Effect of soil matric potential on leaf water potential,diffusive resistance,growth and development ofGmelina arborea L. seedlings

Gmelina arborea L. seedling growth and diurnal stomatal opening (as measured by stomatal resistance) were studied at soil matric potential 0, -0.1 and -0.72 × 10^?5 Pa. Leaf area, leaf number, plant height and dry weights of the vegetative parts were significantly reduced as soil matric potential decreased from 0 to -0.72 × 10^?5 Pa. The growth responses followed the same trend as net assimilation rate and relative growth rate. The highest moisture stress induced leaf senescence and leaf fall. Leaf water potential decreased from - 2 × 10^?5 Pa to - 20 × 10^?5 Pa with increasing soil moisture stress. Results indicate that the diurnal stomatal opening is controlled by photon flux density when this species is grown at soil matrio potential 0 Pa. However, with decreasing soil matrio potential (- 0.10 and -0.72 × 10^?5 Pa) the internal plant water deficit appears to oontrol the stomatal opening.     

黄土高原水土保持林对土壤水分的影响

黄土高原植被恢复的限制因素主要是土壤水分,植被与土壤水分关系的研究对黄土高原植被恢复具有重要意义.2008年7月1日至2009年10月31日间采用EnviroSMART土壤水分定位监测系统以每30min监测1次的频度,对晋西黄土区刺槐人工林地、油松人工林地、次生林地的土壤水分变化进行了研究.研究得出:次生林地0-150 cm土层中平均蓄水量为331.95mm,刺槐人工林地为233.85 mm,有整地措施的油松人工林地为314.85mm,刺槐人工林比次生林多消耗的98.10mm土壤水分主要来源于80 cm以下土层.次生林主要消耗0-80 cm土层的水分,而人工林不但对0-80 cm土层水分的消耗量大于次生林,对深层土壤的消耗也较次生林大,这将有可能导致人工林地深层土壤的“干化”.在土壤水分减少期(11-1月)刺槐人工林土壤水分的日均损耗量为0.86mm、油松人工林为0.82 mm、次生林为0.84 mm.土壤水分缓慢恢复期(2-5月)刺槐人工林地土壤水分的恢复速度0.90mm/d,油松人工林地为0.53 mm/d、次生林地为0.79 mm/d.土壤水分剧烈变化期(5-10月)刺槐人工林地土壤水分含量的极差为95.71mm,油松人工林地为179.1mm,次生林地为72.03mm.在干旱少雨的黄土高原进行植被恢复时,应多采取封山育林等方式,依靠自然力量形成能够与当地土壤水资源相协调的次生林,是防止人工植被过度耗水形成“干化层”、保障水土保持植被持续发挥生态服务功能的关键.     

青藏高原高寒草甸植被特征与温度、水分因子关系

以广布于青藏高原的高寒草甸为研究对象,进行模拟增温实验,探讨高寒草甸植被特征与温度、水分因子关系,并试图论证高寒草甸植被是否符合生物多样性代谢理论.结果表明:①高寒草甸植被物种多样性的对数与绝对温度的倒数呈显著线性递减关系,空气-地表-浅层土壤(0-20 cm)温度(R2 ＞0.6,P＜0.01)较深层土壤(40-100 cm)温度(R2＜0.5,P＜0.05)对物种多样性影响大;其植被新陈代谢平均活化能为0.998-1.85 eV,高于生物多样性代谢理论预测值0.6-0.7 eV,这是高寒草甸植被对长期低温环境适应进化的结果.②除趋势对应分析和冗余分析显示,温度对植被地上部分影响较大,而土壤水分对全株影响均较大,适当的增温与降水均可极显著促进高寒草甸植被生长.③逐步回归和通径分析显示,40 cm、60 cm深度土壤水分对植被地上部分产生直接影响,20 cm高度空气相对湿度和40 cm深度土壤温度对其产生间接影响;40 cm深度土壤温度和60 cm深度土壤水分对植被地下部分产生直接影响,红外地表温度对其产生间接影响.深层土壤温度和水分对高寒草甸植被具有影响作用,这可能与增温后冻土的融化有关,但其机理尚待进一步研究.     

