<?xml version="1.0" encoding="UTF-8"?>
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<title>JKUAT COHRED CONFERENCE Series</title>
<link href="http://localhost/xmlui/handle/123456789/2199" rel="alternate"/>
<subtitle/>
<id>http://localhost/xmlui/handle/123456789/2199</id>
<updated>2026-04-07T00:37:52Z</updated>
<dc:date>2026-04-07T00:37:52Z</dc:date>
<entry>
<title>A Model for Stability Analysis of a Multi-Layered River Bank (SAMLR)</title>
<link href="http://localhost/xmlui/handle/123456789/4147" rel="alternate"/>
<author>
<name>Amiri-Tokaldany, E.</name>
</author>
<author>
<name>Darby, S. E.</name>
</author>
<id>http://localhost/xmlui/handle/123456789/4147</id>
<updated>2018-02-15T09:43:18Z</updated>
<published>2018-02-15T00:00:00Z</published>
<summary type="text">A Model for Stability Analysis of a Multi-Layered River Bank (SAMLR)
Amiri-Tokaldany, E.; Darby, S. E.
River bank erosion can result in considerable riparian land loss and the delivery of&#13;
large volumes of sediment to reaches downstream. Consequently, the ability to predict the&#13;
stability and failure geometry of eroding river banks is an important prerequisite for estimating&#13;
the rate of bank erosion and sediment yield associated with bank erosion. In this&#13;
paper a new model capable of analyzing the stability of layered river banks is introduced.&#13;
The new model takes into consideration the effects of positive pore water pressure in the&#13;
saturated portion, and negative pore water pressure in the unsaturated portion, of the&#13;
bank. Also, the role of hydrostatic confining pressure due to the water level in the river&#13;
and the effects of the water in tension crack on stability analysis is accounted for. Unlike&#13;
many previous analyses, the failure plane is not constrained to pass through the toe of the&#13;
bank. However, it considers only planar-type failure mechanism. Finally the bank profile&#13;
geometry is not restricted to a special case. The new model has been tested using field data&#13;
sets from a site on the Sieve River in Italy and a site on Goodwin Creek in Mississippi.&#13;
The results show some agreement between the predicted and observed values of bank stability.
paper
</summary>
<dc:date>2018-02-15T00:00:00Z</dc:date>
</entry>
<entry>
<title>Fish Parasites in Zarivar Lake</title>
<link href="http://localhost/xmlui/handle/123456789/4145" rel="alternate"/>
<author>
<name>Jalali1, B.</name>
</author>
<author>
<name>Barzegar, M.</name>
</author>
<id>http://localhost/xmlui/handle/123456789/4145</id>
<updated>2018-02-15T09:36:33Z</updated>
<published>2018-02-15T00:00:00Z</published>
<summary type="text">Fish Parasites in Zarivar Lake
Jalali1, B.; Barzegar, M.
Twenty four ecto- and endo- parasite species were found in different organs of eight native&#13;
and exotic fish species in Zarivar Lake situated in the far west of Iran. Overall, 1000&#13;
fish specimens belonging to the Dactylogyridae, Gyrodactylidae families the Cyprinidae,&#13;
Poeciliidae and Mastacembelidae families were examined during 2001 and 2002. Of them,&#13;
five Protozoans, including Trichodina pediculus, Trichodina sp and Myxobolus molnari, a&#13;
pansporogenic stage of the Myxosporean plasmodia and Ichthyophthirius multifiliis were&#13;
recorded. Of the Metazoan parasites, 12 monogenean species, mostly belonging to the&#13;
Dactylogyridae, Gyrodactylidae families and the Ancyrocephalinae subfamily, were found&#13;
and identified at species and genus level. The number of helminthes reached 15 by adding&#13;
one Digenea metacercaria (Diplostomum spathaceum) and 2 coelozoic Cestoda species.&#13;
Crustacean species found on both of native and exotic fishes, belonging to Copepoda and&#13;
Branchiora orders comprised of Argulus foliaceus and Lernaea cyprinacea, in addition an&#13;
unknown Argulus was also found on skin and gills of spiny eel which identified to genus&#13;
level. The only nematode found in the intestine of common carp was identified as Pseudocapillaria&#13;
tomentosa. Besides the first record of parasites of spiny eel, the seasonal prevalence&#13;
of ligulosis is presented. Additionally, zoogeographical analysis and species composition&#13;
of parasitic fauna of Zarivar Lake are discussed.
