Growth response to different constant soil moisture levels in maize (Zea mays L.) during the vegetative phase

The effect of different constant soil moisture levels (90, 60, 30% and 90, 60, 40% respectively, of the maximum capillary capacity) on the vegetative growth of maize was studied by the methods of growth analysis. The constant soil moisture in vegetation pots was maintained by means of the injection method. The constantly decreased soil moisture was applied in one experiment just from the sowing of germinated corns and in the other from the phase of 4–6 leaves. In both the cases plants responded to the different soil moisture levels by a progressively lower growth rate of the total dry weight according to the degree of soil moisture lowering. When the constant soil moistures were applied from the sowing, the differences in the relative growth rate (R.G.R.) were caused mainly by lower leaf area ratio (L.A.R.) values. In the case of constantly lowered soil moistures from the phase of 4–6 leaves, the differences in R.G.R. were caused by lower net assimilation rate (N.A.R.). When the constant soil moisture of 40% was applied from the sowing, the changes in N.A.R. showed the characteristic features of adaptation to unfavourable conditions.     

The effect of constant moisture and aeration levels in soil on Fusarium wilt of tomatoes

Soil patches on opposite sides of Pseudoroegneria spicata plants in the field were treated with either distilled water or a nutrient solution containing N, P, or K. Roots from these enriched and control patches were tested three days later for their capacities of ammonium, phosphate, and potassium uptake. When phosphate was augmented in the enriched patches, rates of phosphate uptake increased significantly, but not rates of ammonium or potassium uptake. When the enriched patches were augmented with nitrogen, uptake capacities of both ammonium and potassium increased significantly (mean increases of up to 88% and 71% for ammonium and potassium, respectively). Potassium augmentation did not lead to increased soil-available K and, correspondingly, did not induce changes in the capacity for uptake of K, N, or P. The potential importance of nutrient uptake kinetics in the exploitation of nutrient-rich soil patches is discussed.     

Effect of different constant soil moisture levels on net assimilation rate,relative transpiration,osmotic pressure of cell sap and water saturation deficit of the leaves

A study was made of the effect of different constant soil moisture (90, 60 and 30 or 40% maximum capillary capacity) on the net assimilation rate (N.A.R.) in maize in relation to changes in relative transpiration (R.T.), water saturation deficit of the leaves (W.S.D.) and osmotic pressure of the cell sap (O.P.). The soil moisture was maintained constant either from the planting of the germinating grain, or from the phase of 4–6 leaves. An attempt was made to interpret the mechanism of action of water deficit on photosynthesis and at a rough differentiation between the indirect effect through changes in internal diffusive resistance to carbon dioxide and the direct effect on the hydration of the photosynthetizing tissue. In plants exposed to different constant soil moisture levels from the phase of 4–6 leaves, the initial difference in N.A.R. corresponding to the degree of lowering of soil moisture gradually evened out during the vegetation season. On applying different constant soil moisture levels from the time of planting no marked differences in N.A.R. were found between plants cultivated at high values of soil moisture (60% and 90%). In plants cultivated from planting at 40% soil moisture, the course of changes in N.A.R. was qualitatively different from that of the above two variants and corresponded more or less to changes characteristic for the process of adaptation to unfavourable conditions. From the analogous course of N.A.R. and R.T. it can be assumed that in all cases the intensity of photosynthesis was very markedly influenced by changes in diffusive resistance to carbon dioxide. On the basis of an analysis of changes in O.P. of the cell sap and W.S.D. of the leaf tissue, the assumption was made that in plants cultivated from planting at 40% and to some extent at 60% soil moisture, irreversible adaptation changes occurred in the structural conditions of photosynthesis as a result of continuous dehydration. In plants cultivated at similar soil moisture levels from the phase of 4–6 leaves, the changes in the intensity of photosynthesis were more likely caused by actual dehydration of the photosynthetizing tissue.     

Growth of three species ofBidens under different levels of soil moisture content

By the assumption that both soil moisture and soil air affect plant growth as linear factor, the relationship between mean plant dry weight and soil moisture content was newly formulated. Its applicability to actual growth data was tested by growing three species ofBidens under different levels of soil moisture content. The growth data ofBidens well satisfied the new formula. The optimum soil moisture content giving a maximum mean plant dry weight was the largest inB. frondosa and the smallest inB. biternata. This result well agreed with field observations. The growth factor represented by the new formula was referred to as “repulsive factor”, and the difference between the repulsive factor and optimum factor was discussed.     