Effects of Soil Moisture on Control of Heterodera schachtii with Aldicarb

Soil moisture and the nematode population density in aldicarb-treated soil influenced control of the sugarbeet nematode, Heterodera schachtii. Greater numbers of nematode larvae infected 14-day-old sugarbeet seedlings growing in aldicarb-treated soil at 20-30% than at 80-100% field capacity (F. C.), and plant growth was inversely related to nematode infection and the nematode population density. Compared with that of control plants, plant growth increase also was greater at 80-100% F. C. when the nematode population was above 1.8 larvae/gm soil. A nematode population of 1.8 larvae/gm soil did not significantly affect sugarbeet yields. Aldicarb gave less control when soil moisture levels dropped to 20 and 50% F. C. at nematode populations of 3.5 and 6.2 larvae/gm soil. More effective control was obtained wth soil moisture levels at or above 80% F. C. This difference was attributed to continued activity of the toxicant in the rhizosphere at the high moisture level.     

Effect of soil moisture on overwintering pupae in Spodoptera exigua (Lepidoptera: Noctuidae)

Spodoptera exigua Hübner (Lepidoptera: Noctuidae), can overwinter as pupae at depths of 0- to 5-cm beneath the ground. In order to understand the effect of soil moisture on the overwintering success of this species, we tested the supercooling point and survival of pupae, and the growth rate of prepupae that were exposed to different temperature and soil moisture in the laboratory. Results showed that supercooling points, body water contents, and survivals after the different pre-treatments were not significantly affected by the soil moisture. The developmental progress of prepupae, survival of prepupae and pupae were negatively correlated with soil moisture as well as the delay of exposure time, which supports the hypothesis that soil moisture acts as a developmental modulator. We presumed that the delay of pupation and lower prepupae survival under higher soil moisture was due to lack of a complete pupal chamber for protection at low temperatures. Low pupal survival was likely attributed to lack of oxygen in the soil, especially under the condition of higher soil moisture. We suggest that using strategies of irrigation and soil tillage during winter may decrease the overwintering population of S. exigua from the perspective of integrated pest management.     

Effect of Soil Water on Infectivity and Development of Rotylenchulus reniformis on Soybean,Glycine max

The effect of soil water content on Rotylenchulus reniformis infectivity of ''Lee'' soybean roots was investigated in an autoclaved sandy clay loam. Nematodes were introduced into soil masses maintained at constant soil water levels ranging from 3.4 to 19% by weight. Seedling growth and the soil water content-water potential relationships of the soil were determined. Nematode infectivity was greatest when the soil water content was maintained just below field capacity in the 7.2 (-1/3 bar) to 13.0% (-1/7 bar) ranges. Nematode invasion of roots was reduced in the wetter 15.5 (-1/10 bar) to 19.0% (-1 /2 0 bar) soil moisture ranges and in the dryer 3.4 (-15 bar) to 5.8% (-3/4 bar) soil moisture ranges.     

Influence of Chilling and Freezing Temperatures on Infectivity of Meloidogyne incognita and M. hapla

Egg masses and second-stage larvae of Meloidogyne incognita and M. hapla in soil were exposed to temperatures ranging from 20 to -8 C. Temperature was lowered in 2-day intervals to 16, 12, 8, 4, 0, -4, and -8 C, and the nematodes remained at 4, 0, -4, or -8 C for 18, 14, 10, or 6 days, respectively. Unhatched larvae of both species were more resistant to low temperatures than were embryonic stages. Within the eggs of M. incognita, 7.5% of embryos and 48% of larval stages survived 14 days at 0 C, whereas 9% of embryos and 90% of larval stages in the eggs of M. hapla survived 10 days at -4 C. Second-stage larvae of both species remained infective in sol.1 at 4 or 0 C, but were injured at -4 and -8 C. Infectivily of these larvae was lower in saturated soil than in soil at 51 cm moisture tension at all temperatures.     

