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Abstract
This work reports on the spatio-temporal characterization of the multiple current pulse regime of diffuse barrier discharges driven by sine-wave feeding voltage at a frequency of 2 kHz in helium with small nitrogen admixtures. The discharge gap of 3 mm is bounded by glass plates on both plane electrodes. Priority is given to the lateral discharge inhomogeneities, underlying volume- and surface-memory effects, and the breakdown mechanism. Therefore, relevant processes in the discharge volume and on the dielectric surfaces were investigated by ICCD camera imaging and optical emission spectroscopy in combination with electrical measurements and surface charge diagnostics using the electro-optic Pockels effect of a bismuth silicon oxide crystal. The number of current pulses per half-cycle of the sine-wave voltage rises with increasing nitrogen admixture to helium due to the predominant role of the Penning ionization. Here, the transition from the first glow-like breakdown to the last Townsend-like breakdown is favored by residual species from the former breakdowns which enhance the secondary electron emission during the pre-phase of the later breakdowns. Moreover, the surface charge measurements reveal that the consecutive breakdowns occur alternately at central and peripheral regions on the electrode surface. These spatial inhomogeneities are conserved by the surface charge memory effect as pointed out by the recalculated spatio-temporal development of the gap voltage.
Background: The association of polyomaviruses BK and JC with other opportunistic infections and graft-versus-host disease (GvHD) in allogeneic stem cell transplantation is controversially discussed. Methods: We conducted a retrospective study of 64 adult patients who received their first allogeneic stem cell transplantation between March 2010 and December 2014; the follow-up time was 2 years. Results: Acute leukemia was the most frequent underlying disease (45.3%), and conditioning included myeloablative (67.2%) and nonmyeloablative protocols (32.8%). All patients received 10 mg of alemtuzumab on day -2 (20 mg in case of mismatch) as GvHD prophylaxis. Twenty-seven patients (41.5%) developed cytomegalovirus (CMV) reactivation. BKPyV-associated hemorrhagic cystitis was diagnosed in 10 patients (15.6%). Other opportunistic infections caused by viruses or protozoa occurred rarely (<10%). There was no association of BKPyV or JCPyV with CMV reactivation, Epstein-Barr virus reactivation, human herpes virus 6, or parvovirus B19 infection requiring treatment. There was a significant correlation of BKPyV-associated hemorrhagic cystitis with toxoplasmosis (p = 0.013). Additionally, there was a significant link of simultaneous BKPyV and JCPyV viruria with toxoplasmosis (p = 0.047). BKPyV and JCPyV were not associated with GvHD, relapse, or death. Conclusion: We found no association of BKPyV or JCPyV with viral infections or GvHD. Only the correlation of both polyomaviruses with toxoplasmosis was significant. This is a novel and interesting finding.
Background
There is a lack of data concerning socioeconomic outcome and quality of life (QoL) in patients after status epilepticus (SE) in Germany.
Patients and methods
Adult patients treated between 2011 and 2015 due to SE at the university hospitals in Frankfurt, Greifswald, and Marburg were asked to fill out a questionnaire regarding long-term outcome of at least 3 months after discharge. The SE cohort consisted of 25.9% patients with an acute symptomatic, 42% with a remote symptomatic and previous epilepsy, 22.2% with a new-onset remote symptomatic, and 9.9% with other or unknown etiology. A matched case–control analysis was applied for comparison with patients with drug refractory epilepsy and seizure remission, both not previously affected by SE.
Results
A total of 81 patients (mean age: 58.7 ± 18.0 years; 58% female) participated. A non-refractory course was present in 59.3%, while 27.2% had a refractory SE (RSE) and 13.6% had a superrefractory SE (SRSE). Before admission, a favorable modified Rankin Scale (mRS) of 0–3 was found in 82.7% (67/81), deteriorating to 38.3% (31/81) (p = 0.003) at discharge. The majority returned home [51.9% (42/81)], 32.1% entered a rehabilitation facility, while 12.3% were transferred to a nursing home and 3.7% to another hospital. The overall mRS at follow-up did not change; 61.8% (45/74) reached an mRS of 0–3. In RSE and SRSE, the proportion with a favorable mRS increased from 45.5% at discharge to 70% at follow-up, while QoL was comparable to a non-refractory SE course. Matched epilepsy controls in seizure remission were treated with a lower mean number of anticonvulsants (1.3 ± 0.7) compared to controls with drug refractory epilepsy (1.9 ± 0.8; p < 0.001) or SE (1.9 ± 1.1; p < 0.001). A major depression was found in 32.8% of patients with SE and in 36.8% of drug refractory epilepsy, but only in 20.3% of patients in seizure remission. QoL was reduced in all categories (QOLIE-31) in SE patients in comparison with patients in seizure remission, but was comparable to patients with drug refractory epilepsy.