paper
</summary>
<dc:date>2018-02-15T00:00:00Z</dc:date>
</entry>
<entry>
<title>Prediction of Irrigation Water Salinity by Means of Hydrometry</title>
<link href="http://localhost/xmlui/handle/123456789/4120" rel="alternate"/>
<author>
<name>Khorsandi, F.</name>
</author>
<author>
<name>Yazdi, F. Alaei</name>
</author>
<id>http://localhost/xmlui/handle/123456789/4120</id>
<updated>2018-02-14T13:38:44Z</updated>
<published>2018-02-14T00:00:00Z</published>
<summary type="text">Prediction of Irrigation Water Salinity by Means of Hydrometry
Khorsandi, F.; Yazdi, F. Alaei
Salinity is the primary water quality concern in irrigated agriculture. An Electrical&#13;
Conductivity (EC) meter and a hydrometer are two possible methods for measurement of&#13;
irrigation water salinity. The conductivity meter method is based on measuring the&#13;
amount of electrical current that a fluid will support. Although it is the most widely used&#13;
method, the instrumentation is rather expensive and in some instances may require&#13;
sample dilution. The hydrometer method is based on measuring the density of the fluid.&#13;
The main objectives of this study were to compare these two methods and, based on&#13;
hydrometer method, develop empirical models for prediction of EC, sodium adsorption&#13;
ratio (SAR), and the principle ion concentrations in the irrigation waters of Yazd&#13;
Province, Iran. The electrical conductivity, temperature, and density of 206 water samples&#13;
from wells across Yazd Province were measured. Temperature correction factors for&#13;
adjusting the hydrometer reading to 25 oC were determined. The correlation between EC&#13;
and hydrometer readings was high (R2 = 0.97). Although the empirical model developed&#13;
for prediction of EC slightly underpredicted the measured values, it is still accurate&#13;
enough for practical purposes. Hydrometer readings were also highly correlated with the&#13;
principle ions and SAR. The salt type also affected the hydrometer readings. Magnesium&#13;
sulfate solution had the highest density among the major salt types present in irrigation&#13;
waters. Finally, a chart was developed for rough estimations of EC, sodium and chlorine&#13;
concentrations in irrigation waters of Yazd Province, Iran.
paper
</summary>
<dc:date>2018-02-14T00:00:00Z</dc:date>
</entry>
<entry>
<title>The Agha Jari Formation: A Potential Source of Ammonium and Nitrate Nitrogen Fertilizers</title>
<link href="http://localhost/xmlui/handle/123456789/4116" rel="alternate"/>
<author>
<name>Yazdian, A. R.</name>
</author>
<author>
<name>Kowsar, S. A.</name>
</author>
<id>http://localhost/xmlui/handle/123456789/4116</id>
<updated>2018-02-14T12:48:19Z</updated>
<published>2018-02-14T00:00:00Z</published>
<summary type="text">The Agha Jari Formation: A Potential Source of Ammonium and Nitrate Nitrogen Fertilizers
Yazdian, A. R.; Kowsar, S. A.
Nitrogen deficiency ranks right behind water shortage as the second-most constraint to&#13;
crop production in the coarse-loamy sand of the Gareh Bygone Plain (GBP) in southern&#13;
Iran. Since better resource utilization is essential for wise energy management, contrary&#13;
to reported cases, surface water pollution by N maybe a boon in the GBP. The Agha Jari&#13;
Formation (AJF), in which the Bisheh Zard Basin (BZB) has been formed, contains anomalously&#13;
high concentrations of NO3&#13;
− and NH4&#13;
+ in its calcareous sandstone, siltstone&#13;
and marl components. As about 60% of our irrigation water is supplied through underground&#13;
resources and are heavily over-exploited, the artificial recharge of groundwater&#13;
(ARG) is actively pursued in Iran. Therefore, a major proportion of the ephemeral discharge&#13;
of the BZB is spread over 1365 hectares of sedimentation basins and recharge&#13;
ponds of the ARG system in the GBP. These basins and ponds are covered with improved&#13;
rangeland, and eucalyptus (Eucalyptus spp.) and acacia (Acacia spp.) plantations. Therefore,&#13;
it is expected that some of the geological-N dissolved in floodwater, and also carried&#13;
by the suspended load, will reach the groundwater and supply the plants coming in contact&#13;
with the water and/or sediment. Moreover, as both NO3&#13;
− and NH4&#13;
+ are considered&#13;
pollutants of groundwater, the relative abundance of each should be determined, so that&#13;
possible remedial measures can be designed and implemented. To study the origin of N&#13;
in the BZB, and to investigate the fate of the dissolved and adsorbed N as it travels from&#13;
the watershed to the root zone, 13 rock samples, 5 floodwater samples and 81 soil samples&#13;
were collected and analyzed for NO3&#13;
−and NH4&#13;
+. The NO3&#13;
−-N concentration was lower than&#13;
that of NH4&#13;
+-N in most of the samples: 5.1 vs. 9.6 mg kg-1 in rocks, 13.4 vs.17.4 mg L-1 dissolved&#13;
in floodwater, 1.3 vs.4.3 mg kg-1 carried by the suspended load, and 10.6 vs.15.5 mg&#13;
kg-1 in the 0-125 cm soil profile. Assuming that the mean annual inflow of the GBP-ARG&#13;
system is 7 million m3 ,we receive 89.4±52.4 kg ha-1 yr-1 of NH4&#13;
+-N and 68.7± 24.6 kg ha-&#13;
1 yr-1 of NO3&#13;
−-N, of which some furnishes the vegetative cover with N. A part of what&#13;
remains may reach the watertable after passing through the vadose zone.
</summary>
<dc:date>2018-02-14T00:00:00Z</dc:date>
</entry>
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