柠条细根的空间分布特征及其季节动态

以晋西北黄土区30年生柠条(Caragana korshinskii Kom.)人工林为研究对象,2007年应用Minirhizotron技术,分别在距茎干水平距离0、50、100 cm处设点,对林地0-100 cm土层深度范围内的柠条细根空间分布及其生长季的动态进行了研究。结果表明:(1)生长季柠条细根根长密度(RLD)总平均值为1.3423 mm/cm²。在水平方向上,距茎干水平距离50 cm处分布最多(1.5369 mm/cm²),其次为0 cm处(1.3855 mm/cm²), 100cm处分布最少(1.1044 mm/cm²)。在垂直深度上,各土层RLD平均值大小顺序为40-60 cm>60-80 cm>20-40 cm>0-20 cm>80-100 cm;(2)在0-100 cm土层范围内,月平均RLD在生长季的波动范围为0.4405 2.1040 mm/cm²,其中9月份最多,4月份最少;RLD在5个土层深度3个水平距离处随季节变化均表现先增加后减少的趋势,且不同空间位置RLD峰值变化均在秋季(8 10月份)波动。细根的这种时空分布差异,可能主要受林下土壤资源空间异质性及其季节性变化的影响,但也不排除其它因素的影响(如真菌,植食性昆虫)。     

A 2700-year high resolution pollen record of climate change from varved Sugan Lake in the Qaidam Basin, northeastern Tibetan Plateau

A 2700-year high resolution pollen record from annually-varved Sugan Lake in the Qaidam Basin at 2793 m a.s.l was obtained to examine vegetation and climatic change on the NE Tibetan Plateau. Pollen data shows that Sugan Basin was constantly covered by open desert-steppe vegetation dominated by Chenopodiaceae, Artemisia, Poaceae and Ephedra. However, large variations in Artemisia/Chenopodiaceae (A/C) ratios suggest regional moisture fluctuations over the last 2700 years, including a dry and relatively stable climate prior to 300 AD, relatively wet climate from 300 to 1200 AD with variability during 1100-1200 AD, and unstable climate since 1200 AD with relatively moister climate during 1250-1400 AD and 1700-1800 AD. However, other proxies (varve thickness, Chironomid taxa, isotopes of oxygen in precipitated carbonate) show fresher water when regional moisture was lower inferred from A/C ratio. This inconsistency suggests the possible difference of in-lake lithology/environment and regional moisture change. Fresh water into the lake from ice melting on the surrounding mountains might have contributed to the in-lake lithology and environment variation. The effective moisture changes in the Basin are in opposite phases to snow accumulation records from Dunde ice core (5325 m a.s.l) and to the monsoon intensity inferred from Dongge Cave, suggesting that the regional topography might have played an important role in mediating moisture changes at regional scale. Pollen data from Sugan Lake shows the shift of moisture at 1200 AD, from stable to variable conditions. This event is well correlated with other paleoclimate proxies in China and other parts of the world; however, the mechanisms behind these patterns require further investigation.     

黄土高原半干旱区不同密度山地苹果园水分生产力模拟

采用修订WinEPIC模型,模拟研究了陕西延安和甘肃静宁1965-2009年7种不同密度处理山地苹果园产量和深层土壤水分效应.结果表明：各密度处理4～45年生果园产量均呈现初期快速增加,达到最大值后又逐年波动性降低趋势;果园密度越高,初期产量增加越快,后期产量随降水量年际波动越剧烈.各密度处理果园遭受干旱胁迫规律基本一致,即生长前期无干旱胁迫,随种植年限延长干旱胁迫波动性加剧,生长后期干旱胁迫日数与年降水量波动趋势相反.生长初期,各密度处理果园0～15 m土层逐年土壤有效含水量均呈现波动性强烈降低趋势,延安和静宁分别在17～22年生和13～20年生之后土壤有效含水量维持在0～600 mm的较低水平.各密度处理果园0～15 m土层土壤湿度剖面分布特征相似：均经历了土壤湿度逐年降低和土壤干层逐年加厚的干燥化过程,土壤稳定干层深度可达12 m.基于0～15 m土壤有效水分含量和4～45年果园产量模拟结果确定,延安和静宁果园适宜种植密度分别为650～800和550～700 株·hm^-2.
     

