Geri Dön

Atça ovası alluviyal topraklarının katyon değişim kapasiteleri ( K.D.K.) , değişebilir katyonları ve bunların diğer toprak özellikleri ile olan ilişkileri

Başlık çevirisi mevcut değil.

  1. Tez No: 27787
  2. Yazar: BETÜL ERGÜN
  3. Danışmanlar: YRD. DOÇ. DR. İHSAN BÜLENT OKUR
  4. Tez Türü: Yüksek Lisans
  5. Konular: Ziraat, Agriculture
  6. Anahtar Kelimeler: Belirtilmemiş.
  7. Yıl: 1993
  8. Dil: Türkçe
  9. Üniversite: Ege Üniversitesi
  10. Enstitü: Fen Bilimleri Enstitüsü
  11. Ana Bilim Dalı: Toprak Ana Bilim Dalı
  12. Bilim Dalı: Belirtilmemiş.
  13. Sayfa Sayısı: 98

Özet

-78- between % loam contents and cation exchange capacity (CEC)? 5 % significancy level and positive (r=0.370x) correlations with exchangeable Na contents; 1 % significancy level and positive (r=Q.452xx) correlations with exchangeable Ca+++ Mg++ contents. 1 % significancy level and positive (r=0.858xx) correlations were obtained between % clay percent of researched samples and cation exchange capacity (CEC); 1 % significancy level and positive (r=0.467xx) correlations with exchangeable K+ş 1 % significancy level and positive (r=0.757xx) correlations exchangeable Ca+++ Mg++ contents. Measured pH values of studied soils at saturated soil were analysed between 7.50-8.63. Because of excess exchangeable Na+ ions, high pH vaules in soils was formed. Exchangeable sodium percentage (ESP) values of soil samples at the soil layers in the profiles was between a wide range from 1.64- 38.49 %.> There were 1 % significancy level and positive (r=0.722xx) correlations between the pH values at saturated soil of soil samples in searched area and exchangeable Na+ contents and 1 % significancy level and positive (r=0.800xx) correlations with exchangeable sodium percentage (ESP) values. Water soluble total salt contents were analysed an average value like 0.32 %. There were 1 % significancy level and positive (r=0.607xx) correlations between the water soluble total salt content of soil and exchangeable Na contents and 1 % significancy level and positive (r=0.54lxx) correlations with exchangeable sodium percentage (ESP) values. Amount of total nitrogen was between 0.02-0.15 % and organic matter contents were between the values of 0.33-1.55 %* Plain soils was supposed to be poor with respect to organic matter content. 1 % significancy level and positive (r=0.457xx) correlations were found between total nitrogen of soils belong to the searched profiles and cation exchange capacities (CEC) | 5 % significancy level and positive (r=0.380x) correlations with exchangeable Na contents. 1 % significancy level and positive (r=0.666xx) correlations were obtained between organic matter contents of soils and cation exchange capacities (CEC); 1 % significancy level and positive-79- (r=0»690xx) correlations with exchangeable K+ contents? 1 % significancy level and positive (r=0.679xx) correlations with exchangeable Ca+++ Mg+ contents. Cation exchange capacities (CEC) of soils analysed in Atça plain were found between 4.02-20.50 rae/100 gr. Due to the amount of clay and organic matter in soil, cation exchange capacities (CEC) of soils raises. Ca + Mg were dominant cations in exchange complex of soils and they were at the range between 3.78-17.57 me/100 gr. Exchangeable K+ contents were between 0.09-0.89 me/100 gr. and exchangeable Na+ contents were between 0.15-6.17 me/100 gr. 1 % significancy level and positive (r=0.449XX) correlations were obtained between cation exchange capacities (CEC) of plain soils and exchangeable K+ contents; 1 % significancy level and positive (r=0.828xx) correlations with exchangeable Ca+++ Mg++ contents. According to the result of soils in saturation extract 9 it was seen that 35 % of plain soils contains Ca++ and 32 % of plain soils contains Na and Mg cation. 5 %-l % significancy levels and positive correlations were obtained between the cations and anions in the saturation extract and electrical c. conductivity (ECxlO ) of saturation extract and especially with Na+ from exchangeable cations. Selected water samples from sources used for the purpose of irrigation of Atça plain were at the C~-S, class and they were moderately salty and had a little sodium.-78- between % loam contents and cation exchange capacity (CEC)? 5 % significancy level and positive (r=0.370x) correlations with exchangeable Na contents; 1 % significancy level and positive (r=Q.452xx) correlations with exchangeable Ca+++ Mg++ contents. 1 % significancy level and positive (r=0.858xx) correlations were obtained between % clay percent of researched samples and cation exchange capacity (CEC); 1 % significancy level and positive (r=0.467xx) correlations with exchangeable K+ş 1 % significancy level and positive (r=0.757xx) correlations exchangeable Ca+++ Mg++ contents. Measured pH values of studied soils at saturated soil were analysed between 7.50-8.63. Because of excess exchangeable Na+ ions, high pH vaules in soils was formed. Exchangeable sodium percentage (ESP) values of soil samples at the soil layers in the profiles was between a wide range from 1.64- 38.49 %.> There were 1 % significancy level and positive (r=0.722xx) correlations between the pH values at saturated soil of soil samples in searched area and exchangeable Na+ contents and 1 % significancy level and positive (r=0.800xx) correlations with exchangeable sodium percentage (ESP) values. Water soluble total salt contents were analysed an average value like 0.32 %. There were 1 % significancy level and positive (r=0.607xx) correlations between the water soluble total salt content of soil and exchangeable Na contents and 1 % significancy level and positive (r=0.54lxx) correlations with exchangeable sodium percentage (ESP) values. Amount of total nitrogen was between 0.02-0.15 % and organic matter contents were between the values of 0.33-1.55 %* Plain soils was supposed to be poor with respect to organic matter content. 1 % significancy level and positive (r=0.457xx) correlations were found between total nitrogen of soils belong to the searched profiles and cation exchange capacities (CEC) | 5 % significancy level and positive (r=0.380x) correlations with exchangeable Na contents. 1 % significancy level and positive (r=0.666xx) correlations were obtained between organic matter contents of soils and cation exchange capacities (CEC); 1 % significancy level and positive

