Aufnahme und Verlagerung von 42K und 86Rb bei jungen Gerstenpflanzen in Abhängigkeit von einer Calcium-Behandlung der Wurzeln

Uptake and translocation of ⁴² and ⁸⁶Rb by young seedlings in relation to different calcium levels in the root medium The uptake of ⁴²K and ⁸⁶Rb by 8-d.-old barley seedlings was studied after 4 h period in solutions containing either ⁴²K or ⁸⁶Rb (1 mmol ⁴²KNO₃ + 1 mmol KCl; 1 mmol ⁸⁶RbCl + 1 mmol RbNO₃). The amount of ⁴²K was 56% and 20% higher than that of ⁸⁶Rb in the roots and shoots respectively (Pict. 1). Increasing the level of Ca in the root medium enhanced ^{42 86}Rb uptake. However the translocation rate of ⁸⁶Rb in the shoot was relatively lower than that of ⁴²K. In view of the content in the roots both elements were translocated to the shoot in a similar percentage (Table 1).     

Zur Abhängigkeit des Bodenwasserpotentials von der Temperatur

Soil-water-potentials depending on temperature The soil-water-potential · of different soils has been measured in dependence of temperature. Between about — 0.2 · 10⁶ and — 0.7 · 10⁶ erg cm^?3 (corresponding to a pressure head of 2 resp. 7 m water) all soils show a significant dependence of the soil-water-potential on temperature always in connection with hysteresis phenomena. With soils rich in clay or sand the dependence is most pronounced. At very high suction values (< — 0.7 · 10⁶ erg cm^?3) the dependence becomes small. Thus the measurements agree well with psychrometric evaluations of Campbell and Gardner (1971) on the no-temperature-dependence of the soil-water-potential in the range of about — 3 ·10⁶ to — 20 ± 10⁶ erg cm^?3.     

Zusammenhang zwischen hydraulischer und mechanischer Bodenstabilität in Abhängigkeit von der Belastungsdauer

Interaction between mechanically and hydraulically affected soil strength depending on time of loading Soil‐deformation analysis often only considers the direct effects of mechanical stress on changes in void ratio or pore functions while the interaction between hydraulic and mechanical processes is seldomly mentioned. Thus, we analyzed the effect of mechanical stress and time of soil settlement on changes in soil strength and the corresponding interactions between stress‐dependent changes in pore water pressure on precompression stress for a clayey silt. Disturbed samples with a bulk density of 1.4 g cm^–3 and a water content of 25 g (100 g)^–1 were compressed for four time steps (10–240 min) at eight stresses (20–400 kPa) with four replications. During the experiments, the changes of pore water pressure and void ratio were registered. With increasing time of stress application, we determined an increased soil strain. The higher the stress‐application time, the smaller gets the void ratio and the precompression stress value. Parallel to these variations in settlement, we also found changes in the pore‐water‐pressure values. This is a consequence of decreasing pore diameter while the water saturation increases. Thus, the proportion of neutral stresses on total stress increases which coincides with a change of water suction (= unsaturated) conditions up to even positive pore‐water‐pressure values (from less negative to positive pore water pressure values). From our experiments, we can conclude that the changes in pore‐water‐pressure values already occur at normal stress values smaller than the precompression stress. This underlines the increasing sensitivity of soil deformation processes close to the internal soil strength. The results support the idea, that in order to quantify the mechanical strength of structured unsaturated soils, we always have to determine the changes in pore‐water‐pressure values, too.     

Dicyandiamidabbau im Boden in Abhängigkeit von der Temperatur

Effect of temperature on the breakdown of dicyandiamide in the soil The breakdown of dicyandiamide in a soil (sandy silty loam, pH 6.2, 0.13 % N) was investigated in relation to temperature. 1. The rate of conversion of dicyandiamide (DCD) (20 mg DCD-N/100 g soil) to guanylurea increased with rising temperature (10°–90°C). After 20 days, 14–100 % of the added DCD was metabolized. Small amounts of DCD (0.67 resp. 1.34 mg DCD-N/100 g soil) were broken down completely within 20–80 days at 8°–20°C. 2. Guanylurea was transformed to guanidine and then to ammonium. Increasing temperature in the region of 10° and 30°C accelerated the transformation. At higher temperatures (up to 70°C) an accumulation of guanidine occurred.     