Relationship between Mefluidide Treatment and Abscisic Acid Metabolism in Chilled Corn Leaves

Mefluidide, N-(2,4-dimethyl-5[([trifluoromethyl]sulfonyl) amino] phenyl)acetamide, a synthetic plant growth regulator, was capable of triggering an increase in endogenous free abscisic acid content when corn (Zea mays L.) plants were grown in a nonstress, day/night, temperature regime (26°C) with sufficient moisture supply. The relevance of such an abscisic acid increase prior to chilling exposure and the water relations during chilling are discussed in reference to the mefluidide protection of the chilled corn plants.     

Warming induced tree-growth decline of Toona ciliata in (sub-) tropical southwestern China

Tropical forests play an important role in the global carbon cycle and climate regulation. However, our understanding of how Asian tropical forest growth responds to climatic variations is still limited. We developed tree ring-width chronologies of Toona ciliata from 90 trees (139 cores) from two study regions in the tropical/subtropical forests in Yunnan, southwestern China. Bootstrapped correlation analysis revealed positive moisture sensitivity (precipitation, self-calibrated Palmer drought severity index, relative humidity, and soil moisture) and negative temperature sensitivity of T. ciliata, and the relationship was strongest during dry and/or dry-to-wet transition months, indicating that radial growth of T. ciliata is primarily limited by moisture availability during early growing season. Furthermore, radial growth of T. ciliata was significantly and negatively correlated with the vapor pressure deficit and potential evapotranspiration during dry and/or dry-to-wet transition months. We analyzed long-term growth trends of T. ciliata using ‘size class isolation' (SCI) and ‘generalized additive mixed models' (GAMM) approaches which remove the effects of tree size on tree growth. We detected decreasing growth trend for both approaches at both study regions, indicating that the growth decline of T. ciliata stands in southwestern China is likely due to global warming-induced moisture deficit. The growth of T. ciliata trees is likely to continually decline under projected warming and drying conditions. The observed growth declines of T. ciliata raised concerns about developing sustainable management and conservation programs for tropical/subtropical forests in China.     

Imbibition temperature sensitivity of lima bean seeds controlled by initial seed moisture

Excised embryonic axes and whole seeds of Phaseolus lunatus L. were previously shown to be injured if exposed to low (5°-15°) temperature during the initial stages of imbibition. Present data show that this chilling injury during imbibition of liquid water can be prevented if axes are first allowed to absorb water vapor. The increase of initial water content to 20% increases growth even of unchilled axes, and reduces leaching of 264 mμ absorbing compounds. Protection resulting from increased water content is at first independent of the temperature at which water vapor was absorbed. However, longer exposure of high moisture axes to low temperature results in typical chilling injury. The response to initial seed moisture is repeatedly reversible with changes in water content. Because the same response occurs in intact seeds, it may be possible both to protect them against low temperature injury and to increase vigor by increasing seed water-content prior to planting.     

Germination,survival, and growth of grass and forb seedlings: Effects of soil moisture variability

Seed germination and seedling growth, survivorship, and final biomass and their responses to watering interval were studied in two grass and six forb species to assess germination and seedling growth responses to increased soil moisture variability as might occur with future increases in precipitation variability. Seeds were planted in prairie soil and watered at 1, 2, 4, or 7 d intervals (I). Seed germination peaked at I = 4 d whereas leaf growth in grasses and forbs, and final biomass in grasses peaked at I = 7 d, suggesting that growth and biomass were favored at greater soil moisture variability than seed germination. Biomass responses to I were stronger than the germination responses, suggesting that soil moisture variability more strongly influenced post germination growth. Individual species responses to I fell into three groups; those with responses to I for: (1) seed germination and seedling survival, (2) biomass, or (3) both germination and biomass production. These species groups may be more useful than life form (i.e., grass/forb) for understanding seed germination and seedling dynamics in grasslands during periods of soil moisture variability. Seed germination and early growth may assume more importance in grassland plant community dynamics under more variable precipitation patterns.     