Discussion
Patients after SE show substantial impairments in their QoL and daily life activities. However, in the long term, patients with RSE and SRSE had a relatively favorable outcome comparable to that of patients with a non-refractory SE course. This underlines the need for efficient therapeutic options in SE.
Background: We assessed the effect of the uniform donor questionnaire (UDQ) on deferral rates in first-time and repeat donors. We focused on the introduced question about unprotected sexual contact with a new partner. Another goal was a stratified comparison of the deferral rates of the donor questionnaire (DQ) and UDQ. Methods: Data on donors and deferrals using the DQ and UDQ were collected at four blood establishments. The comparison included a 2-year period by questionnaire version. For the comparison of the questionnaires, an adjusted multinomial logistic regression was performed. Results: The analysis included 260,848 donations. First-time (FTD) and repeat donations (RD) showed higher deferral rates with the UDQ (FTD +5.4%, RD +1.4%). Deferral due to a new partner was 3.0% in first-time and 0.4% in repeat donors. The majority of these occurred in the youngest age groups. The most frequent deferral criterion was ‘disease' (5.1%). Conclusion: The regression revealed stronger predictors for deferral than the questionnaire version. Especially younger age carried a higher and independent risk for deferral. The additional deferrals of mainly young first-time donors due to a new sexual partner may identify those donors with potential heterosexual risk behavior who would otherwise not be identified.
The dissertation describes an Indigenous dream framework that underscores the significance of dreams as a mirror of trauma and a way that leads back to Indigenous knowledges. Significant differences of Western and Indigenous epistemology are exemplified by juxtaposing Western and Indigenous dream discourses. The selected prose fiction allows for a dream categorization that emphasizes the significance and meaning of dreams as a metaphorical as well as narrative device.
Nightmares/Anxiety dreams are often the result of the devastating effects of colonization and especially Residential School. Nightmares in the texts are often exact replicas of the abuse suffered in the boarding schools. They are discussed in the context of Robert Arthur Alexie’s novel Porcupines and China Dolls (2001/2009) represents dreams and traumatic nightmares and deals with the fictional Blue People First Nation. The community’s collective intergenerational trauma of Residential School experience keeps them stuck in dysfunctional dynamics dominated by suicides, sexual and physical abuse, drug and sex addictions.
Telling dreams, categorized as “instructing dreams,” and “announcing dreams,” teach the dreamer what will happen in the future. They are discussed in the context of Richard Van Camp’s short stories “On the Wings of this Prayer” and “The Fleshing” (Godless but Loyal to Heaven, 2012), which represent the category of the ecological nightmare as well as of telling dreams. Ecological nightmares display environmentally destructive effects of capitalist globalization that have come to “infect” the world. The Windigo figure in the stories serves as a manifestation of resource and in particular petro-capitalism and Western society’s constant need to subjugate nature. Ecological dreams hence call for ecological vigilance and establish Indigenous knowledges as a source of resurgence and restoration.
Existential dreams function as decolonizing tools that facilitate liberation. The thesis provides a literary analysis of Richard Wagamese’ novel Ragged Company (2008) and Cherie Dimaline’s short story “room 414” (Red Rooms, 2007) where homelessness is postulated as the manifestation of individual and tribal/communal disjointedness and isolation. Through existential dreaming, the urban lives of most of the characters dwelling in the shadows and margins of society are existentially transformed and healing seems possible. Paternalistic colonial mindsets continue to patronize Indigenous knowledges (as unreliable and unscientific) until Western “discoveries” prove what has been known for decades.
