Relevant bibliographies by topics / White River (Ind. : River)

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Academic literature on the topic 'White River (Ind. : River)'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "White River (Ind. : River)"

1

Dramane Ouattara, Romuald Sonan Assi, Charles Koffi Boussou, and Séraphin Kouakou Konan. "Diversity and degree of organization of the Ichthyofauna of two branches of the Bandama river in the Marahoue region (Central West of Côte D’Ivoire)." International Journal of Science and Research Archive 3, no. 1 (July 30, 2021): 062–70. http://dx.doi.org/10.30574/ijsra.2021.3.1.0108.

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Diversity and Degree of organization of the ichthyological population of two tributaries of the Bandama River in the Marahoue region located in the center-west of Côte d'Ivoire were studied. Indeed, the two tributaries of the Bandama River that are Marahoue and White Bandama Rivers draining this region are subject to numerous disturbances, the main one being gold panning. Data collection was conducted from September 2019 to November 2020 from experimental and artisanal fisheries. The mesh sizes of the gillnets used for the experimental fishery varied from 10 to 40 mm mesh size. The results showed a dominance of the order Siluriformes represented by 6 families and 18 species in the Marahoue River against 4 families and 13 species in the White Bandama River. Also, the Shannon Index (H') values obtained in the White Bandama River (H' fluctuates from 2.26 to 2.33 bits/ind) are lower than those obtained in the River Marahoue (H' fluctuates from 3.02 to 3.14 bits/ind). Our results also highlighted the equitability. This index appeared relatively high in the Marahoue River (E varies from 0.77 to 0.80) compared to the White Bandama River (E varies from 0.5 to 0.57). Consequently, the Marahoue River appears to be more stable and has a good degree of organization of the ichthyological population compared to the White Bandama River.
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Bhuiyan, Mohammad Azmal Hossain, and Moniruzzaman Khondker. "Water quality and potamoplankton of the river Buriganga and Gomti: A comparison." Dhaka University Journal of Biological Sciences 27, no. 2 (July 20, 2018): 191–200. http://dx.doi.org/10.3329/dujbs.v27i2.46467.

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The studied section of the river Buriganga besets with urban catchment contained higher values of pH, alkalinity, CO2, conductivity, TDS, SRP, SRS and NO3-N concentration compared to its counterpart, namely a section of the river Gomti having rural catchment characteristics. The mean values for a period of six months for the river Buriganga were 8.34, 1.48 meq/l, 8.49 mg/l, 686 μS/cm, 155.17 mg/l, 493 μg/l, 36.07 mg/l and 810.28 μg/l for pH, alkalinity, CO2, conductivity, TDS, SRP, SRS and NO3-N, respectively. While the same for the river Gomti was 7.86, 1.18 meq/l, 5.42 mg/l, 284.44 μS/cm, 79.91 mg/l, 188.37 μg/l, 26.41 mg/l and 203.99 μg/l, respectively for pH, alkalinity, CO2, conductivity, TDS, SRP, SRS and NO3-N. In the river Gomti, the concentration of DO was better (7.87 mg/l) compared to that of river Buriganga (5.53 mg/l). Because of a hilly origin of the river Gomti and availability of sediments in its water, the underwater light climate was poor compared to the river Buriganga. The Secchi depth recorded for Gomti and Buriganga were 0.26 and 0.54 m, respectively. Both the rivers were found diatom dominant in terms of population but the species prevailed were different. Fragillaria virescens Ralfs was the dominant diatom of the river Buriganga. Its density ranged from 6.5-11.09×105 ind/l which was the highest compared to the population of all other groups of potamoplankton. In Gomti another diatom namely, F. pinnata Ehrenberg was dominant and the density of which ranged from 8.45 - 12.65 × 105 ind/l. Community structure of the potamoplankton revealed 30 species from the river Buriganga and 22 species from Gomti. The study reveals that relatively higher concentration of nutrients prevails in the water of the river course having urban catchment characters compared to the rural ones. Dhaka Univ. J. Biol. Sci. 27(2): 191-200, 2018 (July)
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Koshelev, V. N., and N. V. Kolpakov. "Species composition and distribution of fishes and prawns in the Amur River channel." Izvestiya TINRO 200, no. 2 (July 5, 2020): 292–307. http://dx.doi.org/10.26428/1606-9919-2020-200-292-307.

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istribution of fishes and prawns in the Amur River (40–960 km from the mouth) is described on results of the beam-trawl survey conducted in September-October, 2003 (57 trawl stations at the depth of 1.5–23.0 m). In total, 2584 ind. of 22 fish species and 1077 ind. of 1 invertebrate species (prawn Palaemon modestus) were caught. The highest species richness was registered for orders Cypriniformes (13 species) and Siluriformes (4 species). The fish and prawn stocks were evaluated as 32.161 . 106 ind. (583.8 t) for bottom and near-bottom fish and 4.887 . 106 ind. (8.8 t) for prawns. Two commercial fish species were the most abundant: catfishes Tachysurus brashnikowi (16.26 . 106 ind. or 32.9 % of total biomass) and T. sinensis (4.32 . 106 ind. or 24.0 % of total biomass); other 6 fish species with considerable biomass were lizard gudgeon Saurogobio dabryi (12.6 %), ussuri catfish T. ussuriensis (9.7 %), amur white-pinned gudgeon Romanogobio tenuicorpus (7.8 %), amur sturgeon Acipenser schrenckii (5.6 %), amur gudgeon Gobio cynocephalus (2.4 %), and kaluga Huso dauricus (0.6 %). Distribution density varied in the range of 0.01–2.57 g/m2 (on average 0.45 ± 0.27 g/m2) for fish and 0.005–0.044 g/m2 (0.021 ± 0.012 g/m2) for prawns. Abundance of both fish and prawns increased multifold towards the Amur mouth that correlated with increasing of forage benthos biomass in the same direction. So, the main portion of fish biomass (82.4 %) was distributed in the Amur River downstream (40–400 km from the mouth) and the prawn stock was concentrated completely in its lowermost part (50–150 km from the mouth).
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Widyarini, Happy, Niken T. M. Pratiwi, and Sulistiono. "ZOOPLANKTON COMMUNITY STRUCTURE AT MAJAKERTA ESTUARY AND ITS SURROUNDING WATERS, INDRAMAYU REGENCY, WEST JAVA PROVINCE." Jurnal Ilmu dan Teknologi Kelautan Tropis 9, no. 1 (November 2, 2017): 91–103. http://dx.doi.org/10.29244/jitkt.v9i1.17919.