Özet (Çeviri)

-79- (r=0»690xx) correlations with exchangeable K+ contents? 1 % significancy level and positive (r=0.679xx) correlations with exchangeable Ca+++ Mg+ contents. Cation exchange capacities (CEC) of soils analysed in Atça plain were found between 4.02-20.50 rae/100 gr. Due to the amount of clay and organic matter in soil, cation exchange capacities (CEC) of soils raises. Ca + Mg were dominant cations in exchange complex of soils and they were at the range between 3.78-17.57 me/100 gr. Exchangeable K+ contents were between 0.09-0.89 me/100 gr. and exchangeable Na+ contents were between 0.15-6.17 me/100 gr. 1 % significancy level and positive (r=0.449XX) correlations were obtained between cation exchange capacities (CEC) of plain soils and exchangeable K+ contents; 1 % significancy level and positive (r=0.828xx) correlations with exchangeable Ca+++ Mg++ contents. According to the result of soils in saturation extract 9 it was seen that 35 % of plain soils contains Ca++ and 32 % of plain soils contains Na and Mg cation. 5 %-l % significancy levels and positive correlations were obtained between the cations and anions in the saturation extract and electrical c. conductivity (ECxlO ) of saturation extract and especially with Na+ from exchangeable cations. Selected water samples from sources used for the purpose of irrigation of Atça plain were at the C~-S, class and they were moderately salty and had a little sodium.-78- between % loam contents and cation exchange capacity (CEC)? 5 % significancy level and positive (r=0.370x) correlations with exchangeable Na contents; 1 % significancy level and positive (r=Q.452xx) correlations with exchangeable Ca+++ Mg++ contents. 1 % significancy level and positive (r=0.858xx) correlations were obtained between % clay percent of researched samples and cation exchange capacity (CEC); 1 % significancy level and positive (r=0.467xx) correlations with exchangeable K+ş 1 % significancy level and positive (r=0.757xx) correlations exchangeable Ca+++ Mg++ contents. Measured pH values of studied soils at saturated soil were analysed between 7.50-8.63. Because of excess exchangeable Na+ ions, high pH vaules in soils was formed. Exchangeable sodium percentage (ESP) values of soil samples at the soil layers in the profiles was between a wide range from 1.64- 38.49 %.> There were 1 % significancy level and positive (r=0.722xx) correlations between the pH values at saturated soil of soil samples in searched area and exchangeable Na+ contents and 1 % significancy level and positive (r=0.800xx) correlations with exchangeable sodium percentage (ESP) values. Water soluble total salt contents were analysed an average value like 0.32 %. There were 1 % significancy level and positive (r=0.607xx) correlations between the water soluble total salt content of soil and exchangeable Na contents and 1 % significancy level and positive (r=0.54lxx) correlations with exchangeable sodium percentage (ESP) values. Amount of total nitrogen was between 0.02-0.15 % and organic matter contents were between the values of 0.33-1.55 %* Plain soils was supposed to be poor with respect to organic matter content. 1 % significancy level and positive (r=0.457xx) correlations were found between total nitrogen of soils belong to the searched profiles and cation exchange capacities (CEC) | 5 % significancy level and positive (r=0.380x) correlations with exchangeable Na contents. 1 % significancy level and positive (r=0.666xx) correlations were obtained between organic matter contents of soils and cation exchange capacities (CEC); 1 % significancy level and positive-79- (r=0»690xx) correlations with exchangeable K+ contents? 1 % significancy level and positive (r=0.679xx) correlations with exchangeable Ca+++ Mg+ contents. Cation exchange capacities (CEC) of soils analysed in Atça plain were found between 4.02-20.50 rae/100 gr. Due to the amount of clay and organic matter in soil, cation exchange capacities (CEC) of soils raises. Ca + Mg were dominant cations in exchange complex of soils and they were at the range between 3.78-17.57 me/100 gr. Exchangeable K+ contents were between 0.09-0.89 me/100 gr. and exchangeable Na+ contents were between 0.15-6.17 me/100 gr. 1 % significancy level and positive (r=0.449XX) correlations were obtained between cation exchange capacities (CEC) of plain soils and exchangeable K+ contents; 1 % significancy level and positive (r=0.828xx) correlations with exchangeable Ca+++ Mg++ contents. According to the result of soils in saturation extract 9 it was seen that 35 % of plain soils contains Ca++ and 32 % of plain soils contains Na and Mg cation. 5 %-l % significancy levels and positive correlations were obtained between the cations and anions in the saturation extract and electrical c. conductivity (ECxlO ) of saturation extract and especially with Na+ from exchangeable cations. Selected water samples from sources used for the purpose of irrigation of Atça plain were at the C~-S, class and they were moderately salty and had a little sodium.

