Evolution of farm management, nitrogen efficiency and economic performance on Dutch dairy farms reducing external inputs     

Jeroen C.J. Groot  Walter A.H. Rossing  Egbert A. Lantinga 《Livestock Science》2006,100(2-3):99-110

The implementation of the statutory Mineral Accounting System (MINAS) in the Netherlands in the period 1998–2003 required large reductions in nutrient inputs of dairy farms. Patterns in farm management adjustments throughout 6 years and their effectiveness in terms of nitrogen use efficiency (NUE) and economic performance were evaluated for 45 commercial farms participating in a regional nutrient management project.

Six groups of farms were identified that differed in initial NUE and the change therein. Three groups of farms that were able to rapidly reduce fertilizer N input and establish a consistent farm management strategy were most successful in improving NUE. These farms had a higher gross margin per 100 kg milk than farms without a consistent strategy. The three effective strategies were primarily characterized by (i) continuous, gradual adjustment of the integrated farm management combined with a slight reduction in milk production per ha (re-balancing) versus increasing productivity per animal, thereby reducing maintenance N requirements, while (ii) maintaining or (iii) increasing the production intensity per ha. It was concluded that different approaches to improve NUE can be successful, also in economic terms, although a direct relationship between NUE and gross margin was not observed. The probably implicit choice for adoption of a strategy may be governed by farm endowment and the farmer's skills and objectives.  相似文献   

Quecksilber und Methylquecksilber in Böden und Pflanzen unterschiedlich belasteter Standorte der Slowakei. Mercury and methylmercury in soils and plants of differently contaminated sites in Slovakia     

Renta Dombaiov  Jen‐How Huang  Egbert Matzner 《植物养料与土壤学杂志》2005,168(2):238-240

  相似文献   

Beziehung zwischen NO3-Austrägen,C/N-Verhältnissen der Auflage und N-Einträgen in Fichtenwald (Picea abies Karst.)-Ökosystemen Mitteleuropas     

Prof. Dr. E. Matzner  Prof. Dr. C. Grosholz 《European Journal of Forest Research》1996,116(1-6):39-44

  相似文献   

Auswirkungen unterschiedlicher Feinwurzelverteilungen und-biomassen auf das Risiko für Trockenstreß und Nadelverluste in Fichtenbeständen—Ergebnisse von Simulationsrechnungen zum Wasserhaushalt     

B. Manderscheid  E. Matzner 《European Journal of Forest Research》1996,115(1):350-362

  相似文献   

Effect of aluminum uptake on growth and enzyme activity in Pisum sativum var. ‘Alaska’ and ‘Little Marvel’     

Egbert W. Henry  Jeffrey  W. Miller  Lauren J. Dungy  Michael T. Johnson  Julia K. Yeekpeh 《Journal of plant nutrition》2013,36(4):353-373

It is usually assumed that plant tissue responses to nutritional elements are due to specific genetic differences that may exist either between inbred or closely related species. Little Marvel (dwarf) and Alaska (normal) varieties of 14‐day old pea seedlings were treated with four different concentrations of Al‐containing nutrient solution (0.0mM, 0.2mM, 0.6mM and distilled H₂O), prior to being exposed for 14 days to either DARK, LIGHT, or UV. Selected tissues (root tip, main root, main stem and proximal stem) were bioassayed for peroxidase and polyphenol oxidase enzyme activities, fresh wt vs. dry wt, water uptake and stem growth. The present study suggests that Little Marvel and Alaska pea tissue responds to high toxicity levels of Al by demonstrating an enhancement of enzymic activity. Tissue weight, growth and water uptake also show differential tissue specificity in both Little Marvel and Alaska tissue, in terms of Al toxicity response, given a particular external exposure.  相似文献   

C and N natural abundance of the soil microbial biomass     

Paul Dijkstra  Ayaka Ishizu  Stephen C. Hart  Egbert Schwartz  Bruce A. Hungate 《Soil biology & biochemistry》2006,38(11):3257-3266

Stable isotope analysis is a powerful tool in the study of soil organic matter formation. It is often observed that more decomposed soil organic matter is ¹³C, and especially ¹⁵N-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was ¹⁵N-enriched relative to the total (3.2 ‰) and extractable N pools (3.7 ‰), and ¹³C-enriched relative to the extractable C pool (2.5 ‰). The microbial biomass was also ¹³C-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 ‰), but ¹³C-depleted for soils with a C4 signature (−1.1 ‰). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation.  相似文献   

Carbon Control on Nitrogen Dynamics in the Forest Floor of an N-Enriched Deciduous Forest Ecosystem     

Ji-Hyung Park  Egbergt Matzner 《Water, air, and soil pollution》2001,130(1-4):643-648

Recent evidence from nitrogen (N) saturation studies indicates that forest floors in moderately impacted forests are the primary sink for atmospheric N inputs. Some researchers have suggested that the sink capacity of organic horizons is dependent on the amount of available carbon (C), which can be used for microbial N assimilation. To test the hypothesis that C limitation in forest floors exposed to chronic N deposition leads to an enhanced N leaching, a field C input manipulation experiment is under way in a deciduous forest. Since September 1999 aboveground C input has been doubled (by doubling litter input or by amending glucose) or excluded in replicated plots. Here we report the short-term response of concentrations of dissolved inorganic N (DIN: NO₃ ^?-N and NH₄ ⁺-N) in forest floor percolate to the C input manipulation. In autumn following the C input manipulation, DIN concentrations in forest floor percolate decreased in all plots except the No Litter plots compared to the pre-treatment summer concentrations. In contrast, the concentrations of DIN in the No Litter plots remained high. A different seasonal pattern of DIN leaching among treatments, along with measurements of microbial biomass C and potential nitrification rates of forest floor samples, indicates that seasonal N dynamics in the forest floor are largely regulated by C availability changes assoicated with litterfall C input.  相似文献   