Effect of maize canopy and water repellency on moisture patterns in a Dutch black plaggen soil

Man-made raised sandy soils in the Netherlands are classified as brown or black plaggen soils. When dry, the brown soils are wettable, but the black soils are water repellent. For one growing season, transects were sampled in a maize cropped black plaggen soil at the Heino experimental farm. Due to interception and stemflow, water was concentrated near the roots of the maize. Between the maize rows, higher soil water contents were found in microdepressions, due to rainwater dripping to the ground from overhanging leaves. Redistribution of soil water from wet to dry areas was restricted by the water repellency of the dry sand. As a consequence, there was a distinct variation in soil moisture content. These irregular wetting patterns did not induce preferential downward flow, but widened over time; because the dry, water repellent subsoil impeded and resisted infiltration into the deeper subsoil.     

The maintaining of constant soil moisture levels (lower than maximum capillary capacity) in pot experiments

The “injection method” is recommended for maintaining a constant soil moisture at values lower than maximum capillary capacity in pot experiments. The appropriate amount of water is injected into the soil by means of a puncture needle connected with a syringe. The reliability of the above method in relation to the uniformity of the vertical and horizontal distribution of soil moisture was tested in pot experiments with maize. The fortuity of the changes in the soil moisture distribution within the scope of the given variability restricts the “growth of roots towards the water”.     

不同土壤水分条件下容重对玉米生长的影响

用玉米作为实验材料。进行分根实验研究不同土壤水分条件下容重对玉米生长的影响,种子根平分在装有塿土的分隔的白铁皮桶中,土壤容重分4种处理：低容重(两边容重都为1．20g·cm^-3)、中容重(两边容重都为1．33g·cm^-3)、高容重(两边容重都为1．45g·cm^-3)和混合容重(一边为1．20g·cm^-3,另一边为1．45g·cm^-3),土壤水分控制在高基质势(-0．17MPa)和低基质势(-0．86MPa)两个水平,结果表明,当植株生长在紧实土壤或土壤基质势从-0．17MPa降到-0．86MPa时。根长、根干重和地上部干重都显著降低,并且地上部干重的降幅更大,紧实土壤使根长降低的同时还使根的直径增大,无论是容重增大还是土壤水分含量降低所引起的高土壤阻力都使叶片扩展速度降低和植株变小,生长在紧实土壤中的植株变小不仅是因为叶片扩展速度降低,同时是成熟叶片叶面积缩小的结果。然而,当植株生长在混合容重土壤中时,处在低容重土壤中的根系生长得到加强,补偿甚至超补偿高容重土壤中根系生长的不足,整个植株的生长状况与低容重土壤中生长的植株接近。     

Effects of constant and fluctuating soil temperature on growth,development and nutrient uptake of maize seedlings

Summary The effect of constant and fluctuating soil temperature and two soil moisture regimes on the growth, development, transpiration and nutrient uptake by maize seedlings was studied in a greenhouse investigation. The constant root temperatures were maintained at 30, 34, 35, 36, 37, and 38°C for both 250 and 750 cm of soil moisture suctions. The fluctuating root temperature, for 250 cm of soil moisture suction only, of 30–35, 30–39, 30–40, 30–45 and 30–48°C were maintained to simulate the soil temperature regime under field conditions. The constant root temperature of 35°C and fluctuating temperature between 30–40°C significantly decreased the shoot and root growth and transpiration rate. On the average, there was 1.3 and 0.7 g decrease in fresh shoot weight and 0.36 and 0.30 g in fresh root weight per degree increase in root temperature for 250 and 750 soil moisture suction, respectively. In general, the effect of high soil moisture suction on maize seedlings was more severe when at high root temperature. The shoot and root concentration of N, P, and K decreased while that of B increased with increase in root temperature. The root concentration of Zn also decreased with increase in root temperature.     

Effect of soil moisture on bioremediation of chlorophenol-contaminated soil

A chlorophenol-contaminated soil was tested for the biodegradability in a semi-pilot scale microcosm using indigenous microorganisms. More than 90% of 4-chlorophenol and 2,4,6-trichlorophenol, initially at 30 mg kg^–1, were removed within 60 days and 30 mg pentachlorophenol kg^–1 was completely degraded within 140 days. The chlorophenols were degraded more effectively under aerobic condition than under anaerobic condition. Soil moisture had a significant effect with the slowest degradation rate of chlorophenols at 25% in the range of 10–40% moisture content. At 25–40%, the rate of chlorophenol degradation was directly related to the soil moisture content, whereas at 10–25%, it was inversely related. Limited oxygen availability through soil agglomeration at 25% moisture content might decrease the degradation rate of chlorophenols.     

