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  1. Article ; Online: Distribution and storage of soil organic and inorganic carbon in steppe riparian wetlands under human activity pressure

    Xinyu Liu / Xixi Lu / Ruihong Yu / Heyang Sun / Xiangwei Li / Xiang Li / Zhen Qi / Tingxi Liu / Changwei Lu

    Ecological Indicators, Vol 139, Iss , Pp 108945- (2022)

    2022  

    Abstract: Soil organic carbon (SOC) and soil inorganic carbon (SIC) are key components of the global wetland soil carbon pool, which plays a crucial role in carbon cycling. However, research on carbon storage in riparian wetland soils, especially in inland steppe ... ...

    Abstract Soil organic carbon (SOC) and soil inorganic carbon (SIC) are key components of the global wetland soil carbon pool, which plays a crucial role in carbon cycling. However, research on carbon storage in riparian wetland soils, especially in inland steppe river environments impacted by human activities, is relatively scarce. Thus, we evaluated the SOC and SIC distributions and storage in riparian wetland soils under the pressure of human activities in the Xilin River Basin (XRB). We collected surface and profile soil samples, determined the SOC and SIC contents, aboveground biomass, and soil physicochemical properties, and calculated the SOC and SIC storage (SOCs and SICs) values. The surface soil SOC content decreased substantially from the upstream to the downstream zones (mean value range: 76.30–3.18 g/kg), and the SIC content showed the opposite trend (mean value range: 0.08–34.38 g/kg). The SIC content of the riparian wetlands along the permanently flowing stretch of river was much lower than that in the wetlands along the intermittently flowing stretch. In the XRB, the SOCs was primarily affected by vegetation coverage, soil water content, and soil pH, whereas the SICs was greatly affected by soil texture. A dry lake zone was markedly affected by wetland degradation, indicating a potential increase in the decomposition rate of the surface soil SOC; however, the SOC in the deep soils was relatively stable. The high SIC content most likely resulted from weathering, resuspension, and carbonate rock reprecipitation. Compared to different steppe grassland types, riparian wetlands appear to be potential hotspots of SOCs and SICs in the Inner Mongolian region. Riparian wetland SOCs in the upstream zones was substantially greater than in adjacent terrestrial locations. However, the SOCs in the downstream wetlands was similar to that in the grasslands. Under the impact of human activities, the water and soil environments in the downstream zone of the Xilin River were substantially modified, leading to severe wetland ...
    Keywords Riparian wetlands ; Soil organic carbon ; Soil inorganic carbon ; Storage ; Human activities ; Wetland degradation ; Ecology ; QH540-549.5
    Subject code 550
    Language English
    Publishing date 2022-06-01T00:00:00Z
    Publisher Elsevier
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  2. Article ; Online: Greenhouse gas emissions from the water-air interface of a grassland river: a case study of the Xilin River.

    Hao, Xue / Ruihong, Yu / Zhuangzhuang, Zhang / Zhen, Qi / Xixi, Lu / Tingxi, Liu / Ruizhong, Gao

    Scientific reports

    2021  Volume 11, Issue 1, Page(s) 2659

    Abstract: Greenhouse gas (GHG) emissions from rivers and lakes have been shown to significantly contribute to global carbon and nitrogen cycling. In spatiotemporal-variable and human-impacted rivers in the grassland region, simultaneous carbon dioxide, methane and ...

    Abstract Greenhouse gas (GHG) emissions from rivers and lakes have been shown to significantly contribute to global carbon and nitrogen cycling. In spatiotemporal-variable and human-impacted rivers in the grassland region, simultaneous carbon dioxide, methane and nitrous oxide emissions and their relationships under the different land use types are poorly documented. This research estimated greenhouse gas (CO
    Language English
    Publishing date 2021-01-29
    Publishing country England
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ZDB-ID 2615211-3
    ISSN 2045-2322 ; 2045-2322
    ISSN (online) 2045-2322
    ISSN 2045-2322
    DOI 10.1038/s41598-021-81658-x
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  3. Article: Major ion chemistry in the headwater region of the Yellow River: impact of land covers

    Yuanrong, Su / Ruihong, Yu / Mingyang, Tian / Xiankun, Yang / Lishan, Ran / Haizhu, Hu / Zhuangzhuang, Zhang / Xixi, Lu

    Environmental earth sciences. 2021 June, v. 80, no. 11

    2021  

    Abstract: Research on the ionic chemistry of rivers and weathering types provides the basis for elucidating the dynamics of river chemistry and exploring carbon cycling in river systems. There is a lack of water chemistry study in the river systems in the Tibet ... ...

