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Daur Biogeokimia Ekosistem

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Daur Biogeokimia Ekosistem

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Uji pemahaman daur biogeokimia

Created by

Rifka Anisa
Rifka Anisa
Indonesia

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Daur Biogeokimia Ekosistem
 

Daur Biogeokimia EkosistemOnline version

Uji pemahaman daur biogeokimia

by Rifka Anisa
1

Apa jalur utama karbon masuk ke biosfer dalam ekosistem lewat proses apa?

2

Proses mana yang mengubah nitrogen bebasis N2 menjadi bentuk amonia NH3/H2N-?

3

Mengapa fosfor tidak memiliki komponen siklus atmosferik yang signifikan?

4

Peran dekomposer dalam daur karbon ekosistem adalah?

5

Apa dampak utama peningkatan penggunaan pupuk nitrogen terhadap siklusnya di ekosistem akuatik?

6

Proses apa yang mengubah nitrat NO3− menjadi N2 di atmosferik/lingkungan?

7

Apa peran air dalam daur biogeokimia fosfor?

8

Kita menyebut proses yang mengubah bahan organik menjadi NH4+ adalah?

9

Apa sumber utama nitrogen yang tersedia bagi tumbuhan di kebun?

10

Mengapa kuantitas karbon di biosfer penting untuk perubahan iklim?

Feedback

Fotosintesis mengubah CO2 atmosfer menjadi vaksi organik di tumbuhan; yang lain adalah bagian siklus selanjutnya.

Nitrogen fixation mengikat N2 dari udara menjadi amonia; nitrifikasi dan denitrifikasi melibatkan oksidasi/reduksi lain.

Fosfor umumnya berada di tanah/perairan dan bebatuan; volatilitasnya sangat rendah dibanding karbon/nitrogen.

Dekomposer mem mineralisasi materi organik menjadi CO2, air, dan mineral yang dapat diambil oleh tumbuhan.

Nitragen berlebih bisa mencemari air, memicu aliran nutrien dan pertumbuhan alga berlebih.

Denitrifikasi mengubah nitrates menjadi gas N2, melepasnya ke atmosfer.

Fosfor utamanya berpindah secara geokimia melalui pelarutan, sedimentasi, dan mineralisasi.

Amonifikasi adalah pelepasan NH4+ dari materi organik oleh mikroba.

Tumbuhan menyerap NO3− dan NH4+ sebagai bentuk nitrogen yang terlarut.

Daur karbon menentukan seberapa banyak CO2 di atmosfer, mempengaruhi efek rumah kaca.

 
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