Zinc sources for rice in soil at different moisture regimes and organic matter levels

Summary Laboratory incubation experiment was conducted with a clay loam alluvial lowland rice soil to study the relative effectiveness of two sources of Zn (ZnEDTA and ZnSO₄) in maintaining Zn availability in soil under two moisture regimes (saturated and waterlogged) both in presence as well as absence of added organic matter. The results showed that ZnEDTA was always more effective than ZnSO₄ in maintaining higher amount of zinc in available form in soil for a longer perid. Results of greenhouse experiment conducted with rice showed that concentration and uptake of Zn by roots were generally higher with ZnEDTA than with ZnSO₄ both in presence and absence of added organic matter, whereas in respect of shoot this was true only in absence of added organic matter.     

Effect of different seed moisture levels on the germination behaviour ofPhaseolus trilobus Ait

Germination inPhaseolus trilobus is controlled by different moisture levels of seeds. The hard seed coatedness which develops secondarily can be removed by pretreatment with oonc. H₂SO₄. This also enhanced the onset of seed germination.     

Effect of soil moisture at different temperatures on Rhizoctonia root rot of wheat seedlings

The effect of soil moisture at different temperatures on root rot of wheat seedlings caused by Rhizoctonia solani AG-8 was studied in temperature controlled water tanks under glasshouse conditions. Four moisture levels (15, 30, 50 and 75% of soil water holding capacity at saturation which were equal to –10, –7, –5 and –3 kPa, respectively) were tested in tanks maintained 10, 15, 20 or 25 °C. The role of microbial activity in the effect of soil moisture and temperature on disease severity was also studied by including treatments of steam treated soil. Results showed that at soil moisture levels optimum for plant growth (50 and 75% WHC) disease was more severe at a lower temperature (10 °C), but under relatively dry conditions (15% WHC) disease levels were similar at all temperatures tested. In warm soils (20 and 25 °C) at high soil moisture levels (50 and 75% WHC), disease was more severe in steam treated soil than in non-steam treated soil, indicating that the suppression of disease in natural soil under these conditions was associated with high soil microbial activity.     

Growth and development of maxipak wheat as affected by soil salinity and moisture levels

The effect of soil salinity and soil moisture on the growth and yield of maxipak wheat (Triticum aestivum L.) was studied in a lath-house experiment in whih, chloride-sulphate salt mixtures were used to artificially salinize a sandy loam soil from Al-Jadyriah Baghdad. Five soil salinity levels of ECe's equal to 1.7 (Control) 4.2, 5.8, 8.1, 9.4 and 11.0dSm^–1 were prepared and used at 3 levels of available soil moisture depletion, namely, 25, 50, and 75% as determined by weight. Both growth (vegetative) and yield components were studied throughout the growing season.Results showed that increasing the soil salinity from 1.7 to 11.0 dSm^–1, and decreasing the available soil water from 75 to 25% resulted in independent and significant decreases in Mazipak wheat growth and yield components at different stages of plant development. Root growth showed more sensitivity to both available soil water and soil salinity level than other components. It has been concluded that at soil salinity levels of more than 8.0 dSm^–1, available soil water became a limiting factor on wheat growth and the maintenance of 75% of available soil water during the growth period is recommended to obtain satisfactory grain yield.     

Effect of varying static and changing moisture levels during incubation on extractability of soil phosphate

Summary A sandy loam (pH 6.5) was incubated at 28°C at static moisture levels, ranging from 10 per cent saturation to 133 per cent saturation (waterlogging), for 6 and 12 weeks; other samples covering the same moisture range were first incubated for 6 weeks, and after changing all moisture levels to 50 per cent saturation were incubated for a further 6 weeks.With increasing static soil moisture level during incubation there was a slight reduction in Morgan-extractable phosphate up to 70 per cent saturation, but thereafter, due to anaerobic effects, there were considerable increases in extractable phosphate with increasing moisture level.With changing moisture level during incubation the effects of anaerobiosis became apparent where original moisture level was greater than 50 per cent saturation; extractable phosphate was reduced to levels lower than those occurring where the soil was maintained continuously at 50 per cent saturation. The extent of reduction in extractable phosphate increased with original soil saturation level.     