Heat Changes in Maize Storage Influenced by Compound Factors; Different Levels of Maize Weevils,Broken Corn and Foreign Materials,and Moisture Contents

Effect of Sitophilus zeamais Mostschulsky infestation on the heat changes of maize at 13, 16, and 19% moisture content with 0, 5, and 10% broken corn and foreign material was studied in 1.81 thermos containers. Containers with infested and uninfested maize were held in a chamber at 26.6°C and 60±5% r.h. for 80 d. Temperatures were measured continuously using a datalogger system. At 13 and 16% moisture content, more grain heating was recorded in infested than in uninfested maize. Presence of insects and moisture content level were major factors in grain heating during storage. Level of BCFM did not significantly affect the grain heating. At 19% moisture content, grain heating increased in all treatments. Heating appeared to be more related to microbial growth than to insect activity, and accumulated to 26.5–37 kj/kg maize at 3–4 wk. The growth of the maize weevil population was significantly affected by grain moisture content. The greatest number of offspring after 80 d was recorded in the 13% moisture content trial. At 19% moisture content, there were more dead than live insects.     

Crucial importance of length of fatty-acyl chains bound to the sn-2 position of phosphatidylglycerol for growth and photosynthesis of Synechocystis sp. PCC 6803

Phosphatidylglycerol (PG) in thylakoid membrane is essential for growth and photosynthesis of photosynthetic organisms. Although the sn-2 position of PG in thylakoid membrane is exclusively esterified with C₁₆ fatty acids, the functional importance of the C₁₆ fatty-acyl chains at the sn-2 position has not been clarified. In this study, we chemically synthesized non-metabolizable PG molecules: we introduced linoleic acid (18:2, fatty acid containing 18 carbons with 2 double bonds) and one of the saturated fatty acids with different chain length (12:0, 14:0, 16:0, 18:0 and 20:0) by ether linkage to the sn-1 and sn-2 positions, respectively. With the synthesized ether-linked PG molecules, we checked whether they could complement the growth and photosynthesis of pgsA mutant cells of Synechocystis sp. PCC 6803 to understand the importance of length of fatty chains at the sn-2 position of PG. The pgsA mutant is incapable of synthesizing PG, so it requires exogenous PG added to medium for growth. The growth rate and photosynthetic activity of mutant cells depended on the length of fatty chains: the PG molecular species binding 16:0 most effectively complemented the growth and photosynthesis of mutant cells, and other PG molecular species with fatty chains shorter or longer than 16:0 were less effective; especially, those binding 12:0 inhibited the growth and photosynthetic activity of the mutant cells. These data demonstrate that length of fatty chains bound to the sn-2 position of PG is critical for PG performance in growth and photosynthesis.     

Infectivity,Development, and Reproduction of Heterodera cajani on Pigeonpea: Influence of Soil Moisture and Temperature

The effect of soil moisture on penetration, development, and reproduction of Heterodera cajani on pigeonpea (cv. ICPL 87) was investigated in growth chambers held at 20 and 25 C, and in a greenhouse where temperature fluctuated between 25 and 32 C. Averaged across temperatures, the percentage of juveniles that penetrated roots was 34.3, 31.8, 8.8, and 3.7% at 24, 32, 16, and 40% soil moisture levels, respectively. Numbers of females per root system 4 weeks after infesting soil with second-stage juveniles was 79.6 at 24%, 65.3 at 32%, 26.1 at 16%, and 2.9 at 40% soil moisture. Nematode reproduction was greatest (P = 0.001) at 24% soil moisture and 25 C. Reproductive factor was 19.4 at 24%, 15.2 at 32%, 5.7 at 16%, and 0.5 at 40% soil moisture level. Nematode penetration, development, and reproduction at different moisture levels were greater (P = 0.01) at 25 and 25-32 C than at 20 C. Plant growth was retarded at 40% soil moisture and 20 C in comparison to that at 24 and 32% moisture levels and 25 C. This information on influence of temperature and soil moisture will be helpful in developing models for predicting changes in H. cajani densities in pigeonpea fields during rainy and postrainy dry seasons in the semi-arid tropics.     