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Majakerta estuary and its surrounding waters have a high potential fishery resource which is commonly utilized by the community around the area. Fluctuation of physical and chemical parameters of the waters and fishery activities around the estuary can influence the existence of zooplankton. This study was conducted from December 2014 to May 2015. Samples of the zooplankton were collected monthly at four stations (consisted of sea, river and estuary areas). Based on the study, zooplankton in the Majakerta estuary and its surrounding waters consisted of six classes; i.e. Protozoa (11 genera), Crustaceae (4 genera, 1 nauplius stadia), and Rotifera (4 genera). A higher abundance was found at the sea (29025 ind./m3), while a lower abundance was at the river and estuary (7147 ind./m3 dan 7582 ind./m3). Based on the zooplankton diversity index, it can be inferred that the value was relatively low. There were two habitat groups, namely Station Group 1 (Station 1 and 2; river and estuary) and Station Group 2 (Station 3 and 4; sea) with influencing parameters such as transparency, pH, and salinity. Keywords: estuary, Majakerta, zooplankton, community structure
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Winarti, Winarti, and Arman Harahap. "The Diversity of Makrozoobenthos as Bio-Indicators of Water Quality of the River Kundur District Labuhanbatu." Budapest International Research and Critics Institute (BIRCI-Journal): Humanities and Social Sciences 4, no. 1 (February 15, 2021): 1027–33. http://dx.doi.org/10.33258/birci.v4i1.1732.

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Macrozoobenthos used as a bioindicator of the waters, this happens because of the nature of the benthos which has mpergerakan low so it got a lot of influence from the environment. This study aims to determine the condition of the river Kundur with a view the community structure of macrozoobenthos which include: species composition, abundance, diversity, uniformity and dominance as well as the physical and chemical parameters of water as a paremeter supporters. Based on the results of observations, macrozoobenthos were found during the study in the river Kundur consists of 3 phylum, 4 classes, 17 family with 11 species. The composition of the class of macrozoobenthos in the whole of the observation station consists of a Gastropod (37%), Insecta (23%), Malacostraca (20%), Polychaeta (10%) dan Malacostraca (20%). The value of an abundance ranged from 325,7 - 3309,6 ind/m3. With the value of the total abundance at Station I which is equal to 3690,1 ind/m3, Station II 3723,1 ind/m3, Station III 3692,3 ind/m3 can be categorized diversity are light polluted with the value of the index of uniformity (E) that describes the spread of the individual tends to be uniform or relatively the same. While the condition of the physical-chemical parameters and the substrate bottom of the river Kundur in general has a range of relatively homogeneous, spread evenly throughout the observation stations and still be able to support life macrozoobenthos. To the results of measurements of the parameters of physico-chemical water and substrate in the river kundur in general has a range of relatively homogeneous in the whole observation stations and still be able to support the life of the macrozoobenthos.
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Et al., Ajeel. "Diversity, Abundance, and Distribution of Cladocera at the end of the Tigris River North of Basrah – IRAQ." Baghdad Science Journal 16, no. 4 (December 1, 2019): 0854. http://dx.doi.org/10.21123/bsj.2019.16.4.0854.

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Seasonal variations of the species composition and abundance of Cladocera were studied in two stations at the end of the Tigris River and one station at the confluence of the Tigris with Euphrates area, at the beginning of the Shatt Al-Arab River in Al-Qurnah North of Basrah Province, from October 2015 to August 2016. Samples of zooplankton were collected by plankton net 100-µm. mesh size. The population density of Cladocera ranged between 1 Ind /m³ during summer and 211 Ind./m³ during winter at station 1 (Al-Jewaber Bridge). A total of 16 species of Cladocera belonging to 12 genera were recorded in the study. The average density of Cladocera ranged from 23.2 ind./m3 at Station 2 (Hamayon Bridge) to 53.7 Ind./m3 at Station 1 (Al-Jewaber Bridge). The results showed that the Bosmina meridionalis was dominant at the three stations 47.8%, while the other species were as follow Moina affinis 15.1%, Daphnia lumholtzi 9.3%, Simocephalus (Simocephalus) vetuloides 8.1% and Daphnia exilis 6.6% of the total Cladocera.
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Kawirian, Rizky Regina, Arif Nurcahyanto, Didit Abdillah, Grin Tommy Panggabean, Muhammad Irfan Afif, Ahyar Pulungan, Chichilia Qaila Azzahra Rahman, Mursalin Ishak, and Majariana Krisanti. "Produktivitas Sekunder Organisme Bentik (Ordo Diptera) di Sungai Cigambreng, Desa Tapos, Kecamatan Tenjolaya, Kabupaten Bogor, Jawa Barat." Journal of Tropical Fisheries Management 4, no. 1 (May 29, 2020): 43–48. http://dx.doi.org/10.29244/jppt.v4i1.30904.

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Insekta has biodiversity with a wide distribution throughout the world. Sampling was carried out once a week during October 2019. A total of 717 specimens of Order Diptera were found which covered two families in the Cigambreng River. Each family obtained includes one type, Antocha sp. (Family Tipulidae.) and Krenopelopia sp. (Chironomidae). The presence of a chironomid has indicates an excessive input load (pollutant) into the waters of the Cigambreng River. In general, the highest abundance was obtained at the fourth observation, 284 ind/m2, while the lowest abundance was obtained at the second observation, which was 60 ind/m2. Secondary productivity covers P/B ratio of 3.034 /month with a production speed of 14.2458 (g/m2/month) and biomass (4.6954 g/m2).
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Susilo, Hendri, Musrifin Ghalib, and Aras Mulyadi. "MAPPING OF MANGROVE VEGETATION USING LANDSAT SATELLITE IMAGERYIN THE ESTUARY OF GANGSAL RIVER INDRAGIRI HILIR REGENCY RIAU PROVINCE." Asian Journal of Aquatic Sciences 2, no. 3 (January 24, 2020): 181–89. http://dx.doi.org/10.31258/ajoas.2.3.181-189.