The thesis underscores dreams as an essential part of Indigenous Knowledges, i.e. as knowledge sources. Surmounting Western dream perceptions and instead valorizing Indigenous knowledges, the characters in the texts discussed in my thesis, unremittingly follow their dreams’ instruction and eventually achieve reconciliation and healing. In the fictional texts discussed, nightmares represent homelessness, trauma, stagnation, and a disconnection to one’s (Native) background, whereas dreams represent continuity through the restoration of identity, finding home, and a sense of belonging. The notion of a dream reality and a waking reality influencing and informing each other relies on sharing dreams with the community, eventually leading to an enactment of the dream or vision. Dreaming and identity are significantly linked and foster processes of intellectual self-determination. The characters’ inability to externalize their internal wishes, desires, and needs results in further denial and consequential bitterness that feed into the spiral of alcohol and drug abuse as well as metaphorical and literal homelessness. The dreams’ semantic field strongly alludes to ceremonial traditions and provides the prospect of a rooted Indigeneity. At the turning points in the lives of the characters, when dreams and visions start to appear, they are lost in translation. The characters’ own illiteracy towards Native epistemology and spirituality has them trapped in the inability to read and act on their dream messages. Strong (often female) Indigenous presences that go hand in hand with the appearance of dreams provide the protagonists with guidance and lead the way back to the “Old Ways.” Through dreaming, the spiral of colonialism is disrupted and replaced by the circle of reconciliation and relationality.
Background: Mild-to-moderate chronic kidney disease (CKD G3a) is prevalent in older adults. Substantial evidence suggests that individuals with advanced CKD face a high risk for common geriatric conditions, like functional impairment and cognitive decline, whereas the relationships between mild-to-moderate CKD and functional impairment and cognitive decline, but also poor nutritional status and mood disorders, are still unclear. Objective: The aim of this study was to explore associations between mild-to-moderate CKD and impairments in the core domains of geriatric assessment (GA) in a large cohort of community-dwelling older adults. Methods: This was a cross-sectional analysis of 1,476 participants of the Berlin Aging Study II. Study participants were stratified as to presence or absence of CKD G3a (estimated glomerular filtration rate [eGFR] 45-59 mL/min/1.73 m<sup>2</sup> vs. eGFR ≥60 mL/min/1.73 m<sup>2</sup>). GA comprised the following instruments: the Activities of Daily Living Scale (ADL), the Timed up and Go (TUG), the Tinetti test (Tinetti), the Mini-Mental-State Examination (MMSE), the Geriatric Depression Scale (GDS), and the Mini Nutritional Assessment (MNA). We used logistic regression models to estimate multivariable-adjusted associations between CKD G3a and impairments in the respective domains. Results: A total of 282 subjects with mild-to-moderate CKD (CKD G3a) were identified (19.1%). Overall, the prevalence of impairments identified was higher among subjects with compared to without CKD G3a (21 vs. 15.9%, p = 0.043). In multivariable-adjusted models, CKD G3a was consistently associated with increased odds of an impaired gait performance as to the TUG (adjusted odds ratio 2.06, 95% CI 1.04-4.09). In contrast, on average, individuals with and without CKD G3a did not differ as to their results in the MMSE, the ADL, the MNA, and the GDS. Conclusion: GA identified impairments in 21 versus 15.9% of older adults with and without mild-to-moderate CKD, respectively. However, except for an increased likelihood of impaired gait performance (TUG) with mild-to-moderate CKD, we did not find independent associations between mild-to-moderate CKD and geriatric conditions.
Background: ‘Quality in medicine' is a term used in a broad sense. In this work the definition and dimensions of quality in medicine and the implementation of a measurement and reporting system in Germany are discussed. Existing applications are described and possible future effects are pointed out. Methods: The ongoing process of implementing a quality reporting system into the German healthcare system is studied by publicly available legal texts, published reactions of stakeholders and publications of G-BA and IQTIG. Definitions of quality, dimensions of quality and quality measurement in medicine are studied by using textbooks as well as the world wide web and PubMed search. Results: Donabedian‘s ‘dimensions of quality' are fundamental in dealing with quality in medicine. Existing measurement and reporting systems have immanent strengths and weaknesses, as the definition of quality is affected by one‘s point of view. The legislator will have to decide which ‘dimension of quality' is mandatory and how to measure it. Conclusion: Quality has become a control instrument with unforeseeable consequences. A clear definition of the used quality concept is as essential as the use of feasible measurement and reporting systems. The use of routine data could be an interesting option.
