2, 8, 14, 20 dS/m ECe. In vegetable soybean, oxygation increased above ground biomass yield and water use efficiency (WUE) by 13% and 22%, respectively, compared with the control. Higher yield with oxygation was accompanied by greater plant height and stem diameter and reduced specific leaf area and leaf Na+ and Cl-concentrations. In cotton, oxygation increased lint yield and WUE by 18% and 16%, respectively, compared with the control, and was accompanied by greater canopy light interception, plant height and stem diameter. Oxygation also led to a greater rate of photosynthesis, higher relative water content in the leaf, reduced crop water stress index and lower leaf water potential. It did not, however, affect leaf Na+ or Cl- concentration. Oxygation invariably increased, whereas salinity reduced the K+ : Na+ ratio in the leaves of both species. Oxygation improved yield and WUE performance of salt tolerant and moderately tolerant crops under saline soil environments, and this may have a significant impact for irrigated agriculture where saline soils pose constraints to crop production.     

Dissecting the nonlinear response of maize yield to high temperature stress with model‐data integration

Evidence suggests that global maize yield declines with a warming climate, particularly with extreme heat events. However, the degree to which important maize processes such as biomass growth rate, growing season length (GSL) and grain formation are impacted by an increase in temperature is uncertain. Such knowledge is necessary to understand yield responses and develop crop adaptation strategies under warmer climate. Here crop models, satellite observations, survey, and field data were integrated to investigate how high temperature stress influences maize yield in the U.S. Midwest. We showed that both observational evidence and crop model ensemble mean (MEM) suggests the nonlinear sensitivity in yield was driven by the intensified sensitivity of harvest index (HI), but MEM underestimated the warming effects through HI and overstated the effects through GSL. Further analysis showed that the intensified sensitivity in HI mainly results from a greater sensitivity of yield to high temperature stress during the grain filling period, which explained more than half of the yield reduction. When warming effects were decomposed into direct heat stress and indirect water stress (WS), observational data suggest that yield is more reduced by direct heat stress (?4.6 ± 1.0%/°C) than by WS (?1.7 ± 0.65%/°C), whereas MEM gives opposite results. This discrepancy implies that yield reduction by heat stress is underestimated, whereas the yield benefit of increasing atmospheric CO₂ might be overestimated in crop models, because elevated CO₂ brings yield benefit through water conservation effect but produces limited benefit over heat stress. Our analysis through integrating data and crop models suggests that future adaptation strategies should be targeted at the heat stress during grain formation and changes in agricultural management need to be better accounted for to adequately estimate the effects of heat stress.     

土壤含水量与头季稻和再生稻产量的关系

土壤含水量与头季稻和再生稻产量的关系熊洪ＳｏｍｂａｔＣｈｉｎａｗｏｎｇ（四川省农科院水稻高粱所,泸州６４６１００）（ＫａｓｅｔｓａｒｔＵｎｉｖｅｒｓｉｔｙ,Ｂａｎｇｋｏｋ７３１４０）ＲｅｌａｔｉｏｎｓｈｉｐＢｅｔｗｅｅｎＳｏｉｌＷａｔｅｒＣｏｎｔｅｎ...     

Phosphorus nutrition and water deficits in field-grown soybeans

Phosphorus and water deficits are important limiting factors in agricultural production. A field experiment was carried out with soybean (Glycine max (L.) Merr.) to determine whether the effect of water stress on field-grown soybean changes with soil P availability, and whether soil water content affects plant P nutrition. The soil was a Sadler series (fine-silty, mixed, mesic Glossic Fragiudalf) located at Princeton, Kentucky, USA (37°60′ north, 87°60′ west). The experiment was a factorial with three levels of soil P availability (4, 19 and 32 mg kg⁻¹, Mehlich III) and two of water (irrigated and non-irrigated). Most of the effects of phosphorus and water stress on soybean growth were additive, so that, in general, effects of water stress were similar at each P level. Phosphorus deficiency slowed vegetative development, reduced shoot growth, LAI, P absorption and concentration, seed number, size and yield, and increased root length density in the surface soil. Water stress accelerated crop maturity, reduced shoot growth, LAI, P absorption and concentration, seed number, size and yield, and increased root length density. Some interactions between P and water were observed. Water stress slowed vegetative development only at the lowest P level (P0). The crop had a positive response to increasing P availability in both situations, with and without irrigation, suggesting that P addition would be justified even when a dry growing season is likely to occur. This revised version was published online in June 2006 with corrections to the Cover Date.     