Stickstoffernährung und Al-Toxizität bei Buchenjungpflanzen. I: Entwicklung von Buchenjungpflanzen in Abhängigkeit von der Form der Stickstoffernährung und dem Aluminiumgehalt der Nährlösung

Nitrogen nutrition and Al toxicity with young beech plants. I: Development of young beech plants in relation to the source of nitrogen and the Al content of the nutrient solution Young beech plants were grown in aerated nutrient solutions with different Al concentrations over a period of 14 weeks. Nitrogen was supplied in either NO₃- or NH₄-form. pH-changes of the solutions were either corrected to the initial pH of 4 after two days, or not corrected over a period of two weeks. Root growth of the beech seedlings was inhibited by Al. Reduction of root length and dry matter production was more severe if the plants were fed with ammonium nitrogen compared to nitrate nitrogen. Detrimental effect of Al on root growth was also influenced by the pH of the solution. NH₄-N-nutrition led to pH decrease and therefore to increased solubility and toxicity of aluminium. On the contrary, NO₃-N-nutrition weakened Al toxicity because of pH increase at the root surface and in the AFS. This led to an inactivation of Al in the form of insoluble hydroxy aluminium polymers. Compared to NO₃-N-nutrition NH₄-N promoted shoot growth. During 14 weeks no detrimental effect of Al on shoot growth was observed.     

Der Wasserhaushalt von Fichte in Abhängigkeit von Boden und Atmosphäre

The water regime of spruce in relation to soil and atmosphere Simple observations of the water regime of potted spruce trees and measurements in the field are reported, followed by a discussion of spruce water potential in relation to soil and atmosphere water potentials. When the soil is sufficiently moist water regime of spruce is determined by the atmosphere. As higher the atmospheric demand and as lower the hydraulic conductivity of the soil as more difficult it is for a spruce plant to supply transpired water and more and more the potential transpiration rate is reduced. For short term aspects water storage in leaf tissues is of high importance. Observations show the possibility of water uptake by needles if wetted by rain or dew. The maximum amount of this way of water absorption is also given by the internal storage capacity.     

Wasserhaushalt und Dickenwachstum von Kiefern in Abhängigkeit des Grundwasserflurabstandes

Water budget and annual ring growth of pines for different groundwater depth conditions Relation between annual ring width and water supply was examined for different groundwater depth in an old pine stand on a sandy soil. The quotient Ereal/Epot is a suitable parameter to quantify water stress. Multiple regression analyses were used to describe the dependence between annual ring width and water stress. Mean growth of basal area can be expressed by Ereal/Epot of the actual and previous year. This site specific function was used to quantify growth reduction affected by ground-water lowering for various soil conditions.     

Stärkegehalte von Kartoffelknollen in Abhängigkeit von Kalium-Ernährung und Knollenentwicklung

Starch content of potato tubers in relation to K nutrition and tuber growth In a pot experiment with potato (cv Saturna) K content in tubers increased from 1.0 to 2.6 % of tuber-DM due to increasing rates of K fertilizer. Simultaneously starch in tuber fresh matter decreased from 21 to 15 %. Highest starch content in tuber dry matter was obtained in that K treatment which gave the highest yield in dry tubers. Measuring starch accumulation during tuber growth revealed that already in the flowering stage differences exist in the starch contents of the tuber dry matter between the lowest and highest K treatments, namely 69 % for K₁ as compared with 64 % for K₅. The rate of starch accumulation between flowering and final harvest, however, was similar in all K treatments. This suggests that K supply affects the storage tissue at an early stage of tuber development probably via different water relations of tubers.     