Less invasive caries management techniques for treating cavitated carious primary teeth, which involve the concept of caries control by managing the activity of the biofilm, are becoming common. This study aimed to compare the clinical efficacy (minor/major failures) and survival rates (successful cases without any failures) of 3 carious lesion treatment approaches, the Hall Technique (HT), non-restorative caries treatment (NRCT), and conventional restorations (CR), for the management of occlusoproximal caries lesions (ICDAS 3-5) in primary molars. Results at 2.5 years are presented. A total of 169 children (3- to 8-year-olds) were enrolled in this secondary care-based, 3-arm parallel-group, randomised controlled trial. Participants were allocated to: HT (n = 52; sealing caries with stainless-steel crowns without caries removal), NRCT (n = 52; opening up the cavity and applying fluoride varnish), CR (n = 65; control arm, complete caries removal and compomer restoration). Statistical analyses were: non-parametric Kruskal-Wallis analysis of variance, Mann-Whitney U test and Kaplan-Meier survival analyses. One hundred and forty-two participants (84%; HT = 40/52; NRCT = 44/52; CR = 58/65) had follow-up data of 1-33 months (mean = 26). Overall, 25 (HT = 2, NRCT = 9, CR = 14) of 142 participants (17.6%) presented with at least 1 minor failure (reversible pulpitis, caries progression, or secondary caries; p = 0.013, CI = 0.012-0.018; Mann-Whitney U test). Ten (HT = 1, NRCT = 4, CR = 5) of 142 participants (7.04%) experienced at least 1 major failure (irreversible pulpitis, abscess, unrestorable tooth; p = 0.043, CI = 0.034-0.045). Independent comparisons between 2 samples found that NRCT-CR had no statistically significant difference in failures (p > 0.05), but for CR-HT (p = 0.037, CI = 0.030-0.040) and for NRCT-HT (p = 0.011, CI = 0.010-0.016; Kruskal-Wallis test) significant differences were observed. Cumulative survival rates were HT = 92.5%, NRCT = 70.5%, and CR = 67.2% (p = 0.012). NRCT and CR outcomes were comparable. HT performed better than NRCT and CR for all outcomes. This study was funded by the Paediatric Dentistry Department, Greifswald University, Germany (Trial registration No. NCT01797458).
Objective: We performed a pilot RCT to prove the hypothesis that a controlled ingestion of polyphenol-rich beverages (soy drink, decaffeinated black tea) in nutritive dosages by nursing women has an effect on the composition (flavonoid concentration, total antioxidant capacity) of breast milk. Methods: Healthy nursing women were supplemented with either 250 mL of a soy drink (12 mg isoflavones; n = 18), 300 mL decaffeinated black tea (67 mg catechins; n = 18), or 300 mL water (n = 8, control) for 6 days. Milk samples were collected before, during, and after intervention. Flavonoid content (isoflavones/catechins, HPLC) and total antioxidant capacity of milk and test drinks in milk specimens were assessed. Results: Isoflavone content (genistein and daidzein) in breast milk increased up to 12 nmol/L after soy drink consumption; the major flavonoids constituents of black tea (catechin, epicatechin, and respective conjugates) could not be detected in milk samples. With both interventions, the total antioxidant capacity of breast milk was not affected. Conclusions: Mothers' daily consumption of a soy drink considerably increases isoflavone content of breast milk resulting in an estimated daily exposure of 9.6 nmol isoflavones in a 4-month-old suckling infant. Luminal flavanol uptake from black tea consumed by the nursing mother may be too low to affect flavanol concentrations in breast milk.
The aims of this study were to quantify the key mineralization processes and the resulting nutrient release potentials of different sediment types, their ranges of extent and dependency on varying environmental conditions such as seasonal variations or shifts in oxygen availability. Benthic phosphate fluxes and flux potentials were of particular interest as P is an essential nutrient for algal growth in marine systems and phosphate is often limiting primary production, hence strongly promotes the production of new biomass. A major P source in marine environments are mineralization products of early diagenetic processes.
To gain insight into the pathways of organic matter mineralization and subsequent secondary reactions, key reactants in the solid and the dissolved phase were considered in typical sediments of the Baltic Sea and the Black Sea. Seven study sites in the German Baltic Sea region, representative of the major depositional environments, including coarse and fine grained sediments, both rich or poor in organic carbon, were intensively studied. The investigations were conducted on a seasonal basis during ten ship-based expeditions between July 2013 and March 2016, covering spring- and autumn algal blooms, stagnation periods with bottom water hypoxia and winter dormancy. Hypoxic conditions frequently developed in the bottom waters of the Bay of Mecklenburg, Stoltera and the Arkona Basin sites, shallower stations like the Tromper Wiek, the Oder Bank and the Darss Sill were usually not affected by hypoxia. Increased nutrient concentrations in the bottom waters coincided with oxygen depletion. High salinity dynamics were observed in the bottom waters above the studied sediments, which were due to frequent salt water inflows from the North Sea. Bottom water temperature variability was seasonally conditioned.