    Abstract Research on the ionic chemistry of rivers and weathering types provides the basis for elucidating the dynamics of river chemistry and exploring carbon cycling in river systems. There is a lack of water chemistry study in the river systems in the Tibet Plateau, especially in the streams/rivers flowing from and through glaciers and permafrost. Samples in the rivers flowing through different land covers (lakes, glaciers, permafrost, grasslands, peatlands) were collected in different months (April, June, August and October) in 2016, covering various hydrological regimes. The temporal and spatial dynamic variations of major ions and the underlying causes were explored. The results revealed that in the headwater region Ca²⁺ and HCO₃⁻ were the dominant ions, derived primarily from the dissolution of carbonatites and evaporates. However, the concentrations of ions from different land covers were vastly different.The high concentrations of Na⁺ and K⁺ in the lakes sample were mainly affected by evaporation and precipitation. The acid deposition caused by atmospheric pollutants resulted in high concentration of SO₄²⁻ in glacial and permafrost streams. K⁺ concentration was high in the grassland region with frequent agricultural activities such as the planting and fertilization of highland barleys that applied nitrogen and potassium fertilizers. Although Total Dissolved Load (TDS) was higher for the lakes and streams/rivers from glaciers and permafrost, and its average (287.28 ± 40 mg/L) over the headwater region was lower than that in the middle and lower reaches of the Yellow River because of low temperature. The current study provided the basis of and reference for the overall water chemistry characteristics and carbon cycling processes of the entire Yellow River.
    Keywords acid deposition ; calcium ; carbon ; evaporation ; grasslands ; hydrochemistry ; nitrogen ; peatlands ; permafrost ; potassium ; rivers ; temperature ; water ; China ; Yellow River
    Language English
    Dates of publication 2021-06
    Size p. 398.
    Publishing place Springer Berlin Heidelberg
    Document type Article
    Note NAL-AP-2-clean
    ZDB-ID 2493699-6
    ISSN 1866-6299 ; 1866-6280
    ISSN (online) 1866-6299
    ISSN 1866-6280
    DOI 10.1007/s12665-021-09692-6
    Database NAL-Catalogue (AGRICOLA)

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  4. Article: Interactive effects of hydrological conditions on soil respiration in China's Horqin sandy land: An example of dune-meadow cascade ecosystem

    Han, Chunxue / Ruihong Yu / Xixi Lu / Limin Duan / Vijay P. Singh / Tingxi Liu

    Science of the total environment. 2019 Feb. 15, v. 651

    2019  

    Abstract: Soil moisture (Ms) strongly influences dynamic changes in soil respiration (Rs) and is thus an important factor when predicting soil carbon emissions. However, the various sources of Ms (rainfall, groundwater, and condensation) exert complicated and ... ...

    Abstract Soil moisture (Ms) strongly influences dynamic changes in soil respiration (Rs) and is thus an important factor when predicting soil carbon emissions. However, the various sources of Ms (rainfall, groundwater, and condensation) exert complicated and uncertain effects on Rs. This study examined the growth seasonal variation (from April to October) of Rs and the diurnal variation in a cascade ecosystem consisting of sandy bare ground, a transitional artificial Populus forest, and a meadow Phragmites communis community in China's Horqin sandy land. Simultaneous measurements of the 0–10 cm depth soil temperature (Ts) and Ms, rainfall, the surface air relative humidity and the groundwater depth were collected. The results revealed that in sandy bare ground with Ms below field capacity, Ms had a greater impact on Rs than Ts, and rainfall could increase Rs. The effect of condensation on Rs during periods of continuous drought could not be ignored. In the meadowlands with Ms above field capacity, the groundwater affected Rs indirectly by regulating Ms and the relationship with Ts, and rainfall had an adverse effect on Rs. The effects of rainfall, Ms and Ts on Rs were minimum as Ms approached the saturation water content. In the transitional forest, Ms and Ts were the main factors controlling Rs. The most favorable Ms for Rs was close to the field capacity. The results emphasize that field capacity and saturation water content are the demarcation points of a soil carbon emissions prediction model, and the effect of different hydrological conditions and Ts on Rs at each segment are reconsidered accordingly. Ultimately, the carbon emission patterns of the cascade ecosystems in arid and semi-arid areas are extremely complicated and have to be considered specially for estimating terrestrial carbon emissions.
    Keywords Phragmites australis ; Populus ; adverse effects ; carbon ; diurnal variation ; drought ; ecosystems ; emissions ; field capacity ; forests ; groundwater ; meadows ; models ; prediction ; rain ; seasonal variation ; semiarid zones ; soil respiration ; soil temperature ; soil water ; water content ; water table ; China
    Language English
    Dates of publication 2019-0215
    Size p. 3053-3063.
    Publishing place Elsevier B.V.
    Document type Article
    ZDB-ID 121506-1
    ISSN 1879-1026 ; 0048-9697
    ISSN (online) 1879-1026
    ISSN 0048-9697
    DOI 10.1016/j.scitotenv.2018.10.198
    Database NAL-Catalogue (AGRICOLA)

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  5. Article ; Online: Diurnal Variation of Light Absorption in the Yellow River Estuary

    Yanling Hao / Tingwei Cui / Vijay P. Singh / Jie Zhang / Ruihong Yu / Wenjing Zhao

    Remote Sensing, Vol 10, Iss 4, p

    2018  Volume 542

    Abstract: Considering the influence of river discharge and strong winds, the diurnal variability of ocean optical absorption properties in the Yellow River Estuary (YRE) is quantified, using in-situ measurements. The study finds that terrestrial sources due to the ...