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The research was conducted in January - March 2019. This study aims to map and analyze changes in the area and density of mangrove vegetation based on NDVI values and community structure in the Muara Sungai Gangsal, Indragiri Hilir Regency. To analyze the area and density of NDVI using Landsat 5 TM satellite imagery in 2008 and Landsat 8 OLI/TIRS in 2018. Analysis using ArcGis 10.3 software. The calculation of mangroves based on community structure used the Transect Line Plot method at 6 stations for community structure sampling. The area of mangrove vegetation in 2008 was 2,706 ha and in 2018 it was 2,693 ha. The results of the analysis of mangrove vegetation area from 2008 to 2018 there was a reduction of 13 ha. The NDVI value for 2008 criteria is rarely 133 ha, while 2.009 ha are wide and 564 ha is dense. The NDVI value of the 2018 mangrove vegetation is rarely 16 hectares, while 2,135 hectares are in the area and 542 hectares are dense. Based on the analysis of mangrove density in 2018 at 6 sampling point stations ranging from 866 ind/ha to 1,522 ind/ha. Density criteria are rarely detected at station I with a density of 922 ind/ha and station II with a density of 866 ind/ha. The criterion of moderate density was detected at station V with a density of 1,255 ind/ha and station VI with a density of 1,044 ind/ha. Criteria for solid density were detected at station III with a density of 1,522 ind/ha and station IV with a density of 1,511 ind/ha.
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Journal, Baghdad Science. "Biodiversity of Rotifera and Cladocera in the upper region of Euphrates River- Iraq." Baghdad Science Journal 4, no. 2 (June 3, 2007): 221–32. http://dx.doi.org/10.21123/bsj.4.2.221-232.

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Five representative sampling stations were selected in upper region of Euphrates river. Bimonthly sampling were collected from December 2000 to December 2001. Rotifera showed high density in December 2000 while high density of cladocera which recorded in October .The results of relative abundance index showed that rotifera: Polyarthera dolichoptera , Keratella cochlearis , K. valga, Cephalodella auriculata and cladocera: Bosmina longirostris , B.coregoni ,Chydorus spharicus, were more abundant in study stations. The results of constancy index showed 4 taxa belonged to rotifera and 2 taxa belonged to cladocera which were considered constant in the Euphrates river, where the other species varied between accessory and accidental species in study stations. The index values of Species richness of rotifera varied between 0.41 – 2.8 and cladocera varied between 0.5 - 1.95. The Shanon-Weiner index of rotifera varied between 0.54-1.72 bit/ind., while the Shanon index of cladocera varied between 0.5-1.6 bit/ind. The uniformity index of rotifera varied between 0.41 – 0.99 but the uniformity index of cladocera varied between 0.61- 0.98 .
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Shevchuk, L., L. Vasilyeva, M. Taradajnyk, and S. Mezhzherin. "Freshwater Mussels (Mollusca, Bivalvia, Unionidae) of the Danube River Basin of Ukraine." Zoodiversity 55, no. 1 (2021): 41–50. http://dx.doi.org/10.15407/zoo2021.01.041.

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During 2009–2011, 50 points of the Daube River Basin were surveyed. In 23 of them, seven species of Unionidae were recorded: U. pictorum, U. tumidus, U. crassus sensu lato, A. anatina, A. cygnea, P. сomplanatа and S. woodiana, which is an invasive species. Th e index of occurrence of freshwater mussels in general was 100 % in the Lower Danube River (5 study areas), 42 % in Tisa River (31 study areas), 33.3 % in Seret River (3 study areas), 36 % in Prut River (11 study areas). Th e index of occurrence of species was rather low: 24 % of A. anatina, 22 % of U. tumidus, 22 % of U. crassus, 16 % of U. pictorum, 14 % of P. complanata, 14 % of S. woodiana, and 2 % of A. cygnea. U. crassus was not found in the Lower Danube river, while A. cygnea was found only there outside the main watercourse. Th e invasive species S. woodiana occurred in the Lower Danube River and in the sub-basin of Tisa River (with 83 % and 20 % frequency, respectively. Th e mean values of population densities ranged from 1.00 (A. cygnea) to 6.14 ind./m2 (S. woodiana), and the mean biomass varied from 1.14 (P. сomplanatа) to 797.54 g/m2 (S. woodiana).
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More sources

Dissertations / Theses on the topic "White River (Ind. : River)"

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Rippey, Heather A. "Daylighting Pogues Run : an urban stream solution." Virtual Press, 2003. http://liblink.bsu.edu/uhtbin/catkey/1259755.

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This creative project has culminated in a design solution to a water quality problem in the City of Indianapolis, Indiana. Pogues Run is a stream that has been buried in an underground culvert for almost a century. It has a long history of water quality problems including high bacteria levels and nonpoint source pollution. In addition, it has long been a flood threat to neighboring communities.To address the issue, a master plan was created for the last 1400' of Pogues Run before it emptied into the White River. The stream was removed from the culvert, brought back up to grade, a series of wetlands were developed to slow and filter stream flow, and an urban revitalization project was developed centering on the stream. The design solution provided flood control, stormwater storage and treatment, mixed-use redevelopment of historical buildings, a recreational area, and a high-density residential community.
Department of Landscape Architecture
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Germano, Nancy M. "A View of the Valley: The 1913 Flood in West Indianapolis." Thesis, Connect to resource online, 2009. http://hdl.handle.net/1805/1844.