The studied sands showed 2-3 orders of magnitude higher permeability values and about one order of magnitude lower organic matter contents compared to the studied muds. Occasionally, strongly increased organic matter contents were observed in the sands, likely induced by downward mixing of plankton bloom derived particles. The organic matter was found to be essentially supplied by marine phytoplankton, indicated by its elemental composition and isotopic signature.
Additionally, an adapted approach of the Keeling plot method was made to characterize the source material of organic matter mineralization. In marine environments, dissolved inorganic carbon concentrations often increase with depth together with an isotopic carbon signature shift to lighter values due to organic matter mineralization. The Keeling plot method was commonly used to determine the isotopic signature of carbon sources for ecosystem respiration. Conventionally, the influence of respiratory depletion of 13CO2 on the isotopic composition of the atmosphere was studied in terrestrial and limnic biogeochemistry. The same approach was applied on organic matter mineralization in sediments and the water column during this study. Mixing of bottom water derived background DIC and DIC released into the environment during organic carbon decomposition was assumed. In a modification of previous approaches, where changes in concentration and δ13C of DIC were followed over time, vertical profiles were analyzed in this study, which represent time-dependent variations superimposed by transport processes . DI13C gradients in the water column of the Black Sea and pore water profiles in the Black Sea and the Baltic Sea were used to estimate the 13C signature of the mineralized organic carbon via Keeling plot analysis. The Black Sea water column revealed a δ13C signature of the organic matter source close to the signature of typical particulate organic matter in the ocean and previously reported values for the Black Sea euphotic zone. In the pore waters of Black Sea sediments (from short and long sediment cores), Keeling plot analysis clearly demonstrates that the released DIC at depth can be derived from different sources. An isotopically very light carbon source (< –60 ‰) was associated with anaerobic oxidation of methane in the Black Sea. Marine organic matter was the principal source for DIC in the deeps of Baltic Sea basins, while the calculated carbon source isotopic signature in sediments of sand flats and bays was shifted to heavier δ13C signatures compared to marine organic matter. These shifts were attributed to potential dissolution of sedimentary carbonates or organic inputs of terrestrial C4 vascular plants like maize and other agricultural plants. The carbon source isotopic composition calculated via Keeling plot analysis correlated well with directly measured δ13C signatures of surface sediments POM.
Organic matter mineralization activity in the southern Baltic Sea sediments was studied via gross sulfate reduction rate analysis and total oxygen uptake measurements in sands and muds. Oxygen penetration depths were less than 4 mm in both, muddy and sandy sediments. Oxygen uptake rates were similar in muds (10.2 mmol m–2 d–1) and sands (10.7 mmol m–2 d–1), while significantly higher rates were measured in the coastal near sites of the Bay of Mecklenburg (about 12 mmol m–2 d–1) than in the deeper Arkona Basin (about 9 mmol m–2 d–1). Substantial sulfate reduction was measured in the muddy (about 4 mmol m–2 d–1) and the sandy (about 1 mmol m–2 d–1) study sites. Highest sulfate reduction rates (4.4 – 5 mmol m–2 d–1) were detected in the muds of the Bay of Mecklenburg during summer, about twice as high as in the Arkona Basin muds. Increased mineralization activity of the coastal near muds of the Bay of Mecklenburg is attributed to enhanced input of fresh organic matter during algal blooms.
About twofold higher oxygen consumption and sulfate reduction rates were measured in summer compared to winter in sandy and muddy sediments.
The studied sites were usually characterized by a typical biogeochemical zonation with oxic, suboxic and sulfidic zones. The concentration profiles in the muds reflected sulfate reduction and secondary redox-reactions, liberating dissolved carbon, nitrogen, phosphorus and hydrogen sulfide into the interstitial waters. Orders of magnitude lower concentrations were detected in the sands, while their top centimeters were mostly irrigated and mineralization products only accumulated below.
A several centimeter thick suboxic zone was sustained by active downward transport of oxidized material in the southern Baltic Sea coastal sediments, presumably mainly through bioturbation. Especially sulfur and iron species were involved in the secondary reactions between the metabolites of early diagenetic processes occurring in the suboxic zone. Partly high temporal variability was observed in the form of vertical migration of the sulfidic zone and a corresponding expansion and shrinking of the suboxic zone. The Arkona Basin site showed the most stable geochemical zonation over time, while the Luebeck Bight site and especially the Mecklenburg Bight site showed striking dynamics. The consequent redox-regime shifts within the surface sediments might promote mineralization of organic matter as higher sulfate reduction rates and higher total oxygen uptake were measured in these more dynamic muds. The vertical shifts of the redox-gradients can largely be explained by temporal and spatial variability of bioturbation activity, but also anthropogenic activities may play a role. Bottom trawling, may be the dominant mixing process at the Mecklenburg Bight site.