    Abstract Considering the influence of river discharge and strong winds, the diurnal variability of ocean optical absorption properties in the Yellow River Estuary (YRE) is quantified, using in-situ measurements. The study finds that terrestrial sources due to the Yellow River discharge can cause high diurnal variation of water absorption because of the movement of river plume in the YRE, but such an influence diminishes far away from the Yellow River plume. The diurnal variability of water absorption, affected by strong winds, is found to be strengthened with a rapid increase of particles and colored dissolved organic matter (CDOM) arising from re-suspended sediment induced by wave forcing. The diurnal variability of particle absorption is controlled by non-algal particle absorption in the YRE, and the ratio of non-algal particle absorption (aNAP) and total particle absorption for most wavelengths is more than 0.56. The diurnal variation of spectral slope of non-algal particle absorption (SNAP) is found to vary within a narrow range, although large variability in the aNAP spectrum is observed. The CDOM is correlated negatively with salinity, and such negative correlation becomes weaker with the decreasing influence of riverine input. The spectral slope of CDOM absorption (Sg) may reflect the formation and constituents of CDOM with weak relationship to its concentration, and its relationship with the absorption of CDOM at 440 nm may be associated with the source of CDOM. The value of Sg, which is affected by re-suspended bottom sediment, is much lower than that derived from CDOM affected by Yellow River runoff. Disregarding the absorption of pure water, the diurnal variability of total water absorption stems principally from changes in non-algal particle matter rather than CDOM and Chl-a. By the observations of hourly GOCI (Geostationary Ocean Color Imager) data, the major diurnal variations of remote sensing reflectance at 680 nm are observed in near-coastal waters and the estuary of the Yellow River, which are mainly ...
    Keywords Yellow River Estuary ; diurnal variation ; optical properties ; colored dissolved organic matter (CDOM) ; non-algal particles ; suspended particle matter (SPM) ; Science ; Q
    Subject code 550
    Language English
    Publishing date 2018-04-01T00:00:00Z
    Publisher MDPI AG
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  6. Article ; Online: A New Method for Mapping Aquatic Vegetation Especially Underwater Vegetation in Lake Ulansuhai Using GF-1 Satellite Data

    Qi Chen / Ruihong Yu / Yanling Hao / Linhui Wu / Wenxing Zhang / Qi Zhang / Xunan Bu

    Remote Sensing, Vol 10, Iss 8, p

    2018  Volume 1279

    Abstract: It is difficult to accurately identify and extract bodies of water and underwater vegetation from satellite images using conventional vegetation indices, as the strong absorption of water weakens the spectral feature of high near-infrared (NIR) reflected ...

    Abstract It is difficult to accurately identify and extract bodies of water and underwater vegetation from satellite images using conventional vegetation indices, as the strong absorption of water weakens the spectral feature of high near-infrared (NIR) reflected by underwater vegetation in shallow lakes. This study used the shallow Lake Ulansuhai in the semi-arid region of China as a research site, and proposes a new concave–convex decision function to detect submerged aquatic vegetation (SAV) and identify bodies of water using Gao Fen 1 (GF-1) multi-spectral satellite images with a resolution of 16 meters acquired in July and August 2015. At the same time, emergent vegetation, “Huangtai algae bloom”, and SAV were classified simultaneously by a decision tree method. Through investigation and verification by field samples, classification accuracy in July and August was 92.17% and 91.79%, respectively, demonstrating that GF-1 data with four-day short revisit period and high spatial resolution can meet the standards of accuracy required by aquatic vegetation extraction. The results indicated that the concave–convex decision function is superior to traditional classification methods in distinguishing water and SAV, thus significantly improving SAV classification accuracy. The concave–convex decision function can be applied to waters with SAV coverage greater than 40% above 0.3 m and SAV coverage 40% above 0.1 m under 1.5 m transparency, which can provide new methods for the accurate extraction of SAV in other regions.
    Keywords aquatic vegetation ; concave–convex decision function ; remote sensing extraction ; GF-1 satellite ; Lake Ulansuhai ; China ; Science ; Q
    Subject code 550
    Language English
    Publishing date 2018-08-01T00:00:00Z
    Publisher MDPI AG
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  7. Article: Ecological Regime versus Minimum Environmental Flow:Comparison of Results for a River in a Semi Mediterranean Region

    Nikghalb, Saeed / Alireza Shokoohi / Ruihong Yu / Vijay P. Singh

    Water resources management. 2016 Oct., v. 30, no. 13

    2016  

    Abstract: Maintaining Environmental Flow (EF) plays a critical role in protecting rivers and their ecosystems. Because of shortage of data and limited financial resources in developing countries, there is a tendency to use simple hydrologic methods against ... ...

