Soil Nutritional Status of Apricot (Prunus Armeniaca L.) Orchards in Malatya Province

Colak, S.; Çelik, Belgin; Gokalp, K.; Yılmaz, Kadir; Zengin, Yaşar; Kargı, Sevgi Paydaş

doi:10.17660/actahortic.2010.862.54

Cited by 6 publications

(4 citation statements)

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“…These results are in conformity with Norboo (1994), Sanjay et al, (2005) and Colak et al, (2010). Organic carbon present in the soil samples varied from 0.15 to 0.20% with a mean value of 0.18% significantly at 95% Confidence interval in surface layer while-as in sub-surface layers it varied from 0.11 to 0.16% with a mean value of 0.13% at 95% C.I.…”

Section: Resultssupporting

confidence: 91%

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Nutrient Status of Aprioct (Prunus armeniaca L.) Orchards of District Kargil, Ladakh

Ali¹,

Malik²,

Dolkar³

et al. 2018

Int.J.Curr.Microbiol.App.Sci

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Section: Resultssupporting

confidence: 91%

“…(Table 3). Similar reports were reported in their findings by Norboo (1994), Sanjay et al, (2005) and Colak et al, (2010). Calcium carbonate content varied from 0.28 to 0.56% with a mean value of 0.45% while-as in the sub-surface layers it varied from 0.16 to 0.75% with a mean value of 0.51% statistically at 95% C.I.…”

Section: Resultssupporting

confidence: 88%

Nutrient Status of Aprioct (Prunus armeniaca L.) Orchards of District Kargil, Ladakh

Ali¹,

Malik²,

Dolkar³

et al. 2018

Int.J.Curr.Microbiol.App.Sci

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“…Accordingly, significant positive correlations were found between soil K content and leaf Mn content, soil Ca content and leaf Ca, Mn and Zn contents, and soil Mg content and leaf N, P and K contents (Table 4). Colak et al (2010) examined physical and chemical properties of 1297 soil samples taken from apricot orchards in Malatya and its counties. Most of the soil samples were found clay loam or loamy, and 17 % of the orchards were slightly alkaline, 23.9 % were medium alkaline and 51.4 % were strongly alkaline.…”

Section: Resultsmentioning

confidence: 99%

Determination of Nutrition Status of Apple Orchards in Doğanşehir, Malatya

Karlıdağ

Karaat

Kan

et al. 2019

Alınteri Zirai Bilimler Dergisi

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In order to determine nutrition status of the apple orchards in Doğanşehir region of Malatya Province, chemical and physical properties of soil samples, and macro and micro nutrient contents of soil and leaf samples taken from the selected orchards from different parts of the region were determined in 2017. Soil samples were collected from two depths of 0-30 cm and 30-60 cm, 1 kg from each depth, in September. Leaf samples, 100 leaves taken from head level of trees representing the related orchard, were collected 11 weeks after full blossom. Results indicated that soil texture, pH and salinity level was appropriate for apple growing, but loam content was generally high and organic matter was poor. Except Mn and Zn, macro and micro nutrients were found adequate in soil samples of most of the orchards. Sampling depth did not affected soil properties in most of the orchards. Almost all of the leaf samples were found adequate in N, P, Fe, and Cu contents, whereas they were found inadequate in terms of K, Ca, and Zn contents. N content varied between 0.068% and 0.106% in soil samples, and between 1.78% and 2.68% in leaf samples.

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“…According to Marcolongo and Palmieri (1983), Arslantepe is situated favorably within the landscape because of a large hydrogeological catchment, supplying the site reliably with running water. Today, large parts of the area of the Malatya Plain are covered by sediments providing fertile soils for extensive apricot plantations (Colak et al, 2010). So far, the genesis and age of the young sediments exposed at the surface (Pleistocene or Holocene) have rarely been studied (e.g.…”

Section: Regional Settingmentioning

confidence: 99%

Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment

et al. 2014

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Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could reflect geomorphic responses to societal collapse (Late Chalcolithic state, Neo-Hittite kingdom) at Arslantepe. Most intensive Holocene soil erosion and landscape degradation occurred after occupation of the region by the Roman Empire. This is paralleled by the onset of river activity. A part of the lower neo-Hittite town as well as an early Holocene Terra Rossa–like soil that had formed rapidly were found buried. So far, no indication for mid–late Holocene fluvial activity of the adjacent creeks until Roman times has been found. Our results illustrate the large potential of slope deposits for long term reconstructions of human induced landscape transformation in Anatolia.

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Soil Nutritional Status of Apricot (Prunus Armeniaca L.) Orchards in Malatya Province

Cited by 6 publications

References 0 publications

Nutrient Status of Aprioct (Prunus armeniaca L.) Orchards of District Kargil, Ladakh

Nutrient Status of Aprioct (Prunus armeniaca L.) Orchards of District Kargil, Ladakh

Determination of Nutrition Status of Apple Orchards in Doğanşehir, Malatya

Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment

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