In the sands, less reactive iron and manganese contents were available compared to the studied muds, which may be due to frequent irrigation of the top centimeters leading to a loss of pore water reservoirs like dissolved Fe and Mn.
Another mixing process, storm induced sediment resuspension, was suggested to be important for the sediments in the study area. A severe sediment resuspension event at the silty Tromper Wiek site was indicated by steep gradients in pore water concentration and particulate mater content profiles in the top ∼ 5 cm sediments. Carrying out non steady state modeling (Bo Liu, IOW), the successive re-development of the pore water profiles towards a steady-state was simulated and the time span necessary to establish measured pore water profiles after the sediment disturbance event was approximated. In the predicted time span, daily average wind speeds reached an annual high of the category ‘gale’ which was probably sufficient to resuspend and irrigate the surface silt-type sediments.
This study showed that sediment mixing processes have a strong influence on early diagenetic reactions, solute release potentials and actual fluxes from the sediments. Also the sediment mixing via bottom trawl fishing can be regarded as an event-like disturbance. The newly developed approach of non-steady-state modeling of pore water sets (Bo Liu; IOW) can help to answer the question, how long it takes to reach a steady-state after a sediment disturbance event.
The concentration profiles in interstitial waters were used to calculate net transformation rates via the transport-reaction models REC and PROFILE. The calculations revealed net release of H4SiO4 and PO4 within the top 20 cm of the studied muds, while net DIC and NH+4 consumption and sulfate production was clearly evident within the top ∼ 5 cm. Intensive reoxidation of sulfide that was produced via sulfate reduction was also indicated by large deviations between the modeled net sulfate transformation rates and experimentally derived gross sulfate reduction rates. These surface near transformations were probably associated with microbial chemosynthesis.
The studied sands of the southern Baltic Sea were usually characterized by very low pore water gradients, probably due to their frequent irrigation. Accordingly, calculated transformation rates were one to two orders of magnitude lower in the studied sands compared to the muds of the southern Baltic Sea. However, during a situation with a stratified water column, substantial pore water reservoirs with the typical concentration trends were present in the sandy Darss Sill sediments. Integrated production rates of PO4, Mn2+ and H4SiO4 derived from these concentration profiles were in the same order of magnitude as in the muddy Arkona Basin.
Intensive pore water irrigation is also capable to transport fresh organic matter into the sediment as was occasionally indicated by strongly increased surface near TOC in the sands. Considerable gross sulfate reduction rates and total oxygen uptake rates were measured in the sandy Oder Bank sediments, where pore water concentration profiles rather suggested absence of diagenetic processes. The studied sands were, hence, not unreactive substrates but usually rather unable to preserve the mineralization products.
This reflects the often limited significance of pore water evaluations in irrigated sandy sites but also the high mineralization potentials of coastal sands. Early diagenetic processes and the impact of intense benthic-pelagic exchange in such shallow marine environments is still poorly understood, as they were rarely investigated in the past and are methodologically more difficult to investigate.
The Baltic Sea deeps Gotland Deep and Landsort Deep were mainly controlled by sulfate reduction and shallow anaerobic oxidation of methane. Calculated rates of net sulfate reduction and net sulfide production were equivalent, indicating a lack of sulfide re-oxidation reactions. Phosphate liberation rates were low in the surface sediments, but strong linear concentration gradients indicated liberation at depth.
The euxinic Black Sea sediments were purely controlled by sulfate reduction via anaerobic oxidation of methane at the sulfate-methane transition zone in sediment depths of up to several meters. Subsequent diffusive concentration gradients clearly dominated pore water profiles in the surface sediments.