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Thesis (M.A.)--Indiana University, 2009.
Title from screen (viewed on August 27, 2009). Department of History, Indiana University-Purdue University Indianapolis (IUPUI). Advisor(s): Philip V. Scarpino. Includes vita. Includes bibliographical references (leaves 165-173).
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Burkett, Frank Newton. "A general regional research design for the prehistoric archaeological resources of the upper White River Drainage Region of east-central Indiana." Virtual Press, 1987. http://liblink.bsu.edu/uhtbin/catkey/485238.

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This is a general regional research design for the prehistoric archaeological resources of the Upper White River Drainage region of east-central Indiana. Following the example of McGinsey, Davis, and Griffin (1968), this design consists primarily of research problems, questions, and hypotheses suggested by the current state of the regional data base and the pertinent literature. These research problems are organized into three basic groups which represent the goals of the discipline of archaeology (that is, the study of culture history, extinct lifeways, and culture process). These groups are themselves expressed as a hierarchy to demonstrate the relative significance of the problems expressed in each. When used as part of a greater research design process (including more specific designs) this design has the potential to contribute to the scientific rigor as well as the efficiency of archaeological research carried out in this region.
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Stephenson, Patricia Ranel. "Results of a survey to locate Woodland sites within the Upper White River valley of east-central Indiana with the intention of determining a positive correlation with Ross soil." Virtual Press, 1988. http://liblink.bsu.edu/uhtbin/catkey/546134.

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A survey of the Upper White River Valley located 76 new sites additional information on 6 previously recorded sites. After a preliminary literature review, artifacts from the Ball State University Archaeology Laboratory were reanalyzed and local artifact collectors were contacted to obtain additional knowledge survey area. The fieldwork focused on the floodplain and the location of Woodland sites in regards to Ross soil. Surface manifestations of Woodland-affiliated sites indicated that 33% of the sites in the project area were located in the floodplain and all Woodland components were represented on or adjacent to Ross soil. Results from the fieldwork indicate a positive correlation between Woodland sites and Ross soil in the Upper White River Valley of east-central Indiana.
Department of Anthropology
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Rockenbach, Stephen I. ""War upon our border" war and society in two Ohio River Valley communities, 1861-1865 /." Cincinnati, Ohio : University of Cincinnati, 2005. http://www.ohiolink.edu/etd/view.cgi?acc%5Fnum=ucin1124462148.

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Griffis, Neil. "Late Eocene Terrestrial Paleoclimatie Record From The White River Formation At Flagstaff Rim, Wyoming, USA." Master's thesis, Temple University Libraries, 2011. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/116961.

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Geology
M.S.
Flagstaff Rim near Casper, WY preserves the most complete late Eocene section of the White River Group with over 219 m of late Eocene age sediment compared to 35 m preserved at Toadstool Park, NE. While Flagstaff Rim does not span the Eocene-Oligocene transition, it holds the earliest clues in the White River Group of a late Eocene (37-34 Ma) climatic deterioration. In this study 8 paleosols were collected, described and analyzed based on pedogenic features, mineralogy, and geochemistry, above and below dated volcanic ash beds. The lowermost paleosol is composed of smectite- rich red mudstone, with greenish gray drab haloes, and weather into hummocks. The sediments within this part of the section are the lithologic equivalent of the Peanut Peak member of Toadstool Park, NE and reflect a moist humid environment. Overlying these sediments is the lithologic equivalent of the Big Cottonwood Creek member. These sediments are comprised of smectite poor mudstones and yellow/beige sandstones, are indurated with calcium carbonate, and reflect a more arid environment. The transitional zone between the Peanut Peak and Big Cottonwood Creek lithologies corresponds with an increase in volcanism from the Great Basin, impact events, and building of ephemeral glaciers on Antarctica. The impact events and increase in volcanism, while synchronous with the transitional zone between the Peanut Peak and Big Cottonwood Creek lithologies, cannot explain the long term climatic perturbation, which persists within the White River Group. Instead, the climatic deterioration is likely explained by the building of ephemeral Antarctic ice sheets, which was compounded by the increase in volcanism and impacts. Regional variations in ä18O isotopes within the White River Group can likely explain the suggested variations in paleoclimate across the Eocene-Oligocene transition.
Temple University--Theses
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Shackelton, Allison Lee. "REGIONAL AND STRATIGRAPHIC VARIABILITY OF MICROWEAR ON THE MOLARS OF LEPTOMERYX FROM EOCENE-OLIGOCENE STRATA OF WYOMING AND NEBRASKA." Master's thesis, Temple University Libraries, 2016. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/402261.

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Geology
M.S.
Climate change across the terrestrial Eocene-Oligocene boundary of the Great Plains is recorded by shifts in sediments, facies, paleosols, and isotopic records, and is interpreted as a shift to overall cooler and drier conditions. As an independent test of paleoenvironmental shifts caused by climatic change, I compared microwear on M2 molars of Leptomeryx from the White River Group (WR) at Toadstool Park, Nebraska (n = 9) and Flagstaff Rim, Wyoming (n = 11). Comparisons of microwear were made through time at each section. Various measurements of microwear were quantified on original, uncoated specimens using environmental scanning electron microscopy and Microware 4.0 software, and evaluated with ANOVA and Kruskal-Wallis statistical tests. Values of the scratch:pit ratio, scratch number, feature major:minor axis ratio, feature vector length, major axis standard deviation, major:minor axis standard deviation, and feature orientation standard deviation for Leptomeryx M2 molars are significantly different (p<0.05) between Wyoming and Nebraska. Microwear patterns suggest paleoecological differences between the two locations, possibly related to differences in Leptomeryx diet or in amount or character of sediment adhering to ingested vegetation. Little fossil evidence of vegetation type is preserved at either locality, other than clay-filled root traces or occasional rhizoliths or silicified fragments. However, sediments of the WR are a mixture of volcaniclastic enriched mudstone, siltstone, and sandstone, with generally coarser overall particle sizes in Wyoming that reflect proximity to siliciclastic sources. The degree of overall volcaniclastic enrichment and number of airfall tuffs is also higher at Flagstaff Rim. Paleosols suggest a shift from closed canopy forest to progressively open conditions at each locality and, although microwear differences could result from differences in vegetation or particle sizes of adhered sediments on plants, no or very low correlations between microwear features and stratigraphic level were detected at either locality, indicating that any changes in paleoecology over time did not significantly alter the diets of Leptomeryx, although diet may have been geographically different.
Temple University--Theses
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Lukens, William E. "PALEOPEDOLOGY AND PALEOGEOMORPHOLOGY OF THE EARLY OLIGOCENE ORELLA AND WHITNEY MEMBERS, BRULE FORMATION, WHITE RIVER GROUP, TOADSTOOL GEOLOGIC PARK, NEBRASKA." Master's thesis, Temple University Libraries, 2013. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/231796.