Umsetzung von Cyanamid,Harnstoff und Ammonsulfat in Abhängigkeit von Temperatur und Bodenfeuchtigkeit

Transformation of cyanamide, urea and ammonium sulfate as influenced by temperature and moisture of soil The conversion of cyanamide, urea and ammonium sulfate solutions to nitrate was investigated in a sandy silt loam (pH 6.2) in relation to temperature and soil moisture conditions. 1. Cyanamide was transformed to urea within 1–5 days. Increasing temperature (2°–100°C) accelerated the breakdown, whereas high moisture conditions (120 % of total water capacity) decreased transformation. 2. The hydrolysis of urea to ammonia took place within 5–10 days even at 2°C regardless of whether cyanamide or urea was added. Low soil moisture (40 % of total water capacity) and high temperature (up to 50°) accelerated the breakdown. 3. Following urea application (20 mg N) there was a transient formation of up to five times more nitrite (0.5 mg NO₂-N) as compared with cyanamide or ammonium sulfate treatments. 4. Clear differences were observed in the rates of nitrification. The rate was greater for urea than for cyanamide and ammonium sulfate. The formation of nitrate began at 2°C, with an optimum between 20° and 30°C. Under flooded conditions (120 % of total water capacity) and low temperature the rate of nitrification was slow. At higher temperatures rapid denitrification took place.     

Der Bulk-Stomata-Widerstand von Ackerbohnen und seine Abhängigkeit vom Bodenwassergehalt

Bulk stomatal resistance of Vicia faba and its dependence on soil water content Bulk stomatal resistance of beans (Vicia faba L.,) as a function of soil water content was estimated for 41 days by comparison of potential transpiration, determined from meteorological data, and actual transpiration, determined from soil water losses. The resistance of beans is about 46 s/m if soil water content is above 70 % of available field capacity and increases strongly in dryer situations. This behaviour can be described by an exponential function.     

Stickstoffernährung und Al-Toxizität bei Buchenjungpflanzen. II: Mineralstoffgehalte junger Buchen in Abhängigkeit von der Form der Stickstoffernährung und dem Al-Gehalt der Nährlösung

Nitrogen nutrition and Al toxicity with young beech plants. II: Mineral contents of young beech plants in relation to the source of nitrogen and the Al content of the nutrient solution Young beech plants were grown in aerated nutrient solutions with different Al concentrations over a period of 14 weeks. Nitrogen was supplied in either NO₃ or NH₄-form. pH-changes of the solutions were either corrected to the initial pH of 4,0 after two days, or not corrected over a period of two weeks. The cation contents of the roots and shoots were greater if the nitrogen was supplied in NO₃-form. Increasing Al concentrations in the nutrient solutions led to an increase in Al contents and a decrease in Ca- and Mg-contents in roots and shoots.     

Aufnahme und Verlagerung von 15N-Stickstoff bei Sommergerste in Abhängigkeit von K-Ernährung und Mehltaubefall