Benthic solute reservoirs of the top 10 cm pore waters were generally higher in the muds than in the sands of the southern Baltic Sea. The smaller reservoirs in the sands were cause by intensive exchange between pore water and bottom water in these permeable sediments. The three studied muddy sites of the southern Baltic Sea showed great dissimilarities with respect to their pore water compositions. Large observed pools of dissolved Fe2+ and PO4 clearly point to reduction of reactive Fe and release of adsorbed P pools. Multi-dimensional scaling analysis showed that seasonal variability played only a minor role for the observed variability of the benthic solute reservoirs. Principal component analysis revealed that the studied sediments can be characterized by essentially two factors based on their pore water reservoirs of the top 10 cm: 1) their mineralization and accumulation efficiency and 2) their secondary reactions in the suboxic zone, reflecting fundamental differences in their sedimentation conditions and mixing processes. While the sands were similar to each other due to their overall low reservoirs, sands, silts and muds mainly differed in their mineralization and accumulation efficiency. Large variability was also observed within the studied muds regarding their predominating redox metabolites. Highest dissimilarities were evident between the neighboring sites Mecklenburg Bight (mostly suboxic) and Luebeck Bight (mostly sulfidic). Therefore, the biogeochemical state in the studied sediments were shown to be mainly controlled by their sediment type and the transport of reactive iron into the sediments. The supply of organic matter to the sea floor controlled the overall mineralization activity, while the sediment permeability determined the accumulation efficiency of the sediment. Mixing of surface sediments together with the complex relation of oxygen, sulfur, iron and phosphorus in the solid and aqueous phase is controlling benthic nutrient fixation/liberation reactions. Salinity variability showed no noticeable effects on early diagenetic processes. During four sampling occasions in the Arkona Basin, bottom water salinity showed strong variability which was also effecting pore water concentration profiles in more than 15 cm depth. However, concentration profiles of typical organic matter mineralization products remained remarkably stable. Also gross sulfate reduction rates seemed to be unaffected by the variable pore water sulfate concentrations.
Nutrient fluxes across the sediment-water interface were obtained by the interpretation of vertical pore water concentration profiles via different models (diffusive fluxes) and via incubation of intact sediment cores (total fluxes). Benthic diffusive fluxes represent potential release of solutes into the water column. They were often strongly associated with the benthic reservoirs, thus fluxes were highest in the muds, considerably lower in the organic-poorer silts, and generally close to zero in the sands. The dissimilarities between diffusive fluxes in the different sediments were mainly controlled by the sediment type. Highest variability was observed within the muds, controlled by their different diagenetic pathways due to different sediment mixing intensities.
In the muddy sediments, diffusive PO4 fluxes were much higher than mineralization of organic matter with the common element ratios of marine organic matter can provide, indicating active recycling of phosphorus within the muds due to recurring adsorption and re-release on reactive iron oxyhydroxide phases. Especially in the strongly mixed Mecklenburg Bight sediments, pore water dissolved PO4 was primarily controlled by the release of adsorbed P. Actual PO4 release into the bottom waters (determined via core incubation experiments) was only measured under extended bottom water oxygen deficiency conditions. The same applied to the redox-sensitive solutes Fe2+, Mn2+ and sulfide.
For the less redox-sensitive solutes, diffusion usually accounted only for a fraction of the total interfacial flux. The proportion of advective to diffusive transport was estimated with different methods. Bioturbation induced sediment mixing was quantified by comparing the diffusive H4SiO4 fluxes derived from pore water modeling with the total fluxes derived from the core incubations. The studied muds showed infauna induced advection proportions of about 35 – 100 %. Only when infauna was absent, diffusion became the dominant transport process across the sediment-water interface. In the studied sands, advection was the dominating transport process, since their generally low surface near reservoirs lead to diffusive fluxes close to zero. However, it remains unclear whether bioturbation or hydrodynamic irrigation are responsible for that. An attempt was made to estimate the effect of hydrodynamic irrigation for a range of reasonable bottom water velocities from the sediment bedform geometry after Neumann et al. (2017). However, resulting potential hydrodynamic irrigation was found to be rather low compared to reported values from the literature and may significantly underestimate actual irrigation of the sandy sediments.
In a new non steady-state multi-element diagenetic modeling approach (Bo Liu, IOW), vertical δ13C pore water profiles were used to estimate the significance of advective transport processes. Mixing processes at the sediment-water interface were expressed as multiple of pure diffusion (ε). By adjusting this mixing coefficient as boundary condition for best fits of predicted to measured pore water profiles, the degree of these mixing processes was estimated. In the Arkona Basin surface sediments, this approach revealed best fits assuming a mixing depth of 3.5 cm with a tenfold higher total mixing degree based on diffusional transport. The calculated mixing depths and intensities were similar to bioturbation depths and rates obtained via traditional methods (Morys, 2016). The novel modeling approach is a promising method to evaluate surface sediment mixing processes.