The effect of soil strength on the yield of wheat

Although it is well-known that high soil strength is a constraint to root and shoot growth, it is not clear to what extent soil strength is the main physical stress that limits crop growth and yield. This is partly because it is difficult to separate the effects of soil drying and high soil strength, which tend to occur together. The aim of this paper is to test the hypothesis that for two different soil types, yield is closely related to soil strength irrespective of difference in soil water status and soil structure. Winter (Triticum aestivum L., cv. Hereward) and spring wheat (cv. Paragon) were grown in the field on two soils, which had very different physical characteristics. One was loamy sand and the other sandy clay loam; compaction and loosening treatments were applied in a fully factorial design to both. Crop growth and yield, carbon isotope discrimination, soil strength, water status, soil structure and hydraulic properties were measured. The results showed that irrespective of differences in soil type, structure and water status, soil strength gave a good prediction of crop yield. Comparison with previous data led to the conclusion that, irrespective of whether it was due to drying or compaction (poor soil management), soil strength appeared to be an important stress that limits crop productivity.     

稻麦轮作体系下有机肥施用对作物产量和土壤性质影响的整合分析

为明确稻麦轮作系统有机肥施用对作物产量和土壤性质的影响,本研究搜集已公开发表的文献数据,利用meta分析法定量分析了有机肥类型(普通有机肥、生物质炭、秸秆)、施用策略(单施有机肥、有机肥配施部分化肥、有机肥配施全量化肥)、施用年限(短期、中期、长期)对稻麦产量和土壤性质的影响及其对不同土壤条件(酸性、中性、碱性)的响应。结果表明: 与单施化肥相比,有机肥施用对水稻和小麦的增产效应相近,分别为3.1%和3.0%。有机肥施用对土壤性质的提升效果更明显,显著降低了土壤容重(5.7%),显著提高了土壤有机质、全氮、全磷、碱解氮、速效磷和速效钾含量,以及微生物生物量碳、氮,增幅在11.7%～38.4%。不同类型有机肥中,生物质炭和普通有机肥对土壤性质的改良效果优于秸秆;与单施有机肥相比,有机肥配施化肥的作物增产效果更好,而土壤性质改良效果较差;随着有机肥施用年限增加,作物增产和土壤肥力提升效应逐渐增强;在酸性土壤条件下有机肥施用对作物的增产效果最显著。土壤容重与稻麦周年产量呈显著负相关,而土壤全氮、速效磷、速效钾含量和微生物生物量氮与稻麦周年产量呈显著正相关关系。     

Increasing the okra salt threshold value with biochar amendments

Soil salinity is a severe worldwide environmental problem that adversely affects soil properties and the crop growth such as okra. We hypothesized that biochar soil amendments could increase the okra salt threshold, alleviate salt stress and improve soil productivity. In this study, a pot experiment was conducted to investigate whether biochar could ameliorate the effects of salinity on okra plants. Three biochar amendment (BA) soil applications (0%, 5% and 10% by mass of soil) were considered for seven irrigation water salinity levels (0.75, 1.0, 2.0, 4.0, 5.0, 6.0 and 7.0?dS?m^?1) in a randomized block design with three replications. The Maas and Hoffman salt tolerance model was used to evaluate the effects of BA on okra plant growth parameters (e.g. yield, biomass) and water use efficiency for each salinity treatment. The results showed that increasing the soil salinity levels caused significant decreases in plant yields and yield components. However, biochar application rates of 5% and 10% increased the okra threshold by 19.7% and 81.2%, respectively, compared to the control (0%). The 10% biochar application rate also resulted in the greatest okra plant growth and increased yield, indicating that the effects of salt stress were ameliorated; moreover, the soil bulk density was decreased, and the water content was increased. Hence, biochar soil amendments could be considered as an important agronomic practice that could potentially overcome the adverse effects of salt stress.     

土地利用变化对海南土壤水源涵养功能的影响

热带地区已有大量原始林转变为其他土地利用类型,影响了陆地生态系统的水源涵养功能.为了明确热带原始林转变为其他土地类型对土壤水源涵养功能的影响,在海南中部山区选择4种典型土地利用类型,包括林龄大于100年的原始林(VF)、10年生次生林(SF)、12年生槟榔林(AF)和35年生橡胶林(RF),评估土地利用变化对土壤持水性能和水源涵养功能指数(SWI)的影响.结果表明: 与原始林相比,表层土壤(0～10 cm)中,其他土地类型土壤持水性能指标均降低,12年槟榔林各土层指标均最低.土壤含水量和最大持水量与植被郁闭度、土壤有机质和土壤容重显著相关,表明郁闭度、土壤有机质和紧实度的改变是土壤持水性能变化的重要原因.与原始林相比,次生林、槟榔林和橡胶林土壤水源涵养功能分别减少27.7%、54.3%和11.5%,不同土层的差异各异,橡胶林仅表层土壤水源涵养功能显著降低.植被郁闭度、土壤有机质和土壤容重可解释土壤水源涵养功能变量的83.3%.土地利用转变显著改变了土壤持水性能和土壤水源涵养功能,相比12年槟榔林,35年橡胶林能更好地保持土壤水分,土地管理中增加土壤有机质和减少土壤紧实度可改善土壤持水性能及水源涵养功能.