Nährstoffauswaschung aus Weinbergsböden an der Mittelmosel

Leaching of plant nutrients from vineyard soils Leaching of plant nutrients particularly of nitrate from vineyard, arable, and forest soils of the Middle-Mosel have been investigated over a two-year period. Nitrate concentration in the leachate of vineyards amounted to an average of 326 mg NO₃/l and was about 10 to 20 times higher than the nitrate concentration in the leachate of arable and forest soils. According to the hydro-dynamic model assumptions on groundwater flow in the slates of the Rhenish Massif, the data obtained for the groundwater recharge (158-180 mm/year as gained in spring) and leaching of nitrate (144 kg N/ha/year) must be considered as minimum values. Hydrodynamic model assumptions suggest nitrate leaching rates of about 200 kg N/ha. Main reasons for the high leaching of nutrients are heavy fertilizer application and high mineralization rates in the vineyard soils favoured by relatively high soil temperatures and a high soil permeability.     

Tonmineral- und K-Ca-Austauscheigenschaften von Oberböden des Nährstoffpotentialversuches Hallertau

Clay mineralogy and K-Ca-exchange properties of surface soils from the nutrient potential trial Hallertau (Bavaria) In soils of four locations of the Hallertau nutrient potential trial, with a soil texture consisting of sand, silty sand, silty loam and sandy clayey loam, clay mineral properties were measured with the standardized glycerol expansion method and with n-alkylammonium (Rn_c-NH₃⁺-clay). The expandable minerals of the sandy soils consist exclusively of smectites s.s., (s.s. = sensu stricto) with 0.42 to 0.28 charge equivalents per formula unit (p.f.u.). The expandable minerals of the loams are an assemblage of smectites s.s. and vermiculites. The total layer charge of the smectites s.s. extend from 0.54 to 0.28 charge eq. p.f.u. The fine clay fractions (< 0.1 μm) do not contain vermiculites. The layer charge density of vermiculites with homogeneous charge in the coarse fractions varies between 0.60 and 0.95 charge eq. p.f.u. The immediate K-Ca-exchange was extended with the values of the continued K exchange versus Ca at low K intensity. The Q/I isotherms of sandy soils have a more pronounced curvature than the isotherms of the loams; in all cases, however, the exchange curves have a continuous form. This phenomen is discussed in terms of the clay mineralogy of the soils. After 8 years without K fertilizing, samples gave values between 168 and 497 kg smectite-K/ha for the surface soils. The constant rates of K-desorption vary between 12.8 and 28.7 kg K/ha (surface soil). The rates are better differentiated between unfertilized and fertilized soils for the loams than for the sandy soils. The constant rates of K release were found to be controlled at an AR-level between 1.6 · 10^?4 M^1/2 (unfertilized sandy soil) and 5.2 · 10^?4 M^1/2 (fertilized sandy clayey loam soil).     

Eine Split-root-Technik zur Untersuchung der Nährstoffverfügbarkeit in Abhängigkeit vom Wassergehalt im Boden

A Split-Root Technique for the Investigation of the Relationship between Nutrient Availability and Soil Water content . Nutrient availability in soils depends among other factors on soil water content. In order to investigate the quantitative relationship between availability and soil water content a special technique was developed. This split-root technique has to fulfil several conditions. 1. This technique must be able to allow to differentiate between the direct influence of water supply on plant growth and the influence of soil water content on nutrient availability and the effect of the latter on plant growth. 2. It must grant a sufficient supply of water oxygen and all nutrients to the plant with the exception of that nutrient the availability of which is to be examined. 3. A predetermined water content or water tension should be maintained as constant as possible during the experiment. These requirements are best met with by means a split-root technique. The experiments were carried out in such a way that the plants were grown in a container consisting of three compartments of which the centre one contained quartz sand whereas the two outer compartments were filled with soil (fig.1). Each plant had half of its root system growing in the sand and half of it in the soil. The quartz sand was supplied with a nutrient solution containing all nutrients except the one the availability of which is to be examined. The water content of the soil was regulated by means of ceramic filter candles which were linked to a water reservoir. This water reservoir was kept under negative pressure according to the required water tension in the soil. The water tension in the soil was monitored by 2–4 tensiometers in each of the soil compartmens (tab.1). Water tension up to pF 2.7 could be established and maintained in the soil. There was little variation of water tension during an experiment (3 weeks) and the moisture distribution in the soil was uniform. In order to obtain good reproducibilities the experiments were carried out in growth chamber.     