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Geology
M.S.
Understanding local and regional reactions to the global Eocene-Oligocene climate transition is a continuing challenge. The White River Group in the North American midcontinent preserves dynamic fluvial, volcaniclastic and lacustrine facies that yield to aeolianites. To test whether this shift in sedimentation style was driven by climate change, 20 paleosols from 8 profiles were analyzed from the fluvial-aeolian Orella Member through the aeolian-dominated Whitney Member of the earliest Oligocene Brule Formation at Toadstool Geologic Park, NE. Paleosol morphology and geochemistry were used to assess the balance of aeolian vs. alluvial sedimentation at key stratigraphic intervals and lithologic transitions. Significant loess deposition began at least as early as the lower Orella Member but is masked in most settings by concomitant fluvial deposition. As fluvial influence on landscapes waned across the Orella-Whitney Member boundary, loess deposits predominated and became more recognizable. Paleosols follow different pedogenic pathways in direct response to depositional setting. Whereas all paleosols formed through top-down pedogenesis in alluvial settings, paleosols in aeolian-dominated settings formed though pedogenic upbuilding during aggradational phases and through top-down pedogenesis during depositional hiatuses. The disparity between each style of pedogenic development creates fundamentally different pedogenic associations that must first be understood before climatic interpretations can be drawn from macroscopic paleosol morphology alone. Microscopic analysis of loessic and alluvial paleosols indicates that pedogenic features do not greatly change across the Orella-Whitney Member boundary. Furthermore, results of climofunction calculations from five paleosol Bw and Btk horizons show mean annual temperature (ca. 9.0-10.5 °C) and precipitation (ca. 650-800 mm/y) do not significantly vary across the Orella-Whitney Member transition. Clay mineralogy and the presence of pedogenic carbonate and translocated clay corroborate paleoclimate estimates. However, geochemical paleosol profiles are uniform and do not reflect observed vertical associations of pedogenic features. Constant additions of aeolian sediment, which replenishes base losses through leaching, explain this phenomenon. Interpretations of paleovegetation from root trace morphology and paleosol taxonomy indicate that predominantly open canopy to savanna habitats were in place in the lower Orella Member and continued into the Whitney Member. Evidence for riparian partitioning exists in the lower Orella Member but disappears as fluvial deposits wane in the Whitney Member. Lacking evidence of climate change from paleosol analysis, changes in sedimentation style and vegetative biomes are most likely a reaction to increased aeolian deposition.
Temple University--Theses
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Snidow, Dean C. "Assessing the impact of urbanization on White River water and sediment geochemistry in an agricultural watershed." CardinalScholar 1.0, 2009. http://liblink.bsu.edu/uhtbin/catkey/1477281.

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Increased urbanization in the United States and the rest of the world, has led to more research on the effects it has on the local ecology. Urbanization can be defined as the creation of impervious cover in areas previously covered by natural vegetation (forest, grassland or farmland) as well as the potential influence of sewage treatment plants. Small increases in impervious cover can cause noticeable changes in stream chemistry. The goal of this study is to quantify the impact of smaller industrial cities on water and sediment geochemistry in a largely agricultural watershed. The study area is in east-central Indiana along the west fork of the White River and includes the cities of Winchester, Muncie and Anderson. This area is dominated by agriculture and the impact of cities in the region on water chemistry has not been studied. To evaluate this impact, sampling sites were selected up- and downstream of the three cities to characterize White River water chemistry before and after it flows through the cities as well as sewage treatment plants. Sampling was done over the course of one year to obtain samples characteristic of high and low flow river conditions. Samples were analyzed for major cation and anion concentrations as well as total suspended solids. Metals data was also obtained in sediments, although sampled only twice throughout the study. Results show that sediment load, on average, increases on the downstream side as the river flows through urbanized areas. Chemical analyses show that major cations and anions, Na, K, SO4 and Cl, have distinct spikes in concentration on the downstream side of the cities, as well. Na and Cl are specifically linked to human and urbanized activity, and were up to four times higher downstream of urbanized cities. The concentration of other major ions, including Ca, Mg and NO3, was mostly due to agricultural land use and local bedrock geology. Trace metals characteristic of pollution from automobiles, including Cd, Cr and Zn, showed large increases downstream of urban areas as well. This indicates that even in an area that is largely dominated by agriculture, smaller cities have a quantifiable impact to White River water quality.
Department of Geology
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Zoll, Mitchell K. "Prehistoric settlement in the upper Wabash River Valley." Virtual Press, 1993. http://liblink.bsu.edu/uhtbin/catkey/864934.

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1989, the Archaeological Resources Management Service Ball State University conducted a reconnaissance level survey of 550 acres located within and adjacent to the Wabash River Valley in Huntington and Wabash Counties, Indiana. Additional survey was conducted in 1990 and 1991 on areas of expanded right-of-way within the original project area. The field reconnaissance located 188 archaeological sites. Twenty-one of the sites located by those surveys were subjected to archaeological testing.This study examines data from the survey and testing and presents a distribution of sites and human settlement across the study area. The study also develops a site typology which is used to address settlement pattern questions for the study area.
Department of Anthropology
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Books on the topic "White River (Ind. : River)"

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Lawson, Daniel E. Physical processes and natural attenuation alternatives for remediation of white phosphorus contamination, Eagle River Flats, Fort Richardson, Alaska. [Hanover, N.H.]: US Army Corps of Engineers, Cold Regions Research & Engineering Laboratory, 1996.