Long-term development of element budgets in a Norway spruce (Picea abies (L.) Karst.) forest of the German solling area     

B. Manderscheid  E. Matzner  K. -J. Meiwes  Y. Xu 《Water, air, and soil pollution》1995,79(1-4):3-18

To evaluate ecosystem response to changing atmospheric deposition, element budgets were established over the period from 1973 to 1991 for a Norway Spruce (Picea abies (L.) Karst.) site. Budgets for Na⁺, Cl^?, Ca²⁺, Mg²⁺, N, S and H⁺ were based on total deposition and seepage water fluxes. The deposition of Ca²⁺, Mg²⁺, particularly, of S and H⁺ decreased with time, while calculated N deposition remained constant at a high level. The decrease in Ca²⁺ deposition led to a reduction of Ca²⁺ fluxes with seepage water. The decrease of Mg²⁺ deposition did not have an effect on the output fluxes of Mg²⁺. The reversibility of soil and seepage water acidification by reduced S deposition was delayed by the release of previously accumulated soil SO ₄ ^2? . The highest NO ₃ ^? fluxes were observed during the period of 1986 to 1988; NO ₃ ^? fluxes in general demonstrated a considerable annual and periodic variation. Total N accumulation in the ecosystem amounted to nearly 590 kg ha^?1 yr^?1 during the observation period. The major sink of N in the spruce site is the aggrading humus layer. The results emphasize the need for measurements over several years to make conclusions regarding the function of ecosystems in response to atmospheric deposition.  相似文献   

SOM fractionation methods: Relevance to functional pools and to stabilization mechanisms   总被引：2，自引：0，他引：2  

Margit von Lützow  Ingrid Kögel-Knabner  Heinz Flessa  Egbert Matzner 《Soil biology & biochemistry》2007,39(9):2183-2207

Soil organic matter (SOM) consists of various functional pools that are stabilized by specific mechanisms and have certain turnover rates. For the development of mechanistic models that predict changes in SOM storage, these pools have to be quantified and characterized. In the past, numerous fractionation schemes have been developed to separate and analyse such SOM fractions. In this review, the SOM fractions obtained with such operational fractionation procedures are described in terms of their pool sizes, chemical properties, and turnover rates. The main objective of this review is to evaluate these operationally defined fractions with respect to their suitability to describe functional SOM pools that could be used to parameterize SOM turnover models. Fractionation procedures include (1) physical separation of SOM into aggregate, particle size, and density fractions and fractions according to their magnetic susceptibility, and (2) various wet chemical procedures that fractionate SOM according to solubility, hydrolysability, and resistance to oxidation or by destruction of the mineral phase. Furthermore, combinations of fractionation methods are evaluated.The active SOM pool with turnover rates <10 years may best be represented by the soil microbial biomass and the light fraction (<1.6-2 g cm⁻³) obtained by density fractionation (if black carbon contents are considered). Most chemical and physical fractionations as well as combinations of methods yield SOM fractions that are not homogeneous in terms of turnover rates. It has proven to be particularly difficult to isolate functional fractions that represent the passive model pools in which the majority of soil SOM is stabilized. The available fractionation methods do not correspond to specific stabilization mechanisms and hence do not describe functional SOM pools. Another problem is that comprehensive data for turnover rates and data for whole soil profiles are only now becoming available, especially for new fractionation methods. Such information as well as the use of specific markers and compound-specific isotope analysis may be important for future differentiation and evaluation of functional SOM fractions.  相似文献   

Effects of aluminium on the mineralization of dissolved organic carbon derived from forest floors   总被引：5，自引：0，他引：5  

D. Schwesig  K. Kalbitz  & E. Matzner 《European Journal of Soil Science》2003,54(2):311-322

Aluminium (Al) is abundant in soils, but the influence of Al on the mineralization of dissolved organic carbon and thus on carbon sequestration in soil is only poorly understood. We investigated the extent and rate of mineralization of dissolved organic carbon at various Al/C ratios. Dissolved organic carbon extracted from Oi and Oa layers under coniferous and deciduous forest was incubated with initial molar Al/C ratios from < 0.004 to 0.44 for 130 days. Mineralization was quantified by measurement of CO₂. Rapidly and slowly mineralizable pools of dissolved organic C and their decomposition rate constants and half‐lives (as a measure of labile and stable C) were modelled with a double exponential equation. Increasing initial Al/C ratios up to 0.1 led to a considerable decrease in mineralization (up to 50% compared with control samples). The half‐life of the stable C pool increased up to 4‐fold, whereas the half‐life of the labile C pool was unaffected. Ratios of Al/C > 0.1 did not further decrease the mineralization, but led to increasing concentrations of free Al³⁺ in solution, and to increasing Al/C ratios in the precipitate, indicating that the Al complexation capacity of dissolved organic C was exceeded. Decrease in mineralization as well as formation of particulate organic matter (up to 56% of initial dissolved organic C) affected mainly the stable pool. Mineralization of dissolved organic C can be predicted from UV absorption by use of exponential regressions, but adding an Al variable did not improve the prediction significantly. We conclude that Al influences substantially the biodegradability of dissolved organic C percolating into the mineral soil, which may have consequences for the carbon sequestration in the soil. Declining Al concentrations would increase the mineralization of dissolved organic C only if the Al/C ratio becomes less than the ‘threshold value’ in the range of the Al complexation capacity of the dissolved organic C.  相似文献