Metric quick check
Kirish
10,000 m² open water area, 15,000 m³ inflow, 12,000 m³ drainage, 4,500 m³ reuse, 800 m³ storage increase
Chiqish
Evaporation is about 900 m³, net balance is about +5,800 m³, and reuse share is about 23%.
Konchilik hisob-kitobi
Browser-only
Metric / imperial
Climate-adjusted evaporation
Konchilik suv balansi kalkulyatori
Kirim, drenaj, qayta foydalanish, bug'lanish va saqlash o'zgarishidan kon maydoni suv balansini bir joyda baholang.
Davr jami, kunlik o'rtacha, kaskad diagrammasi va ulashiladigan URL lar brauzerda qoladi.
Xavfsizlik eslatmalari
Barcha hisoblar shu brauzerda bajariladi va hech narsa serverga yuborilmaydi.
- Bu tezkor balans tekshiruvi, gidrologiya yoki ruxsatnoma modeli emas.
- Evaporation is estimated from area and simple climate factors, so use measured data when you have it.
- Check the unit system before sharing a result.
Bu vosita nima ko'rsatadi
Uchrashuvlar va hisobotlar uchun tezkor xulosa.
- Davr jami va kunlik o'rtacha bir xil hisobdan olinadi.
- Iqlim zonasi va mahalliy sharoitlar bug'lanish bahosini moslaydi.
- Ulashiladigan URL lar joriy holatni qayta tiklay oladi.
Qanday foydalanish
- Hisobot davri va birlik tizimini tanlang.
- Maydon, iqlim, kirim, drenaj, qayta foydalanish va saqlash o'zgarishini kiriting.
- Boshlang'ich nuqta kerak bo'lsa, namunani yuklang.
- Kaskad diagrammasi, taqsimot jadvali va ulashish URL ini ko'rib chiqing.
Misollar
Kirish / Chiqish
Imperial quick check
Kirish
1 acre open water area, 500,000 US gal inflow, 650,000 US gal drainage, 120,000 US gal reuse, 40,000 US gal storage increase
Chiqish
Evaporation is about 288,700 US gal and net balance is about -358,700 US gal.
Formulalar
- tempFactor = clamp(1 + (temperature - 20) × 0.025, 0.65, 1.45)
- humidityFactor = clamp(1 - (humidity - 50) × 0.0035, 0.55, 1.25)
- climateFactor = clamp(tempFactor × humidityFactor × windFactor × sunFactor, 0.5, 1.8)
- evaporation = area × depth × period
- net balance = inflow + reuse - drainage - evaporation - storage change
Lug'at
- Davr jami
- Tanlangan hisobot davridagi umumiy hajm.
- Kunlik o'rtacha
- Davr jami kunlar soniga bo'lingan qiymat.
- Iqlim omili
- Asosiy bug'lanish chuqurligini moslaydigan oddiy ko'paytirgich.
- Storage change
- Davr davomida saqlashga qo'shilgan yoki undan olingan suv.
Tez-tez so'raladigan savollar
Is this a replacement for a water balance model?
No. It is a quick reporting and comparison tool.
How is evaporation estimated?
The tool multiplies a base depth by simple climate factors and the open water area.
Can I compare periods in different unit systems?
Yes. The same input state can be shared with a URL, and the unit system is stored with it.
Can I leave the open water area at zero?
Yes. Evaporation becomes zero and the rest of the balance still works.
Eslatmalar
- Bu vosita tezkor balans tekshiruvi va hisobotlar uchun, batafsil gidrologiya uchun emas.
- Iqlim juda keskin ko'rinsa, bug'lanish bahosini taxminiy qo'llanma sifatida oling.
- Drenaj kirim va qayta foydalanishdan ancha katta bo'lsa, odatda birlik xatosi bo'ladi.
- Hisoblarni solishtirganda bir xil birlik tizimidan foydalaning.