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White River dreams. Uhrichsville, OH: Heartsong Presents, 2011.

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Devine, Frances. White River sunrise. Uhrichsville, Ohio: Heartsong Presents, 2012.

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Lassiter, Karl. White River massacre. New York: Pinnacle Books, 2002.

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Copyright Paperback Collection (Library of Congress), ed. White River song. Uhrichsville, Ohio: Heartsong Presents, 2011.

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White River Junction: Poems. Amherst, Mass: Amherst Writers & Artists, 1987.

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B, Patten Lewis. Massacre at White River. Bath, England: Chivers Large Print, 1994.

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United States. Forest Service. Rocky Mountain Region. White River National Forest. Glenwood Springs, CO]: United States Dept. of Agriculture, Forest Service, Rocky Mountain Region, 2002.

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KSMU (Radio station : Springfield, Mo.), ed. White River journal: RadioBook. [Springfield, Mo.?]: KSMU, 1997.

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Rathnow, Ron. Youghiogheny River. Birmingham, Ala: Menasha Ridge Press, 1987.

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Book chapters on the topic "White River (Ind. : River)"

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Sychitkokhong Uy, Phitsamay. "From the Mekong River to the Merrimack River." In Experiences of Racialization in Predominantly White Institutions, 109–19. Abingdon, Oxon ; New York, NY : Routledge, 2021.: Routledge, 2020. http://dx.doi.org/10.4324/9780429355639-10.

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Zhao, Yiheng. "Subculture as Moral Paradox: A Study of the Texts of the White Rabbit Play." In The River Fans Out, 53–80. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-7724-6_6.

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Gordeev, Viacheslav V., Oleg S. Pokrovsky, and Vladimir P. Shevchenko. "The Geochemical Features of the River Discharge to the White Sea." In The Handbook of Environmental Chemistry, 47–81. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/698_2018_329.

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Sandberg, Sveinung, and Willy Pedersen. "Trajectories to The River." In Street capitalBlack cannabis dealers in a white welfare state, 15–31. Policy Press, 2011. http://dx.doi.org/10.1332/policypress/9781847421203.003.0002.

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"On the Banks of the White River." In Life in the Leatherwoods, 19–30. University of Arkansas Press, 2000. http://dx.doi.org/10.2307/j.ctv10crd9f.7.

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Wallus, Robert, and Thomas P. Simon. "White Bass." In Reproductive Biology and Early Life History of Fishes in the Ohio River Drainage, 222–41. CRC Press, 2006. http://dx.doi.org/10.1201/9781420003604-51.

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"Historical Changes in Large River Fish Assemblages of the Americas." In Historical Changes in Large River Fish Assemblages of the Americas, edited by Terry R. Maret and Christopher A. Mebane. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569728.ch4.

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<em>Abstract.</em>—The Snake River is the tenth longest river in the United States, extending 1,667 km from its origin in Yellowstone National Park in western Wyoming to its union with the Columbia River at Pasco, Washington. Historically, the main-stem Snake River upstream from the Hells Canyon Complex supported at least 26 native fish species, including anadromous stocks of Chinook salmon <em>Oncorhynchus tshawytscha</em>, steelhead <em>O. mykiss</em>, Pacific lamprey <em>Lampetra tridentata</em>, and white sturgeon <em>Acipenser transmontanus</em>. Of these anadromous species, only the white sturgeon remains in the Snake River between the Hells Canyon Complex and Shoshone Falls. Today, much of the Snake River has been transformed into a river with numerous impoundments and flow diversions, increased pollutant loads, and elevated water temperatures. Current (1993–2002) fish assemblage collections from 15 sites along the Snake River and Henrys Fork contained 35 fish species, including 16 alien species. Many of these alien species such as catfish (Ictaluridae), carp (Cyprinidae), and sunfish (Centrarchidae) are adapted for warmwater impounded habitats. Currently, the Snake River supports 19 native species. An index of biotic integrity (IBI), developed to evaluate large rivers in the Northwest, was used to evaluate recent (1993– 2002) fish collections from the Snake River and Henrys Fork in southern Idaho and western Wyoming. Index of biotic integrity site scores and component metrics revealed a decline in biotic integrity from upstream to downstream in both the Snake River and Henrys Fork. Two distinct groups of sites were evident that correspond to a range of IBI scores—an upper Snake River and Henrys Fork group with relatively high biotic integrity (mean IBI scores of 46–84) and a lower Snake River group with low biotic integrity (mean IBI scores of 10–29). Sites located in the lower Snake River exhibited fish assemblages that reflect poor-quality habitat where coldwater and sensitive species are rare or absent, and where tolerant, less desirable species predominate. Increases in percentages of agricultural land, total number of diversions, and number of constructed channels were strongly associated with these decreasing IBI scores.
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"Historical Changes in Large River Fish Assemblages of the Americas." In Historical Changes in Large River Fish Assemblages of the Americas, edited by Terry R. Maret and Christopher A. Mebane. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569728.ch4.