¹⁵N uptake and distribution by spring barley in relation to K nutrition and mildew attack Barley cv. Aramir was grown in complete nutrient solution containing 0,5 (K₁), 1,5 (K₂) and 4,5 mM K (K₃) respectively till maturity. Part of the plants was infected by mildew (Erysiphe graminis), whereas control treatments were kept mildew-free by fungicide sprays. Symptoms of mildew attack were less at K₂ and K₃ and grain yields of infected plants were raised from 98 (K₁) to 160 (K₂) and 165 g/pot (K₃). In control treatments grain yields were 130 (K₁), 164 (K₂) and 163 (K₃) g/pot. During anthesis nitrogen in the nutrient solution was labelled with ¹⁵N for two days and ¹⁵N metablism was studied within 7 consecutive days. The aim of this pulse-chase experiment was to find out, how mildew attack and K nutrition influence N metabolism. The following results were obtained: a) ¹⁵N uptake increased from K₁ to K₂ in infected and healthy plants, though at slightly lower levels in the infected treatments. b) During 7 days after the ¹⁵N pulse up to 17,1% of the ¹⁵N absorbed were translocated into the grains. Better K status as well as spray treatments stimulated nitrogen translocation. c) Mildew attack of leaves does not seem to influence the conversion of grain-¹⁵N into grain proteins. Better K supply stimulates the rate of protein synthesis in the grain. d) In mildew infected leaves relatively more of the ¹⁵N absorbed is incorporated into leaf proteins. But this may be a consequence of slower grain growth, because already 7 days after anthesis infected plants in all K treatments had significantly lower grain yield. In spite of the short duration of the experiment the ¹⁵N data do not indicate that the visible depression of mildew attack by better K nutrition of the crop might inter alia be due to K stimulated defense reactions within N metabolism. This is in agreement with a previous experiment.     

Die Phosphatmobilität im Hochmoorboden in Abhängigkeit von der Düngung

Phosphate mobility in relation to fertilizing effects in raised-bog peat The phosphate solubility of raised-bog peat soils is very different from the phosphate solubility of mineral soils. Compared to mineral soils the losses of phosphates by leaching are 10 to 20 times higher. This mobility of phosphates is destined by the quantity, kind and time of fertilizing, land use (grassland or arable land) and fertilizing technique. Field and lysimeter trials with raised-bog peat soils show: 1. Water soluble phosphates are quickly translocated and leached. 2. Water insoluble phosphates are quickly solved and leached in raised-bog peat soils. The mobility of the phosphates decreases with increasing pH-value of the top soil and topdressing. At a pH-value of 4,O nearly 80% of Thomasphosphat and nearly 70% of Hyperphos phosphates are leached in lysimeter trials; at pH-value of 4 3 only 17 % of Thomasphosphat and 15 % of Hyperphos phosphates are leached. 3. To minimize leaching losses phosphate fertilizingin spring is recommended to reduce the phosphate leaching. 4. The phosphate leaching in grassland is twice or thrice less than in arable land.     

Ermittlung bodenphysikalischer Kennwerte in Abhängigkeit von Bodenart,Lagerungsdichte und Humusgehalt

Evaluation of soil physical parameters as a function of soil texture, effective density and humus content The latest, 4. edition of the Soil Mapping Instruction presents a new soil texture diagram with 31 partially newly defined soil textures. This diagram works without alternative names of clay silt mixtures, it takes into account the latest scientific findings and should obligatory be used in the new and old Bundesländer of the BRD. Though the soil textures define almost all soil specific valuations, the soil physical parameters depending from texture had to be recalculated on an enlarged database. 6352 records from 8 Bundesländer were used on this calculation. Out of these records most of the 31 soil textures could be characterized by representative and statistically proved values of air capacity, available water capacity, field moisture capacity and mean water permeability as a function of bulk density, dry, effective density and humus content. The values are presented in tables.     

Molybdängehalte einiger Acker- und Grünlandpflanzen Schleswig-Holsteins in Abhängigkeit von Bodenfaktoren

Mo contents of some crops and grassland plants of Schleswig-Holstein in relation to soil factors . The Mo content of about 170 plant samples of typical soils of Schleswig-Holstein were in the range of 0,2–11 ppm, increasing from grass to red clover, white clover and rape. By comparison with limiting values for adequate Mo supply (0,3 ppm Mo for red clover and probably also for the other three plants), a fairly good supply of the plants investigated can be deduced. The factors responsible for the varying Mo contents of plants are first of all the pH-value, furthermore the content of active iron and available phosphorus in the soil. The different contents of oxalat-soluble Mo had apparently no influence in this range of good supply. Whereas the correlation between one soil factor and plant Mo content was high only in some cases, coefficients of determination of up to 80% resulted from the use of several factors by multiple correlation.