    Abstract Maintaining Environmental Flow (EF) plays a critical role in protecting rivers and their ecosystems. Because of shortage of data and limited financial resources in developing countries, there is a tendency to use simple hydrologic methods against comprehensive EF assessment methods. In this research, two most common hydrologic methods (Tennant and Q95) were compared with a habitat simulation method (PHABSIM) under the condition of data shortage. It was concluded that while the results of habitat simulation method even using imprecise input data were justified, the impacts of implementing EF discharges of the two hydrologic methods on the ecosystem might be irreversible. It was found that the Tennant and Q95 methods led to dramatically low discharges as fixed minimum environmental flows, while habitat simulation method gave an acceptable ecological regime. In the absence of ecological data and after deciding on the target species in a case study in the southern part of the Caspian Sea, a special Delphi technique was employed for preparing the suitability data. For enhancing the PHABSIM hydraulic module results, HEC-RAS was implemented for hydraulic simulation and then with a simple modification on average velocity, the cross-sectional velocity distribution for deriving the Weighted Usable Area (WUA) was generated. It was found that this method along with maintaining high flows in the river preserved Mean Annual Flow (MAF) during wet months and preserved Mean Annual Low Flow (MALF) during dry months which is equal to maintaining Environmental Flow Requirement (EFR) in such a way that provides the river with an ecological regime near its historical one and guarantees river health.
    Keywords case studies ; developing countries ; ecosystems ; habitats ; hydrologic models ; rivers ; stream flow ; Caspian Sea ; Mediterranean region
    Language English
    Dates of publication 2016-10
    Size p. 4969-4984.
    Publishing place Springer Netherlands
    Document type Article
    ZDB-ID 59924-4
    ISSN 1573-1650 ; 0920-4741
    ISSN (online) 1573-1650
    ISSN 0920-4741
    DOI 10.1007/s11269-016-1488-2
    Database NAL-Catalogue (AGRICOLA)

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  8. Article: Chemical denudation in the Yellow River and its geomorphological implications

    Ran, Lishan / Huiguo Sun / Jingtai Han / Ruihong Yu / X.X. Lu

    Geomorphology. 2015 Feb. 15, v. 231

    2015  

    Abstract: Chemical denudation plays an important role in regulating atmospheric CO2 balance and modulating global climate. With weekly collected water samples at three stations on the Yellow River mainstem from July 2011 to July 2012, we investigate its chemical ... ...

    Abstract Chemical denudation plays an important role in regulating atmospheric CO2 balance and modulating global climate. With weekly collected water samples at three stations on the Yellow River mainstem from July 2011 to July 2012, we investigate its chemical denudation characteristics on the basis of water geochemistry and discuss the geomorphological implications. Because of limited atmospheric inputs into the Yellow River, chemical weathering is of first importance in affecting the chemical compositions of its water geochemistry. As a result of extensive carbonates within the watershed, carbonate dissolution is the major source of the dissolved solids, accounting for 28–33.7% of the total dissolved solids (TDS). In contrast, silicate weathering contributes only 9.9–10.9%. With a mean TDS concentration of 639mgl−1, the TDS flux into the ocean is estimated at 16Mtyr−1, corresponding to a specific chemical denudation rate of 21.3tkm−2yr−1. Comparative analysis with physical erosion suggests the dominance of physical erosion over chemical weathering in providing riverine loads. Rapid removal by physical erosion may have restrained the chemical denudation processes. Rock weathering consumes, on average, 2.3Mt of atmospheric CO2 during the one-year-long sampling campaign, accounting for 0.22–0.31% of the global annual CO2 consumption through chemical weathering. Of the CO2 consumed, 74% is caused by carbonate weathering and 26% by silicate weathering, indicating the predominance of carbonate weathering in consuming atmospheric CO2 within the watershed.
    Keywords carbon dioxide ; carbonates ; climate ; geochemistry ; geomorphology ; silicates ; total dissolved solids ; watersheds ; weathering ; Yellow River
    Language English
    Dates of publication 2015-0215
    Size p. 83-93.
    Publishing place Elsevier B.V.
    Document type Article
    ZDB-ID 58028-4
    ISSN 0169-555X
    ISSN 0169-555X
    DOI 10.1016/j.geomorph.2014.12.004
    Database NAL-Catalogue (AGRICOLA)

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