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<em>Abstract.</em>—The Snake River is the tenth longest river in the United States, extending 1,667 km from its origin in Yellowstone National Park in western Wyoming to its union with the Columbia River at Pasco, Washington. Historically, the main-stem Snake River upstream from the Hells Canyon Complex supported at least 26 native fish species, including anadromous stocks of Chinook salmon <em>Oncorhynchus tshawytscha</em>, steelhead <em>O. mykiss</em>, Pacific lamprey <em>Lampetra tridentata</em>, and white sturgeon <em>Acipenser transmontanus</em>. Of these anadromous species, only the white sturgeon remains in the Snake River between the Hells Canyon Complex and Shoshone Falls. Today, much of the Snake River has been transformed into a river with numerous impoundments and flow diversions, increased pollutant loads, and elevated water temperatures. Current (1993–2002) fish assemblage collections from 15 sites along the Snake River and Henrys Fork contained 35 fish species, including 16 alien species. Many of these alien species such as catfish (Ictaluridae), carp (Cyprinidae), and sunfish (Centrarchidae) are adapted for warmwater impounded habitats. Currently, the Snake River supports 19 native species. An index of biotic integrity (IBI), developed to evaluate large rivers in the Northwest, was used to evaluate recent (1993– 2002) fish collections from the Snake River and Henrys Fork in southern Idaho and western Wyoming. Index of biotic integrity site scores and component metrics revealed a decline in biotic integrity from upstream to downstream in both the Snake River and Henrys Fork. Two distinct groups of sites were evident that correspond to a range of IBI scores—an upper Snake River and Henrys Fork group with relatively high biotic integrity (mean IBI scores of 46–84) and a lower Snake River group with low biotic integrity (mean IBI scores of 10–29). Sites located in the lower Snake River exhibited fish assemblages that reflect poor-quality habitat where coldwater and sensitive species are rare or absent, and where tolerant, less desirable species predominate. Increases in percentages of agricultural land, total number of diversions, and number of constructed channels were strongly associated with these decreasing IBI scores.
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Prothero, Donald R. "Magnetic stratigraphy of the White River Group in the High Plains." In The Terrestrial Eocene-Oligocene Transition in North America, 262–77. Cambridge University Press, 1996. http://dx.doi.org/10.1017/cbo9780511665431.014.

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"Historical Changes in Large River Fish Assemblages of the Americas." In Historical Changes in Large River Fish Assemblages of the Americas, edited by Thomas P. Simon, Ronda L. Dufour, and Brant E. Fisher. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569728.ch20.

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<em>Abstract.</em>—The Patoka River drainage is a lowland-gradient watershed of the Wabash River lowlands in southwestern Indiana. During the late 18th century, the river was part of an extensive riparian floodplain wetland that connected the White River with the lower Wabash River. Through anthropogenic changes as a result of ditching, channelization, levee creation, coal extraction, and oil and gas exploration, the Patoka River drainage has been highly altered. These changes have resulted in a loss of sitespecific biological diversity and integrity, causing drainage-wide biological diversity decline. Extirpations in the watershed have resulted in the local loss of 12.7% of the fish fauna during the last century. The local extirpations of six species included central mudminnow <em>Umbra limi</em>, black redhorse <em>Moxostoma duquesnei</em>, brindled madtom <em>Noturus miurus</em>, bluebreast darter <em>Etheostoma camurum</em>, slenderhead darter <em>Percina phoxocephala</em>, and saddleback darter <em>P. vigil</em>. Black redhorse, bluebreast darter, slenderhead darter, and saddleback darter were only known from pre-1900, while brindled madtom and central mudminnow were known until the early 1940s. These species may have been rare to begin with in the Patoka River drainage, but since they are widespread elsewhere, it seems more probable that they disappeared as a result of the land-use changes. Sensitive species of darters and minnows have declined in abundance, but recent sampling has shown that they remain in the watershed at low abundance. Based on a probability sample, less than 12% of the channels represented reference least-disturbed conditions, while 61% exhibited degraded conditions.
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Conference papers on the topic "White River (Ind. : River)"

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Baldauf, Paul, Patrick Burkhart, and Paul R. Hanson. "QUATERNARY AEOLIAN CHRONOLOGY, WHITE RIVER BADLANDS, SOUTH DAKOTA, NORTHERN GREAT PLAINS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286691.

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Byers, Colton W., Henry D. Kramer, Patrick A. Burkhart, Paul Baldauf, Gregory S. Baker, Brett McClinton, Cody Brown, Ellis Peet, Ashley Forrest, and Dylan Ramey. "SAND PROVENANCE ACROSS THE WHITE RIVER BADLANDS TOWARD THE NEBRASKA SAND HILLS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338117.

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Baldauf, Paul, Gregory S. Baker, Patrick Burkhart, Paul Hanson, Maraina Miles, and Henry D. Kramer. "GEOMORPHOLOGIC AND COMPOSITIONAL CONTROLS ON LATE HOLOCENE AEOLIAN REACTIVATION, WHITE RIVER BADLANDS, SOUTH DAKOTA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319029.

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Baldauf, Paul, Patrick Burkhart, P. R. Hanson, Maraina Miles, Ashley K. Larsen, and Lucca Libonatti. "EPISODIC REACTIVATION OF QUATERNARY AEOLIAN DEPOSITS, WHITE RIVER BADLANDS, SOUTH DAKOTA, NORTHERN GREAT PLAINS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301813.

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Gallucci, John E., Dennis O. Terry, and Paul Victor Ullmann. "CONTROLS ON SOFT TISSUE PRESERVATION IN EOCENE-OLIGOCENE VERTEBRATE FOSSILS OF THE WHITE RIVER GROUP." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335712.

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Czuba, Jonathan A., Scott R. David, Douglas A. Edmonds, and Graham H. Johnston. "MORPHODYNAMIC INSIGHTS INTO A CHANNELIZED FLOODPLAIN ALONG THE MEANDERING EAST FORK WHITE RIVER, INDIANA, USA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303729.

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Persico, Geno Salvatore, David C. Viertel, and Diane M. Burns. "EIGHT DECADES OF GEOMORPHOLOGICAL CHANGE TO THE LITTLE WABASH RIVER IN WHITE COUNTY, SOUTH-CENTRAL ILLIONIS, USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316728.

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Zimovets, Alina, Alina Zimovets, Yury Fedorov, Yury Fedorov, Asya Ovsepyan, Asya Ovsepyan, Vyacheslav Savitskiy, and Vyacheslav Savitskiy. "THE REGULARITY OF HEAVY METALS DISTRIBUTION AND BEHAVIOR IN THE BOTTOM SEDIMENTS ON THE PROFILE “NORTHERN DVINA RIVER – WHITE SEA”." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b431771359a.