陇中黄土高原半干旱区苜蓿地土壤干燥化特征及适宜种植年限

研究了陇中黄土高原半干旱区不同种植年限紫花苜蓿地土壤水分特征及适宜种植年限.结果表明： 3、8、12和14年生苜蓿地0～300 cm土层土壤平均含水量均明显低于当地土壤稳定湿度值.12和14年生苜蓿地0～300 cm土层土壤含水量仅为9.2%和7.1%,甚至低于作物有效水分下限.1、3、8、12和14年生紫花苜蓿地0～300 cm土层干燥化指数分别为125.4%、30.5%、18.4%、-34.2%和-83.3%,除1年生苜蓿地土壤无干燥化现象之外,其余种植年限苜蓿地土壤均呈不同程度的干燥化.随苜蓿种植年限的延长,土壤干燥化程度加剧,但干燥化速率呈减缓趋势.综合苜蓿生产力动态和土壤水分状况,该区紫花苜蓿适宜的种植年限为8～10 年.     

平茬对半干旱黄土丘陵区柠条林地土壤水分的影响

半干旱黄土丘陵区多年生柠条人工林地发生土壤旱化,研究柠条林平茬对土壤水分影响对于防治土壤旱化具有重要意义。采用中子仪测定土壤水分,对未平茬和平茬柠条林地土壤水分进行测定,分析了平茬对土壤水分的影响。结果表明:未平茬和平茬柠条林地降雨补给量(R₁,R₂)同降雨量(P)显著正相关(P<0.05)。定义降雨耗损量(林冠截留量和地表径流之和)占降雨量的百分比为降雨耗损率,未平茬林地降雨损耗率(L₁)和平茬柠条林地降雨损耗率(L₂)分别与其降雨前土壤表层(0-20 cm)含水量(S₁,S₂)呈明显指数关系(P<0.05):L₁=2.54exp(0.22S₁),L₂=2.40exp(0.27S₂),表层含水量相同时,平茬林地降雨损耗率明显高于未平茬林地。平茬后,林地降雨最大入渗深度减小,土壤水分利用深度减小;短时间内(2个月左右)林地20-160 cm含水量增加,之后平茬林地土壤含水量与未平茬林地土壤含水量接近;丰水年和丰水年后的第一年,平茬林地含水量低于未平茬林地,0-400 cm土壤储水量比未平茬林地最多低45.9 mm。平茬后200-400 cm土层土壤水分有少量增加,但是0-200 cm土层土壤含水量损失更严重。平茬3a后,平茬对柠条林地土壤水分的影响减弱。     

Anhydrobiosis in Pratylenchus penetrans and Tylenchorhynchus n. sp. in Cultivated Soils Cropped to Winter Rye

Anhydrobiotes of Pratylenchus penetrans were found in two cultivated soils sown to rye in southern Ontario during the growing season. Anhydrobiotes at the 0-2.5-cm depth were recovered from 9 and 6 of 11 samplings, respectively, of a Vineland silt loam and a Fox loamy sand during the dry summer of 1983. At the 2.5-15.0-cm depth, anhydrobiotes were recovered less frequently. In the summer of 1984, anhydrobiotes of P. penetrans were recovered once and anhydrobiotes of Tylenchorhynchus n. sp. twice in 11 samplings. The percentages of P. penetrans populations that were anhydrobiotes in 1983 and 1984 were closely related to soil moisture content and corresponding moisture tensions. Populations of P. penetrans were greatest in October in the lower soil depth, 2.5-15.0 cm; those of Tylenchorhynchus n. sp. were greater in the surface layer of soil, 0-2.5 cm, and peaked in August.