PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS

weet corn productivity in Indonesia is still in the low category. One of the causes is the problem of soil with low pH. Soil with a low pH causes the availability of nutrients to decrease, thereby inhibiting plant growth and development. Efforts can be made to add dolomite, because hydrolyzed dolomi...

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Main Authors: Lenny Sri Nopriani, Filka Ramadhani, Rizki Maulana Ishaq, Syahrul Kurniawan, Muhamad Taufiq Hidayat, Georona Kusma Albarki
Format: Article
Language:English
Published: Universitas Brawijaya 2025-01-01
Series:JTSL (Jurnal Tanah dan Sumberdaya Lahan)
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Online Access:https://jtsl.ub.ac.id/index.php/jtsl/article/view/1150
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author Lenny Sri Nopriani
Filka Ramadhani
Rizki Maulana Ishaq
Syahrul Kurniawan
Muhamad Taufiq Hidayat
Georona Kusma Albarki
author_facet Lenny Sri Nopriani
Filka Ramadhani
Rizki Maulana Ishaq
Syahrul Kurniawan
Muhamad Taufiq Hidayat
Georona Kusma Albarki
author_sort Lenny Sri Nopriani
collection DOAJ
description weet corn productivity in Indonesia is still in the low category. One of the causes is the problem of soil with low pH. Soil with a low pH causes the availability of nutrients to decrease, thereby inhibiting plant growth and development. Efforts can be made to add dolomite, because hydrolyzed dolomite can increase nutrient availability in the soil. Therefore, this research was carried out with the aim of analyzing the effect of adding various doses of dolomite on soil chemical properties, plant uptake of Ca, Mg and P, population of phosphate solubilizing bacteria, and sweet corn productivity in the Tegalan Land of Junrejo Village, Batu City, East Java. The research design used a randomized block design (RAK) consisting of 9 treatments with 3 replications. Treatment consisted of: M0 = control; M1 = 100% N, P, K; M2 = 100% N,P,K + 100% Kieserite; M3 = 100% N,P,K + 50% Dolomit; M4 = 100%  N,P,K + 100% Dolomit; M5 = 100%  N,P,K + 150% Dolomit; M6 = 75%  N,P,K + 50% Dolomit; M7 = 75%  N,P,K + 100% Dolomit; M8 = 75%  N,P,K + 150% Dolomit. The data was analyzed for diversity using R studio software and continued with the DMRT (Duncan Multiple Range Test) test at 5% level. Next, to see the relationship and influence between parameters, correlation and regression tests were carried out. The findings demonstrated that adding 2.8 tonnes of dolomite per hectare might raise soil CEC (50.61%) and pH (13.41%). In addition, the addition of 4.2 tons/ha of dolomite was able to decrease soil P-available (5.65%), increase Ca-dd (26.4%), Mg-dd (85%), Ca absorption (165.12%), Mg absorption (366.67%), P absorption (78.57%), and sweet corn yield (78.04%). The addition of different doses of dolomite did not significantly alter the overall population parameter of phosphate-solubilizing bacteria. Furthermore, the link between sweet corn yield and nutritional absorption was both robust and weak. The increase in sweet corn output was impacted by P, Ca, and Mg absorption by 54.54%, 41.21%, and 42.79%, respectively.
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spelling doaj-art-cdececb02fbd4b8f8984f35241d563ca2025-08-20T02:52:58ZengUniversitas BrawijayaJTSL (Jurnal Tanah dan Sumberdaya Lahan)2549-97932025-01-0112121122110.21776/ub.jtsl.2025.012.1.20967PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANISLenny Sri Nopriani0https://orcid.org/0009-0006-7724-6684Filka Ramadhani1Rizki Maulana Ishaq2https://orcid.org/0000-0002-5811-5199Syahrul Kurniawan3https://orcid.org/0000-0003-3053-9755Muhamad Taufiq Hidayat4Georona Kusma Albarki5Program Studi Agroekoteknologi, Fakultas Pertanian, Universitas BrawijayaProgram Studi Pengelolaan Tanah dan Air, Fakultas Pertanian, Universitas BrawijayaProgram Studi Agroekoteknologi, Fakultas Pertanian, Universitas BrawijayaProgram Studi Agroekoteknologi, Fakultas Pertanian, Universitas BrawijayaProgram Studi Agroekoteknologi, Fakultas Pertanian, Universitas BrawijayaProgram Studi Pengelolaan Tanah dan Air, Fakultas Pertanian, Universitas Brawijayaweet corn productivity in Indonesia is still in the low category. One of the causes is the problem of soil with low pH. Soil with a low pH causes the availability of nutrients to decrease, thereby inhibiting plant growth and development. Efforts can be made to add dolomite, because hydrolyzed dolomite can increase nutrient availability in the soil. Therefore, this research was carried out with the aim of analyzing the effect of adding various doses of dolomite on soil chemical properties, plant uptake of Ca, Mg and P, population of phosphate solubilizing bacteria, and sweet corn productivity in the Tegalan Land of Junrejo Village, Batu City, East Java. The research design used a randomized block design (RAK) consisting of 9 treatments with 3 replications. Treatment consisted of: M0 = control; M1 = 100% N, P, K; M2 = 100% N,P,K + 100% Kieserite; M3 = 100% N,P,K + 50% Dolomit; M4 = 100%  N,P,K + 100% Dolomit; M5 = 100%  N,P,K + 150% Dolomit; M6 = 75%  N,P,K + 50% Dolomit; M7 = 75%  N,P,K + 100% Dolomit; M8 = 75%  N,P,K + 150% Dolomit. The data was analyzed for diversity using R studio software and continued with the DMRT (Duncan Multiple Range Test) test at 5% level. Next, to see the relationship and influence between parameters, correlation and regression tests were carried out. The findings demonstrated that adding 2.8 tonnes of dolomite per hectare might raise soil CEC (50.61%) and pH (13.41%). In addition, the addition of 4.2 tons/ha of dolomite was able to decrease soil P-available (5.65%), increase Ca-dd (26.4%), Mg-dd (85%), Ca absorption (165.12%), Mg absorption (366.67%), P absorption (78.57%), and sweet corn yield (78.04%). The addition of different doses of dolomite did not significantly alter the overall population parameter of phosphate-solubilizing bacteria. Furthermore, the link between sweet corn yield and nutritional absorption was both robust and weak. The increase in sweet corn output was impacted by P, Ca, and Mg absorption by 54.54%, 41.21%, and 42.79%, respectively.https://jtsl.ub.ac.id/index.php/jtsl/article/view/1150bakteri pelarut fosfatdolomitjagung manisph rendahserapan hara
spellingShingle Lenny Sri Nopriani
Filka Ramadhani
Rizki Maulana Ishaq
Syahrul Kurniawan
Muhamad Taufiq Hidayat
Georona Kusma Albarki
PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
JTSL (Jurnal Tanah dan Sumberdaya Lahan)
bakteri pelarut fosfat
dolomit
jagung manis
ph rendah
serapan hara
title PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
title_full PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
title_fullStr PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
title_full_unstemmed PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
title_short PENGARUH DOLOMIT TERHADAP SIFAT KIMIA TANAH, BAKTERI PELARUT FOSFAT, SERAPAN Ca, Mg, P DAN PRODUKSI JAGUNG MANIS
title_sort pengaruh dolomit terhadap sifat kimia tanah bakteri pelarut fosfat serapan ca mg p dan produksi jagung manis
topic bakteri pelarut fosfat
dolomit
jagung manis
ph rendah
serapan hara
url https://jtsl.ub.ac.id/index.php/jtsl/article/view/1150
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