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A study was conducted to investigate the level of heavy metals in bottom sediments of the Northern Dvina mouth area and the White Sea in various seasons since 2004. Of greatest interest for the study was presented as such heavy metals as Hg, Pb, Cd, Cu, Ni, Zn, Cr, which belong to the priority group of toxic elements. The heavy metals concentrations were determined with atomic absorption spectrometer. Also the grain-size composition, concentrations of organic carbon and values of hydrogen ion exponent (pH) and redox potential (Eh) in bottom sediments were determined. It was found that the levels of heavy metals in sediments significantly changed in the lateral radial direction. There is a tendency to increased concentrations of some heavy metals downstream of the river. The high concentrations of heavy metals were found within the influence of cities and towns. So the extremely high mercury concentrations were found in the sediments of small and shallow channels crossing the Arkhangelsk city. The study of heavy metal concentrations in the bottom sediments along the profile “the Northern Dvina - Dvina Bay - White sea” showed that the marginal filter contributes to the coprecipitation with suspended metals of anthropogenic genesis. These processes greatly reduce the contamination risk of the White Sea. Thus, the impact of the river on the ecosystem of the White Sea outside the marginal filter is significantly less.
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Zimovets, Alina, Alina Zimovets, Yury Fedorov, Yury Fedorov, Asya Ovsepyan, Asya Ovsepyan, Vyacheslav Savitskiy, and Vyacheslav Savitskiy. "THE REGULARITY OF HEAVY METALS DISTRIBUTION AND BEHAVIOR IN THE BOTTOM SEDIMENTS ON THE PROFILE “NORTHERN DVINA RIVER – WHITE SEA”." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93c8b57a02.64869435.

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A study was conducted to investigate the level of heavy metals in bottom sediments of the Northern Dvina mouth area and the White Sea in various seasons since 2004. Of greatest interest for the study was presented as such heavy metals as Hg, Pb, Cd, Cu, Ni, Zn, Cr, which belong to the priority group of toxic elements. The heavy metals concentrations were determined with atomic absorption spectrometer. Also the grain-size composition, concentrations of organic carbon and values of hydrogen ion exponent (pH) and redox potential (Eh) in bottom sediments were determined. It was found that the levels of heavy metals in sediments significantly changed in the lateral radial direction. There is a tendency to increased concentrations of some heavy metals downstream of the river. The high concentrations of heavy metals were found within the influence of cities and towns. So the extremely high mercury concentrations were found in the sediments of small and shallow channels crossing the Arkhangelsk city. The study of heavy metal concentrations in the bottom sediments along the profile “the Northern Dvina - Dvina Bay - White sea” showed that the marginal filter contributes to the coprecipitation with suspended metals of anthropogenic genesis. These processes greatly reduce the contamination risk of the White Sea. Thus, the impact of the river on the ecosystem of the White Sea outside the marginal filter is significantly less.
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Gillham, Robert B., and Ross Secord. "CHANGES IN MAMMALIAN ABUNDANCE THROUGH THE EOCENE-OLIGOCENE CLIMATE TRANSITION IN THE WHITE RIVER GROUP OF NEBRASKA, USA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338705.

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Reports on the topic "White River (Ind. : River)"

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Dauble, D. D., K. R. Price, and T. M. Poston. Radionuclide concentrations in white sturgeon from the Columbia River. Office of Scientific and Technical Information (OSTI), September 1992. http://dx.doi.org/10.2172/7277267.

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Dauble, D. D., K. R. Price, and T. M. Poston. Radionuclide concentrations in white sturgeon from the Columbia River. Office of Scientific and Technical Information (OSTI), September 1992. http://dx.doi.org/10.2172/10175140.

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Dauble, D. D., K. R. Price, and T. M. Poston. Radionuclide concentrations in white sturgeon from the Columbia River. Revision 1. Office of Scientific and Technical Information (OSTI), November 1993. http://dx.doi.org/10.2172/10107902.

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Glass, Ronald J., Gerald Walton, Herbert E. Echelberger, and Herbert E. Echelberger. Estimates of recreational stream use in the White River drainage, Vermont. St. Paul, MN: U.S. Department of Agriculture, Forest Service, North Central Research Station, 1992. http://dx.doi.org/10.2737/ne-rp-658.

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Thiesfeld, Steven L., Ronald H. McPeak, Brian S. McNamara, and Isadore Honanie. Bull Trout Population Assessment in the White Salmon and Klickitat Rivers, Columbia River Gorge, Washington, 2001 Annual Report. Office of Scientific and Technical Information (OSTI), January 2002. http://dx.doi.org/10.2172/797031.

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Platfoot, J. H., M. W. Wendel, and P. T. Williams. Multidimensional Computational Fluid Dynamics Modeling of the Dispersion of White Oak Creek Contaminants in the Clinch River. Office of Scientific and Technical Information (OSTI), October 1996. http://dx.doi.org/10.2172/460796.

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Nigro, Anthony A. Status and Habitat Requirements of White Sturgeon Populations in the Columbia River Downstream from McNary Dam, 1989-1990 Annual Report. Office of Scientific and Technical Information (OSTI), September 1990. http://dx.doi.org/10.2172/6301384.

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Nigro, Anthony A. Status and Habitat Requirements of White Sturgeon Populations in the Columbia River Downstream from McNary Dam, 1988-1989 Annual Report. Office of Scientific and Technical Information (OSTI), September 1989. http://dx.doi.org/10.2172/5206937.

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McCabe, Jr ,. George T., Lance G. Beckman, and Gayle Kreitman. Status and Habitat Requirements of White Sturgeon Populations in the Columbia River Downstream from McNary Dam, 1986-1987 Annual Report. Office of Scientific and Technical Information (OSTI), June 1987. http://dx.doi.org/10.2172/774387.

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Nigro, Anthony A. Status and Habitat Requirements of White Sturgeon Populations in the Columbia River Downstream from McNary Dam, 1987-1988 Annual Report. Office of Scientific and Technical Information (OSTI), September 1988. http://dx.doi.org/10.2172/774388.

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