Benzer Tezler

  1. Tez No

    717000

    Kolorektal karsinomalarda DNA yanlış eşleşme onarım genlerinin immünohistokimyasal yolla analizi

    Immunohistochemical analysis of dna mismatch repair genes in colorectal carcinomas

    MÜMİNE GÖRMEZ

    Tıpta Uzmanlık

    Türkçe

    Türkçe

    2021

    PatolojiTokat Gaziosmanpaşa Üniversitesi

    Tıbbi Patoloji Ana Bilim Dalı

    PROF. DR. REŞİT DOĞAN KÖSEOĞLU

  2. Tez No

    439620

    Gemlik körfezi'nde geç pleistosen-holosen dönemi deniz seviyesi ve paleo-iklim değişimleri

    Late pleistocene to holocene paleoceanographic and paleo-climatic changes in gulf of gemlik, sea of Marmara, Turkey

    BETÜL FİLİKCİ

    Yüksek Lisans

    Türkçe

    Türkçe

    2016

    Jeoloji Mühendisliğiİstanbul Teknik Üniversitesi

    Jeoloji Mühendisliği Ana Bilim Dalı

    DOÇ. DR. KÜRŞAD KADİR ERİŞ

  3. Tez No

    582722

    Kadın ve benlik kurgusu: Ağaoğlu, Burak, Soysal ve Özlü

    Woman and self-construal: Ağaoğlu, Burak, Soysal and Özlü

    MÜLKİYE ATÇA

    Yüksek Lisans

    Türkçe

    Türkçe

    2019

    Türk Dili ve EdebiyatıVan Yüzüncü Yıl Üniversitesi

    Türk Dili ve Edebiyatı Ana Bilim Dalı

    DOÇ. DR. SEYİT BATTAL UĞURLU

  4. Tez No

    742341

    Coupling of NAMI DANCE and XBeach numerical models to simulate tsunami induced morphological changes: Case study in Sığacık bay

    Tsunami kaynaklı morfolojik değişimlerin benzetimi için NAMI DANCE ve XBeach sayısal modellerinin etkileşimli kullanımı: Sığacık koyu'ndan vaka çalışması

    YAĞIZ ARDA ÇİÇEK

    Yüksek Lisans

    İngilizce

    İngilizce

    2022

    İnşaat MühendisliğiOrta Doğu Teknik Üniversitesi

    İnşaat Mühendisliği Ana Bilim Dalı

    PROF. DR. AHMET CEVDET YALÇINER

    DR. ÖĞR. ÜYESİ CÜNEYT BAYKAL

  5. Tez No

    387137

    Acoustic design based on multi-aspect performance analysis

    Çok yönlü başarım çözümlemesine dayalı akustik tasarım

    EMRE ATÇA

    Yüksek Lisans

    İngilizce

    İngilizce

    2013

    Mimarlıkİzmir Yüksek Teknoloji Enstitüsü

    Mimarlık Ana Bilim Dalı

    DOÇ. DR. MUSTAFA EMRE İLAL

Geri Dön