施氮量对小麦/玉米带田土壤水分及硝态氮的影响

通过田间试验研究了河西绿洲灌区典型的小麦/玉米间作群体不同施氮量(0、210、420和630 kg/hm2)对小麦、玉米带田土壤水分和硝态氮(NO3(-)-N)的动态的影响.结果表明:小麦/玉米总籽粒产量随着施氮量的增加而增加,但当施氮量超过420kg/hm2时,总籽粒产量不再随施氮量增加而增加,最高总籽粒产量可达13661-14668 kg/hm2.水分利用效率在施氮420 kg/hm2时最高可达21.25 kg·hm-2·mm-1.小麦收获后,0-120 cm土层内土壤含水量随施氮量增加而减少,NO3(-)-N的累积量随施氮量增加而增加,并且表层土壤(0-60 cm) NO3(-)-N含量明显高于深层土壤(60-200 cm).在小麦/玉米整个生育期,土壤硝态氮的变化呈双峰曲线.施氮0和210 kg/hm2的土壤硝态氮第一峰值和第二峰值均分别出现在小麦三叶期和玉米大喇叭口期;施氮420和630 kg/hm2的土壤硝态氮第一峰值出现在小麦挑旗期,第二峰值分别出现在玉米大喇叭口期和玉米灌浆期.因此,在该地区小麦/玉米间作栽培模式下,施氮水平控制在420 kg/hm2时,使混合产量达到最高,同时可减轻土壤硝态氮的累积和运移,从而达到高效、安全的目的.     

旱作农田不同耕作土壤呼吸及其对水热因子的响应

为研究旱作农田春玉米生育期不同耕作土壤呼吸变化特征及其对水热因子的响应情况,在山西省寿阳县旱农试验基地采用红外气体分析法测定了传统耕作(CT)、少耕(RT)和免耕(NT)土壤呼吸速率,并同步测定了各土层土壤水分、温度.研究表明:在春玉米生育期内,土壤呼吸速率均呈单峰型变化趋势,峰值出现在8月;传统耕作与少耕土壤呼吸速率变化趋势基本一致,而免耕土壤与前两者相比波动幅度较大;土壤呼吸峰值与水分、温度之间无明显相关,其余时期土壤呼吸与水分、温度因子具有良好的相关性;双因子模型较单因子模型能更好的描述土壤呼吸与水分、温度之间关系,基于水热双因子(10-20 cm)的指数-幂模型能够解释土壤呼吸变化的81％-87％ (P＜O.01);3种耕作土壤呼吸对水热因子协同影响的敏感性表现为CT＞NT＞RT.     

Suction force variation in double-hybrid maize as a function of soil moisture

In experiments with double-hybrid maize grown in the field and in a greenhouse, we analysed the value of the suction force as related to the regime of irrigation. The results showed that the level of water supply to the plants is in good connection with the value of the suction force and the coefficient H (the relative degree of water saturation of the cells) analysed at the same time. In the case of the 2 hybrids under investigation the highest value of coefficient H was found to be between 35–48. The data indicate that the use of these two indices should take part in a physiological method for the settlement and the application of water rules in irrigation.     

Growth and survival of Pseudomonas putida strains degrading naphthalene in soil model systems with different moisture levels

The effect of different moisture levels (from 20 to 70%) on the growth and survival of Pseudomonas putida strains G7 and BS3701 degrading naphthalene was studied in soil model systems. P. putida G7 contains plasmid NAH7 and P. putida BS3701 harbours plasmids pBS1141 and pBS1142. A mathematical model is proposed to describe the observed dynamics of the number of viable bacterial cells. Naphthalene and soil organic matter were considered as substrates available to bacteria. Data fitting allowed the estimation of model parameters characterizing microbial growth rate, utilization rate of substrates, specific maintenance rate and yield coefficient. Both the maximum bacterial concentration and the highest yield coefficient were observed at a soil moisture level of 40%. This optimal moisture level is close to but less than the water capacity (48%) of the soil used.     

Effect of soil moisture stress on legume-rhizobium symbiosis in soybeans

Summary In a pot culture experiment, the influence of soil moisture stress at different physiological stages of soybean, cv. Hark, on nodulation, symbiosis and nitrogen accumulation was studied. Moisture stress reduced leghemoglobin content of root nodules and nitrogen uptake by plants. It had no effect on number of bacteroids. Stress at mid bloom and rapid pod filling stages reduced yield and seed protein content. However, these parameters were not affected by stress at nodule initiation and early flowering stages, though, flower initiation and maturity of the plant were delayed. Moisture stress at any stage did not alter nitrogen status of roots.