Increased mineralization activity during productive seasons lead to increased oxygen consumption and therefore frequent bottom water hypoxia. The effects of hypoxic bottom water conditions on the early diagenetic processes in the sediments were studied via prolonged core incubation experiments. Shifts to bottom water oxygen deficiency had various consequences for benthic reservoirs and fluxes. The oxygen consumption decreased during hypoxic incubation phases. Decreased bioturbation activity diminished advective transport so that total fluxes of redox-insensitive solutes (e.g. H4SiO4) were decreased. Reactive iron and manganese oxides act as barrier (“iron curtain”) in the suboxic zone, preventing redox-sensitive solutes from their release into the water column. After a shift to bottom water hypoxia, these reactive oxides are re-dissolved and liberated into the water column. Prolonged incubation experiments suggested that the Mn-oxide reservoirs were depleted first before the Fe-oxides with the adsorptively bound phosphate were liberated.
The release of nutrients (especially phosphorus), dissolved inorganic carbon, and redox- sensitive compounds (e.g. hydrogen sulfide) strongly varied in the different studied environments, covering coastal-near oxic, temporary hypoxic and euxinic conditions.
In environments, where advection through hydrodynamic irrigation or bioturbation do not occur, like in anoxic or euxinic systems, surface-near pore water gradients reflect total solute interfacial fluxes. They depend on the supply of organic matter to the sea floor, the mineralization rates in the sediments and the composition of the overlying bottom water. In the Black Sea, much of the organic matter mineralization was performed already in the water column and not in the sediments, leading to a decreasing export of organic matter to the sediment and increasing concentrations of mineralization products in the bottom water with increasing water depth. Accordingly, benthic fluxes across the sediment-water interface of the deep Black Sea sites were the lowest of the entire study, essentially reflecting the low mineralization rates of AOM in deeper layers. Highest fluxes in the Black Sea were observed at the continental slope at intermediate water depths, but were still lower than in the Baltic Sea deeps.
In contrast, highest DIC fluxes were detected in the oxygen depleted Baltic Sea deeps Gotland Deep and Landsort Deep. These basins are shallow enough that reactive organic matter reaches the sea floor, where it is mineralized via sulfate reduction close to the sediment surface. Strong concentration gradients and therefore high diffusive interfacial fluxes across the sediment-water interface were evident. As bioturbation was absent, these diffusive fluxes were representative for total interfacial fluxes unlike in sediments with additional advective flux components.
In more complex environments, like coastal oxic sediments, inhabited by macrofauna, overflowed by currents and affected by resuspension events, the sediment surface represents an interface between turbulent and calm conditions, high and low concentrations and/or different redox-states. Such gradients are the basis for intensive exchange processes. The surface sediments in the coastal sites of the southern Baltic Sea were characterized by active organic matter mineralization via sulfate reduction and mixing induced secondary reactions taking place in the suboxic zone. This included the removal of dissolved sulfide due to iron oxide reduction with simultaneous liberation of PO4 into the interstitial waters. High surface near P reservoirs existed due to internal P cycling within the sediments, which was in turn driven by continuous re-oxidation of the reduced iron by downwards transported oxygen. These reservoirs were only actually released into the water column during bottom water oxygen deficiency situations, when the iron re-oxidation was inhibited.
This also applies for sediments of the Gulf of Finland and the deeper Baltic Sea basins Bornholm Basin and Gdanks basin, where temporary hypoxic conditions are responsible for recurrent benthic phosphate release.
The widespread occurring phosphate adsorption on sedimentary solid iron phases is a much debated ecosystem service of marine sediments. As discussed in this work, the sedimentary P liberation rates and pools of readily bio-available dissolved phosphate can be substantial in Baltic Sea muddy sediments. Actual phosphate fluxes across the sediment-water interface, though, are relatively small because phosphate is scavenged by adsorption on iron oxyhydroxides that are usually an integral part of coastal marine sediments if overlain by oxic bottom waters. Although muddy sediments often show only an oxic layer of only few millimeters thickness, adsorption capacities of iron oxyhydroxides are large enough to substantially retain P from being liberated into the water column. Falling under reducing conditions, iron oxyhydroxides are re-dissolved, liberating high amounts of PO4 into the surrounding waters. While permanently oxic sediments will preserve adsorbed P, permanently anoxic sediments steadily release mineralized P into the water column. However, sedimentary environments of oscillating redox conditions are predestined for high, burst-like benthic P fluxes. Especially in a quasi isolated environment like the Baltic Sea, with high nutrient inputs but only few sinks, these internal recycling processes promote eutrophication in the long-term. Further expanding hypoxia and anoxia in the Baltic Sea with a subsequent loss of benthic fauna and altered nutrient dynamics in the surface sediments may be the consequence.