Nährstoffverlagerung und Wasserbilanz einer Braunerde aus Löß-Kolluvium unter Ackernutzuug

Nutrient displacement and water balance under oat crop on a Cambisol from loess colluvium Field experiments with oat on a loess soil were carried out from January until December 1978 on a since 6 years cultivated small plot area to study the water budget and the influence of different nitrogen fertilization on nutrient leaching. Ceramic cups were used to obtain soil water samples at a depth of 100 cm at two-week intervals, two years after application of a compost and after the application of artificial nitrogen fertilizers. Main components of the water balance were calculated with the use of a computer simulation (CSMP) program, the performance of which was controlled by tensiometer measurements. It was calculated that 214 mm of the total 608 mm rainfall in 1978 drained out of the profile, and that the cumulative evapotranspiration was 448 mm. This study included 70 stress days during which evapotranspiration was reduced. Chemical analyses of the soil solution samples showed that an intensive nitrogen fertilization surrendered to a significant increase in the nitrate displacement, whereas the average yearly losses of other nutrient elements, including potassium, phosphorus, calcium and magnesium were unchanged. The use of the compost fertilizer resulted in a significant increase in the sodium concentration of the soil solution samples.     

Die Bedeutung der Aggregierung für die Nährstoffsorption in Böden

The role of structure for nutrient sorptivity of soils The influence of the aggregation in 2 differently textured and structured soils (Haplumbrept and Chromudert) on the cation exchange capacity CEC was investigated. The results clearly demonstrated, that from the total soil (< 2 mm), natural and disturbed aggregates (Ø 5–8 mm) and the separated outer and inner part of those aggregates, the undisturbed aggregates had the lowest CEC. Furthermore, the aggregate skin was more chargeable than the inner part, due to a higher amount of silt and clay in that part. Because of higher bulk densities of the aggregates and theoretically increased tortuosity, the solution of elements in percolating water, especially in clay soils, is limited to the interaggregate pores. Thus, measured differences between the element distribution in different compartments can be explained.     

Erhebungsuntersuchung zur Nährstoffversorgung von Picea omorika im Zusammenhang mit dem Omorikensterben

A survey investigation of the relationship between nutritional factors and the decline of Picea omorika growth Soil and needle samples were collected from 193 sites of Picea omorika (mostly in private gardens) in Northern Germany ranging from normal to seriously damaged plants. The needles were analysed for N, P, K, Ca, Mg, Cu, Zn, Mn, Fe, B, Cl and Na. In the soil samples pH, P, K and Mg were determined.

• 1 In 54 cases (= 30,3% of the 178 sites with injured trees) the cause of the damage could not be established. In a few cases only (12 sites = 6,7%) Mg deficiency seemed to have caused the injuries. But in a large number of cases the needles showed high Cl contents, hence Cl toxicity was the most important cause (103 sites = 57,9%) of the damage.
• 2 The critical content of needles sampled in autumn is 0,27 % C1. Above this value CI-toxicity is highly probable and between 0,22 and 0,27 % CI it is possible.
• 3 High Cl-content is associated with mottled chlorosis and in many cases also with a brown discoloration beginning at the tip of the needle. The symptoms are usually stronger at the tips of branches than in central or basal parts.
• 4 Susceptibility to Cl-toxicity is similar for Picea omorika and Picea abies.
• 5 C1-toxicity may be caused by high application of deicing salt and Cl-containing fertilizers. Some of the fertilizers specially developed for the nutrition of conifers even contain too much Cl.

     

Vergleichende Betrachtung von Verfahren zur Auswertung von Nährstoffsteigerungsversuchen am Beispiel Phosphor

Comparison of two procedures to evaluate phosphate‐fertilizing field trials Growth response of agricultural crops to different input levels (e.g., fertilizer rates) can be described by the “law of diminishing increments”, which has been formulated mathematically amongst others by Mitscherlich (1928) and von Boguslawski and Schneider (1962, 1963, 1964). In the present paper, the economically optimal phosphate‐fertilizer requirements in 43 long‐term phosphate (P)‐fertilization experiments were calculated using equations on the basis of the yield functions of Mitscherlich or von Boguslawski and Schneider, respectively. For three field trials with linear or disproportionately high yield responses on P fertilization, none of the two procedures could be used. The same held for four trials with maximum yields already appearing at the first fertilization level. Similar P‐fertilization optima were calculated for 36 trials following the “law of diminishing increments”, resulting in a highly significant correlation (R² = 0.946) between both procedures. The correlation coefficients between the phosphate balance at the calculated optimum profitability and CAL‐P content in the soils at trial start were R² = 0.70 (Mitscherlich, 1928) and R² = 0.65 (von Boguslawski and Schneider, 1962, 1963, 1964), respectively. An optimal soil P content of 8–10 mg CAL‐P (100 g soil)^–1 was deduced. Both methods are applicable to calculate the optimum phosphate‐fertilizer requirement if yield effects due to P fertilization follow the “law of diminishing increments” and the increments of fertilization levels in each trial are established in a way that diminishing yield increments can be expected.