Yusufcabrera8524

Straightforward sediment transport is not common in nature and material is storage during transport and reworked by the same processed that lead to initial mass erosion. Despite the development of quantitative assessment by application high accuracy topography measurement, lack of conceptualisation and combination with precise elevation model changes is still missing. This paper presents a field-based channel-bluff connectivity study based on a sediment cascade approach. A TLS (terrestrial laser scanning) time-series database was generated by systematic monitoring of cut-bluff slope surface of the braided-wandering Belá River. The database was used to estimate volume changes and allowed to develop the conceptualisation model of coupling of cut-bluff slope based on spatial and temporal analyses of channel hydrology, gravity conditioned transformation of matter and a detailed of sediment budget calculations. Historical analyses have shown that a flow direction perpendicular to the slope is crucial to activate cut-bluff slope material movement and initiate a sediment cascade, as significant contributors of sediment into the river. Sediment supply to the channels correlates with the magnitude of flood events (maximum discharge, cumulative discharge, cumulative discharge higher than RI1.5, and duration of discharges higher than RI1.5) and lateral migration as a main factor controlling the behaviour of the cut-bluff slope-channel system. During the survey from March 2016 to November 2018, were transported 10,103 m3 (25,964 t) of fine-grained sediment into the river channel.This study investigates the influence of marine habitats (i.e., the intertidal zone, supralittoral zone, and seawater), and polymer types (i.e., polyethylene, PE; polyethylene terephthalate, PET) on the diversity and structure of bacterial communities in marine microplastics. A three-month exposure experiment was conducted in Zhairuoshan Island, Zhoushan, China, a typical caldera volcanic island with minor anthropogenic disturbances. At the end of the exposure period, the transition for peaks corresponding to oxidized groups was observed using micro-Fourier transform infrared spectroscopy. Damages, including pits and cracks, and microorganisms were observed on the surfaces of the PE and PET pellets using scanning electron microscopy. Next-generation amplicon sequencing of the bacterial communities that had colonized the microplastics revealed that bacterial composition significantly varied depending on marine habitats and exposure times, rather than polymer type. Plastic debris in the intertidal zone exhibited the highest bacterial richness and diversity, and Bacillus was considered a potential degrader of plastic debris. The findings demonstrate that bacterial communities that colonize on microplastics are more potentially shaped by marine habitat and exposure time, and this would deepen our understanding of the ecological niche of microplastics surface.The consecutive occurrence of drought and reduction in natural water availability over the past several decades requires searching for alternative water sources for the agriculture sector in California. One alternative source to supplement natural waters is oilfield produced water (OPW) generated from oilfields adjacent to agricultural areas. For over 25 years, OPW has been blended with surface water and used for irrigation in the Cawelo Water District of Kern County, as permitted by California Water Board policy. This study aims to evaluate the potential environmental impact, soil quality, and crop health risks of this policy. We examined a large spectrum of salts, metals, radionuclides (226Ra and 228Ra), and dissolved organic carbon (DOC) in OPW, blended OPW used for irrigation, groundwater, and soils irrigated by the three different water sources. We found that all studied water quality parameters in the blended OPW were below current California irrigation quality guidelines. Yet, soils irrigated by blended OPW showed higher salts and boron relative to soils irrigated by groundwater, implying long-term salts and boron accumulation. We did not, however, find systematic differences in 226Ra and 228Ra activities and DOC in soils irrigated by blended or unblended OPW relative to groundwater-irrigated soils. Based on a comparison of measured parameters, we conclude that the blended low-saline OPW used in the Cawelo Water District of California is of comparable quality to the local groundwater in the region. Nonetheless, the salt and boron soil accumulation can pose long-term risks to soil sodification, groundwater salinization, and plant health; as such, the use of low-saline OPW for irrigation use in California will require continual blending with fresh water and planting of boron-tolerant crops to avoid boron toxicity.The influence of temperature on soil ammonia (NH3) and nitrite (NO2-) oxidation and related NO2- accumulation in soils remain unclear. The soil potential NH3 oxidation (PAO) and NO2- oxidation (PNO) rates were evaluated over a temperature gradient of 5-45 °C in six greenhouse vegetable soils using inhibitors. The values of temperature sensitivity traits such as temperature minimum (Tmin), temperature optimum (Topt), and maximum absolute temperature sensitivity (Tm_sens) were also fitted to the square root growth (SQRT) and macromolecular rate theory (MMRT) models. The ammonia-oxidizing archaea (AOA) and bacteria (AOB) were determined by quantifying amoA, and nitrite-oxidizing bacteria (NOB) were determined by quantifying the nxrA and nxrB. Both models identified that Topt for PAO (34.0 °C) was significantly greater than that for PNO (26.0 °C). The Tm_sens (23.4 ± 2.1 °C) and Tmin (1.0 ± 2.0 °C) for PAO were higher than those for PNO (16.8 ± 3.2 °C and - 11.7 ± 6.7 °C). PAO was positively correlated with AOB-amoA at 20-30 °C and with AOA-amoA at 30-35 °C, while PNO was positively correlated with nxrB at 5-30 °C. click here Additionally, NO2- and N2O were positively correlated with the (AOA + AOB amoA) to (nxrA + nxrB) ratio, and the concentration of N2O was positively correlated with NO2- accumulation. These results highlight that elevated temperatures resulted in the uncoupling of NH3 oxidation and NO2- oxidation, leading to NO2- accumulation, which could stimulate N2O emissions.